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Aruba | Table of Content | Short description, Etymology, History, Pre-ceramic age, Early human migration and cultural exchange, Neo-Indian period: the Caquetío, Caquetío chiefdom, Political units and governance, Agriculture, trade, and network, Burial practices, Last indigenous Aruban, Spanish period, Early explorations, Conquistadors, Spanish ranch, Early Dutch period, Dutch conquest: salt, New Netherland, Slavery, English interregnum and economic development, 20th and 21st centuries, Autonomy, Geography, Regions, Flora and fauna, Climate and natural hazards, Demographics, Language, Religion, Government, Politics, Foreign relations, Military, Education, Economy, Tourism, Culture, Architecture, Sport, Infrastructure, Places of interest, Notable people, See also, Notes, Sources, References, Further reading, External links |
Articles of Confederation | Short description | The Articles of Confederation, officially the Articles of Confederation and Perpetual Union, was an agreement and early body of law in the Thirteen Colonies, which served as the nation's first frame of government during the American Revolution. It was debated by the Second Continental Congress at present-day Independence Hall in Philadelphia between July 1776 and November 1777, was finalized by the Congress on November 15, 1777, and came into force on March 1, 1781, after being ratified by all 13 colonial states.
A central and guiding principle of the Articles was the establishment and preservation of the independence and sovereignty of the original 13 states. The Articles consciously established a weak confederal government, affording it only those powers the former colonies recognized as belonging to the British Crown and Parliament during the colonial era. The document provided clearly written rules for how the states' league of friendship, known as the Perpetual Union, was to be organized.
While waiting for all states to ratify the Articles, the Congress observed them as it conducted business during the American Revolution, directing the Revolutionary War effort, conducting diplomacy with foreign states, addressing territorial issues, and dealing with Native American relations. Little changed procedurally once the Articles of Confederation went into effect, since their ratification mostly codified laws already in existence and procedures the Continental Congress had already been following. The body was renamed the Congress of the Confederation, but most Americans continued to call it the Continental Congress, since its organization remained the same.
As the Confederation Congress attempted to govern the continually growing 13 colonial states, its delegates discovered that the limitations on the central government, such as in assembling delegates, raising funds, and regulating commerce, limited its ability to do so. As the government's weaknesses became apparent, especially after Shays's Rebellion, several prominent political thinkers in the fledgling union began asking for changes to the Articles that would strengthen the powers afforded to the central government.
In September 1786, some states met to address interstate protectionist trade barriers between them. Shortly thereafter, as more states became interested in meeting to revise the Articles, a meeting was set in Philadelphia on May 25, 1787. This became the Constitutional Convention. Delegates quickly agreed that the defects of the frame of government could not be remedied by altering the Articles, and so went beyond their mandate by authoring a new constitution and sent it to the states for ratification. After significant ratification debates in each state and across the nation, on March 4, 1789, the government under the Articles was replaced with the federal government under the Constitution. The new Constitution provided for a much stronger federal government by establishing a chief executive (the president), courts, and taxing powers. |
Articles of Confederation | Background and context | Background and context
The political push to increase cooperation among the then-loyal colonies began with the Albany Congress in 1754 and Benjamin Franklin's proposed Albany Plan, an inter-colonial collaboration to help solve mutual local problems. Over the next two decades, some of the basic concepts it addressed would strengthen; others would weaken, especially in the degree of loyalty (or lack thereof) owed the Crown. Colonists' civil disobedience resulted in the British enacting coercive and quelling measures, such as the passage of what colonists called the Intolerable Acts in the British Parliament, and armed skirmishes which resulted in dissidents being proclaimed rebels. These actions eroded the number of colonists continuing to be Loyalists to the Crown. Together with the highly effective propaganda campaign of the Patriot leaders, caused an increasing number of colonists to begin agitating for independence from the mother country. In 1775, with events outpacing communications, the Second Continental Congress began acting as the provisional government for the United Colonies.
It was an era of constitution writing—most states were busy at the task—and leaders felt the new nation must have a written constitution; a "rulebook" for how the new nation should function. During the war, Congress exercised an unprecedented level of political, diplomatic, military and economic authority. It adopted trade restrictions, established and maintained an army, issued fiat money, created a military code and negotiated with foreign governments.
To transform themselves from outlaws into a legitimate nation, the colonists needed international recognition for their cause and foreign allies to support it. In early 1776, Thomas Paine argued in the closing pages of the first edition of Common Sense that the "custom of nations" demanded a formal declaration of American independence if any European power were to mediate a peace between the Americans and Great Britain. The monarchies of France and Spain, in particular, could not be expected to aid those they considered rebels against another legitimate monarch. Foreign courts needed to have American grievances laid before them persuasively in a "manifesto" which could also reassure them that the Americans would be reliable trading partners. Without such a declaration, Paine concluded, "[t]he custom of all courts is against us, and will be so, until, by an independence, we take rank with other nations."
Beyond improving their existing association, the records of the Second Continental Congress show that the need for a declaration of independence was intimately linked with the demands of international relations. On June 7, 1776, Richard Henry Lee introduced a resolution before the Continental Congress declaring the colonies independent; at the same time, he also urged Congress to resolve "to take the most effectual measures for forming foreign Alliances" and to prepare a plan of confederation for the newly independent states. Congress then created three overlapping committees to draft the Declaration, a model treaty, and the Articles of Confederation. The Declaration announced the states' entry into the international system; the model treaty was designed to establish amity and commerce with other states; and the Articles of Confederation, which established "a firm league" among the thirteen free and independent states, constituted an international agreement to set up central institutions for the conduct of vital domestic and foreign affairs. |
Articles of Confederation | Drafting | Drafting
thumb|right|upright=.90|alt=Historical 13-cent postage stamp commemorating the Articles of Confederation 200th anniversary|1977 13-cent U.S. Postage stamp commemorating the Articles of Confederation bicentennial; the draft was completed on November 15, 1777
On June 12, 1776, a day after appointing the Committee of Five to prepare a draft of the Declaration of Independence, the Second Continental Congress resolved to appoint a committee of 13 with one representative from each colony to prepare a draft of a constitution for a union of the states. The committee was made up of the following individuals:
John Dickinson (Pennsylvania, chairman of the committee)
Samuel Adams (Massachusetts)
Josiah Bartlett (New Hampshire)
Button Gwinnett (Georgia)
Joseph Hewes (North Carolina)
Stephen Hopkins (Rhode Island)
Robert R. Livingston (New York)
Thomas McKean (Delaware)
Thomas Nelson (Virginia)
Edward Rutledge (South Carolina)
Roger Sherman (Connecticut)
Thomas Stone (Maryland)
Francis Hopkinson (New Jersey, added to the committee last)
The committee met frequently, and chairman John Dickinson presented their results to the Congress on July 12, 1776. Afterward, there were long debates on such issues as state sovereignty, the exact powers to be given to Congress, whether to have a judiciary, western land claims, and voting procedures. To further complicate work on the constitution, Congress was forced to leave Philadelphia twice, for Baltimore, Maryland, in the winter of 1776, and later for Lancaster then York, Pennsylvania, in the fall of 1777, to evade advancing British troops. Even so, the committee continued with its work.
The final draft of the Articles of Confederation and Perpetual Union was completed on November 15, 1777. Consensus was achieved by including language guaranteeing that each state retained its sovereignty, leaving the matter of western land claims in the hands of the individual states, including language stating that votes in Congress would be en bloc by state, and establishing a unicameral legislature with limited and clearly delineated powers. |
Articles of Confederation | Ratification | Ratification
The Articles of Confederation was submitted to the states for ratification in late November 1777. The first state to ratify was Virginia on December 16, 1777; 12 states had ratified the Articles by February 1779, 14 months into the process. The lone holdout, Maryland, refused to go along until the landed states, especially Virginia, had indicated they were prepared to cede their claims west of the Ohio River to the Union. It would be two years before the Maryland General Assembly became satisfied that the various states would follow through, and voted to ratify. During this time, Congress observed the Articles as its de facto frame of government. Maryland finally ratified the Articles on February 2, 1781. Congress was informed of Maryland's assent on March 1, and officially proclaimed the Articles of Confederation to be the law of the land.
The several states ratified the Articles of Confederation on the following dates: References to a 1778 Virginia ratification are based on an error in the Journals of Congress: "The published Journals of Congress print this enabling act of the Virginia assembly under date of Dec. 15, 1778. This error has come from the MS. vol. 9 (History of Confederation), p. 123, Papers of the Continental Congress, Library of Congress."
State Date 30px Virginia 30px South Carolina 30px New York 30px Rhode Island 26px Connecticut 30px Georgia 30px New Hampshire 30px Pennsylvania 30px Massachusetts 30px North Carolina 30px New Jersey 30px Delaware 30px Maryland |
Articles of Confederation | Article summaries | Article summaries
The Articles of Confederation contain a preamble, thirteen articles, a conclusion, and a signatory section. The individual articles set the rules for current and future operations of the confederation's central government. Under the Articles, the states retained sovereignty over all governmental functions not specifically relinquished to the national Congress, which was empowered to make war and peace, negotiate diplomatic and commercial agreements with foreign countries, and to resolve disputes between the states. The document also stipulates that its provisions "shall be inviolably observed by every state" and that "the Union shall be perpetual".
Summary of the purpose and content of each of the 13 articles:
Establishes the name of the confederation with these words: "The stile of this confederacy shall be 'The United States of America.
Asserts the sovereignty of each state, except for the specific powers delegated to the confederation government: "Each state retains its sovereignty, freedom, and independence, and every power, jurisdiction, and right, which is not by this Confederation expressly delegated."
Declares the purpose of the confederation: "The said States hereby severally enter into a firm league of friendship with each other, for their common defense, the security of their liberties, and their mutual and general welfare, binding themselves to assist each other, against all force offered to, or attacks made upon them, or any of them, on account of religion, sovereignty, trade, or any other pretense whatever."
Elaborates upon the intent "to secure and perpetuate mutual friendship and intercourse among the people of the different States in this union," and to establish equal treatment and freedom of movement for the free inhabitants of each state to pass unhindered between the states, excluding "paupers, vagabonds, and fugitives from justice." All these people are entitled to equal rights established by the state into which they travel. If a crime is committed in one state and the perpetrator flees to another state, if caught they will be extradited to and tried in the state in which the crime was committed.
Allocates one vote in the Congress of the Confederation (the "United States in Congress Assembled") to each state, which is entitled to a delegation of between two and seven members. Members of Congress are to be appointed by state legislatures. No congressman may serve more than three out of any six years.
Only the central government may declare war, or conduct foreign political or commercial relations. No state or official may accept foreign gifts or titles, and granting any title of nobility is forbidden to all. No states may form any sub-national groups. No state may tax or interfere with treaty stipulations already proposed. No state may wage war without permission of Congress, unless invaded or under imminent attack on the frontier; no state may maintain a peacetime standing army or navy, unless infested by pirates, but every State is required to keep ready, a well-trained, disciplined, and equipped militia.
Whenever an army is raised for common defense, the state legislatures shall assign military ranks of colonel and below.
Expenditures by the United States of America will be paid with funds raised by state legislatures, and apportioned to the states in proportion to the real property values of each.
Powers and functions of the United States in Congress Assembled.
Grants to the United States in Congress assembled the sole and exclusive right and power to determine peace and war; to exchange ambassadors; to enter into treaties and alliances, with some provisos; to establish rules for deciding all cases of captures or prizes on land or water; to grant letters of marque and reprisal (documents authorizing privateers) in times of peace; to appoint courts for the trial of pirates and crimes committed on the high seas; to establish courts for appeals in all cases of captures, but no member of Congress may be appointed a judge; to set weights and measures (including coins), and for Congress to serve as a final court for disputes between states.
The court will be composed of jointly appointed commissioners or Congress shall appoint them. Each commissioner is bound by oath to be impartial. The court's decision is final.
Congress shall regulate the post offices; appoint officers in the military; and regulate the armed forces.
The United States in Congress assembled may appoint a president who shall not serve longer than one year per three-year term of the Congress.
Congress may request requisitions (demands for payments or supplies) from the states in proportion with their population, or take credit.
Congress may not declare war, enter into treaties and alliances, appropriate money, or appoint a commander in chief without nine states assenting. Congress shall keep a journal of proceedings and adjourn for periods not to exceed six months.
When Congress is in recess, any of the powers of Congress may be executed by "The committee of the states, or any nine of them", except for those powers of Congress which require nine states in Congress to execute.
If Canada [referring to the British Province of Quebec] accedes to this confederation, it will be admitted. No other colony could be admitted without the consent of nine states.
Affirms that the Confederation will honor all bills of credit incurred, monies borrowed, and debts contracted by Congress before the existence of the Articles.
Declares that the Articles shall be perpetual, and may be altered only with the approval of Congress and the ratification of all the state legislatures. |
Articles of Confederation | Congress under the Articles | Congress under the Articles |
Articles of Confederation | Army | Army
Under the Articles, Congress had the authority to regulate and fund the Continental Army, but it lacked the power to compel the States to comply with requests for either troops or funding. This left the military vulnerable to inadequate funding, supplies, and even food. Further, although the Articles enabled the states to present a unified front when dealing with the European powers, as a tool to build a centralized war-making government, they were largely a failure; Historian Bruce Chadwick wrote:
Phelps wrote:
The Continental Congress, before the Articles were approved, had promised soldiers a pension of half pay for life. However Congress had no power to compel the states to fund this obligation, and as the war wound down after the victory at Yorktown the sense of urgency to support the military was no longer a factor. No progress was made in Congress during the winter of 1783–84. General Henry Knox, who would later become the first Secretary of War under the Constitution, blamed the weaknesses of the Articles for the inability of the government to fund the army. The army had long been supportive of a strong union.
Knox wrote:
As Congress failed to act on the petitions, Knox wrote to Gouverneur Morris, four years before the Philadelphia Convention was convened, "As the present Constitution is so defective, why do not you great men call the people together and tell them so; that is, to have a convention of the States to form a better Constitution."
Once the war had been won, the Continental Army was largely disbanded. A very small national force was maintained to man the frontier forts and to protect against Native American attacks. Meanwhile, each of the states had an army (or militia), and 11 of them had navies. The wartime promises of bounties and land grants to be paid for service were not being met. In 1783, George Washington defused the Newburgh conspiracy, but riots by unpaid Pennsylvania veterans forced Congress to leave Philadelphia temporarily.
The Congress from time to time during the Revolutionary War requisitioned troops from the states. Any contributions were voluntary, and in the debates of 1788, the Federalists (who supported the proposed new Constitution) claimed that state politicians acted unilaterally, and contributed when the Continental army protected their state's interests. The Anti-Federalists claimed that state politicians understood their duty to the Union and contributed to advance its needs. Dougherty (2009) concludes that generally the States' behavior validated the Federalist analysis. This helps explain why the Articles of Confederation needed reforms. |
Articles of Confederation | Foreign policy | Foreign policy
The 1783 Treaty of Paris, which ended hostilities with Great Britain, languished in Congress for several months because too few delegates were present at any one time to constitute a quorum so that it could be ratified. Afterward, the problem only got worse as Congress had no power to enforce attendance. Rarely did more than half of the roughly sixty delegates attend a session of Congress at the time, causing difficulties in raising a quorum. The resulting paralysis embarrassed and frustrated many American nationalists, including George Washington. Many of the most prominent national leaders, such as Washington, John Adams, John Hancock, and Benjamin Franklin, retired from public life, served as foreign delegates, or held office in state governments; and for the general public, local government and self-rule seemed quite satisfactory. This served to exacerbate Congress's impotence.
Inherent weaknesses in the confederation's frame of government also frustrated the ability of the government to conduct foreign policy. In 1786, Thomas Jefferson, concerned over the failure of Congress to fund an American naval force to confront the Barbary pirates, wrote in a diplomatic correspondence to James Monroe that, "It will be said there is no money in the treasury. There never will be money in the treasury till the Confederacy shows its teeth." [Original source: The Papers of Thomas Jefferson, vol. 10, June 22–December 31, 1786, ed. Julian P. Boyd. Princeton: Princeton University Press, 1954, pp. 560–566]
Furthermore, the 1786 Jay–Gardoqui Treaty with Spain also showed weakness in foreign policy. In this treaty, which was never ratified, the United States was to give up rights to use the Mississippi River for 25 years, which would have economically strangled the settlers west of the Appalachian Mountains. Finally, due to the Confederation's military weakness, it could not compel the British army to leave frontier forts which were on American soil—and which, in 1783, the British promised to leave, but which they delayed leaving pending U.S. implementation of other provisions such as ending action against Loyalists and allowing them to seek compensation. This incomplete British implementation of the Treaty of Paris would later be resolved by the implementation of Jay's Treaty in 1795 after the federal Constitution came into force. |
Articles of Confederation | Taxation and commerce | Taxation and commerce
Under the Articles of Confederation, the central government's power was kept quite limited. The Confederation Congress could make decisions but lacked enforcement powers. Implementation of most decisions, including modifications to the Articles, required unanimous approval of all thirteen state legislatures.
Congress was denied any powers of taxation: it could only request money from the states. The states often failed to meet these requests in full, leaving both Congress and the Continental Army chronically short of money. As more money was printed by Congress, the continental dollars depreciated. In 1779, George Washington wrote to John Jay, who was serving as the president of the Continental Congress, "that a wagon load of money will scarcely purchase a wagon load of provisions." Mr. Jay and the Congress responded in May by requesting $45 million from the States. In an appeal to the States to comply, Jay wrote that the taxes were "the price of liberty, the peace, and the safety of yourselves and posterity." He argued that Americans should avoid having it said "that America had no sooner become independent than she became insolvent" or that "her infant glories and growing fame were obscured and tarnished by broken contracts and violated faith." The States did not respond with any of the money requested from them.
Congress had also been denied the power to regulate either foreign trade or interstate commerce and, as a result, all of the States maintained control over their own trade policies. The states and the Confederation Congress both incurred large debts during the Revolutionary War, and how to repay those debts became a major issue of debate following the War. Some States paid off their war debts and others did not. Federal assumption of the states' war debts became a major issue in the deliberations of the Constitutional Convention. |
Articles of Confederation | Accomplishments | Accomplishments
Nevertheless, the Confederation Congress did take two actions with long-lasting impact. The Land Ordinance of 1785 and Northwest Ordinance created territorial government, set up protocols for the admission of new states and the division of land into useful units, and set aside land in each township for public use. This system represented a sharp break from imperial colonization, as in Europe, and it established the precedent by which the national (later, federal) government would be sovereign and expand westward—as opposed to the existing states doing so under their sovereignty.
The Land Ordinance of 1785 established both the general practices of land surveying in the west and northwest and the land ownership provisions used throughout the later westward expansion beyond the Mississippi River. Frontier lands were surveyed into the now-familiar squares of land called the township (36 square miles), the section (one square mile), and the quarter section (160 acres). This system was carried forward to most of the States west of the Mississippi (excluding areas of Texas and California that had already been surveyed and divided up by the Spanish Empire). Then, when the Homestead Act was enacted in 1867, the quarter section became the basic unit of land that was granted to new settler-farmers.
The Northwest Ordinance of 1787 noted the agreement of the original states to give up northwestern land claims, organized the Northwest Territory and laid the groundwork for the eventual creation of new states. Although it did not happen under the articles, the land north of the Ohio River and west of the (present) western border of Pennsylvania ceded by Massachusetts, Connecticut, New York, Pennsylvania, and Virginia, eventually became the states of Ohio, Indiana, Illinois, Michigan, and Wisconsin, and the part of Minnesota that is east of the Mississippi River. The Northwest Ordinance of 1787 also made great advances in the abolition of slavery. New states admitted to the union in this territory would never be slave states.
No new states were admitted to the Union under the Articles of Confederation. The Articles provided for a blanket acceptance of the Province of Quebec (referred to as "Canada" in the Articles) into the United States if it chose to do so. It did not, and the subsequent Constitution carried no such special provision of admission. Additionally, ordinances to admit Frankland (later modified to Franklin), Kentucky, and Vermont to the Union were considered, but none were approved. |
Articles of Confederation | Presidents of Congress | Presidents of Congress
Under the Articles of Confederation, the presiding officer of Congress—referred to in many official records as President of the United States in Congress Assembled—chaired the Committee of the States when Congress was in recess, and performed other administrative functions. He was not, however, an executive in the way the later president of the United States is a chief executive, since all of the functions he executed were under the direct control of Congress.
There were 10 presidents of Congress under the Articles. The first, Samuel Huntington, had been serving as president of the Continental Congress since September 28, 1779.
President TermSamuel Huntington July 10, 1781Thomas McKean November 5, 1781John Hanson November 4, 1782Elias Boudinot November 3, 1783Thomas Mifflin June 3, 1784 Richard Henry Lee November 4, 1785John Hancock June 5, 1786Nathaniel Gorham November 3, 1786Arthur St. Clair November 4, 1787Cyrus Griffin November 15, 1788 |
Articles of Confederation | U.S. under the Articles | U.S. under the Articles
The peace treaty left the United States independent and at peace but with an unsettled governmental structure. The Articles envisioned a permanent confederation but granted to the Congress—the only federal institution—little power to finance itself or to ensure that its resolutions were enforced. There was no president, no executive agencies, no judiciary, and no tax base. The absence of a tax base meant that there was no way to pay off state and national debts from the war years except by requesting money from the states, which seldom arrived. Although historians generally agree that the Articles were too weak to hold the fast-growing nation together, they do give credit to the settlement of the western issue, as the states voluntarily turned over their lands to national control.
By 1783, with the end of the British blockade, the new nation was regaining its prosperity. However, trade opportunities were restricted by the mercantilism of the British and French empires. The ports of the British West Indies were closed to all staple products which were not carried in British ships. France and Spain established similar policies. Simultaneously, new manufacturers faced sharp competition from British products which were suddenly available again. Political unrest in several states and efforts by debtors to use popular government to erase their debts increased the anxiety of the political and economic elites which had led the Revolution. The apparent inability of the Congress to redeem the public obligations (debts) incurred during the war, or to become a forum for productive cooperation among the states to encourage commerce and economic development, only aggravated a gloomy situation. In 1786–87, Shays's Rebellion, an uprising of dissidents in western Massachusetts against the state court system, threatened the stability of state government.
The Continental Congress printed paper money which was so depreciated that it ceased to pass as currency, spawning the expression "not worth a continental". Congress could not levy taxes and could only make requisitions upon the States. Less than a million and a half dollars came into the treasury between 1781 and 1784, although the governors had been asked for two million in 1783 alone.
When John Adams went to London in 1785 as the first representative of the United States, he found it impossible to secure a treaty for unrestricted commerce. Demands were made for favors and there was no assurance that individual states would agree to a treaty. Adams stated it was necessary for the States to confer the power of passing navigation laws to Congress, or that the States themselves pass retaliatory acts against Great Britain. Congress had already requested and failed to get power over navigation laws. Meanwhile, each State acted individually against Great Britain to little effect. When other New England states closed their ports to British shipping, Connecticut hastened to profit by opening its ports.
By 1787, Congress was unable to protect manufacturing and shipping. State legislatures were unable or unwilling to resist attacks upon private contracts and public credit. Land speculators expected no rise in values when the government could not defend its borders nor protect its frontier population.
The idea of a convention to revise the Articles of Confederation grew in favor. Alexander Hamilton realized while serving as Washington's top aide that a strong central government was necessary to avoid foreign intervention and allay the frustrations due to an ineffectual Congress. Hamilton led a group of like-minded nationalists, won Washington's endorsement, and convened the Annapolis Convention in 1786 to petition Congress to call a constitutional convention to meet in Philadelphia to remedy the long-term crisis. |
Articles of Confederation | Signatures | Signatures
The Second Continental Congress approved the Articles for distribution to the states on November 15, 1777. A copy was made for each state and one was kept by the Congress. On November 28, the copies sent to the states for ratification were unsigned, and the cover letter, dated November 17, had only the signatures of Henry Laurens and Charles Thomson, who were the President and Secretary to the Congress.
The Articles, however, were unsigned, and the date was blank. Congress began the signing process by examining their copy of the Articles on June 27, 1778. They ordered a final copy prepared (the one in the National Archives), and that delegates should inform the secretary of their authority for ratification.
On July 9, 1778, the prepared copy was ready. They dated it and began to sign. They also requested each of the remaining states to notify its delegation when ratification was completed. On that date, delegates present from New Hampshire, Massachusetts, Rhode Island, Connecticut, New York, Pennsylvania, Virginia and South Carolina signed the Articles to indicate that their states had ratified. New Jersey, Delaware and Maryland could not, since their states had not ratified. North Carolina and Georgia also were unable to sign that day, since their delegations were absent.
After the first signing, some delegates signed at the next meeting they attended. For example, John Wentworth of New Hampshire added his name on August 8. John Penn was the first of North Carolina's delegates to arrive (on July 10), and the delegation signed the Articles on July 21, 1778.
The other states had to wait until they ratified the Articles and notified their Congressional delegation. Georgia signed on July 24, New Jersey on November 26, and Delaware on February 12, 1779. Maryland refused to ratify the Articles until every state had ceded its western land claims. Chevalier de La Luzerne, French Minister to the United States, felt that the Articles would help strengthen the American government. In 1780, when Maryland requested France provide naval forces in the Chesapeake Bay for protection from the British (who were conducting raids in the lower part of the bay), he indicated that French Admiral Destouches would do what he could but La Luzerne also "sharply pressed" Maryland to ratify the Articles, thus suggesting the two issues were related.
thumb|upright=.90|The Act of the Maryland legislature to ratify the Articles of Confederation, February 2, 1781
On February 2, 1781, the much-awaited decision was taken by the Maryland General Assembly in Annapolis. As the last piece of business during the afternoon Session, "among engrossed Bills" was "signed and sealed by Governor Thomas Sim Lee in the Senate Chamber, in the presence of the members of both Houses ... an Act to empower the delegates of this state in Congress to subscribe and ratify the articles of confederation" and perpetual union among the states. The Senate then adjourned "to the first Monday in August next." The decision of Maryland to ratify the Articles was reported to the Continental Congress on February 12. The confirmation signing of the Articles by the two Maryland delegates took place in Philadelphia at noon time on March 1, 1781, and was celebrated in the afternoon. With these events, the Articles were entered into force and the United States of America came into being as a sovereign federal state.
Congress had debated the Articles for over a year and a half, and the ratification process had taken nearly three and a half years. Many participants in the original debates were no longer delegates, and some of the signers had only recently arrived. The Articles of Confederation and Perpetual Union were signed by a group of men who were never present in the Congress at the same time. |
Articles of Confederation | Signers | Signers
The signers and the states they represented were:
Connecticut
Roger Sherman
Samuel Huntington
Oliver Wolcott
Titus Hosmer
Andrew Adams
Delaware
Thomas McKean
John Dickinson
Nicholas Van Dyke
Georgia
John Walton
Edward Telfair
Edward Langworthy
Maryland
John Hanson
Daniel Carroll
Massachusetts Bay
John Hancock
Samuel Adams
Elbridge Gerry
Francis Dana
James Lovell
Samuel Holten
New Hampshire
Josiah Bartlett
John Wentworth Jr.
New Jersey
John Witherspoon
Nathaniel Scudder
New York
James Duane
Francis Lewis
William Duer
Gouverneur Morris
North Carolina
John Penn
Cornelius Harnett
John Williams
Pennsylvania
Robert Morris
Daniel Roberdeau
Jonathan Bayard Smith
William Clingan
Joseph Reed
Rhode Island and Providence Plantations
William Ellery
Henry Marchant
John Collins
South Carolina
Henry Laurens
William Henry Drayton
John Mathews
Richard Hutson
Thomas Heyward Jr.
Virginia
Richard Henry Lee
John Banister
Thomas Adams
John Harvie
Francis Lightfoot Lee
Roger Sherman (Connecticut) was the only person to sign all four great state papers of the United States: the Continental Association, the United States Declaration of Independence, the Articles of Confederation and the United States Constitution.
Robert Morris (Pennsylvania) signed three of the great state papers of the United States: the United States Declaration of Independence, the Articles of Confederation and the United States Constitution.
John Dickinson (Delaware), Daniel Carroll (Maryland) and Gouverneur Morris (New York), along with Sherman and Robert Morris, were the only five people to sign both the Articles of Confederation and the United States Constitution (Gouverneur Morris represented Pennsylvania when signing the Constitution). |
Articles of Confederation | Parchment pages | Parchment pages
Original parchment pages of the Articles of Confederation, National Archives and Records Administration. |
Articles of Confederation | Revision and replacement | Revision and replacement
In September 1786, delegates from five states met at what became known as the Annapolis Convention to discuss the need for reversing the protectionist interstate trade barriers that each state had erected. At its conclusion, delegates voted to invite all states to a larger convention to be held in Philadelphia in 1787. The Confederation Congress later endorsed this convention "for the sole and express purpose of revising the Articles of Confederation". Although the states' representatives to the Constitutional Convention in Philadelphia were only authorized to amend the Articles, delegates held secret, closed-door sessions and wrote a new constitution. The new frame of government gave much more power to the central government, but characterization of the result is disputed. The general goal of the authors was to get close to a republic as defined by the philosophers of the Age of Enlightenment, while trying to address the many difficulties of the interstate relationships. Historian Forrest McDonald, using the ideas of James Madison from Federalist 39, described the change this way:
In May 1786, Charles Pinckney of South Carolina proposed that Congress revise the Articles of Confederation. Recommended changes included granting Congress power over foreign and domestic commerce, and providing means for Congress to collect money from state treasuries. Unanimous approval was necessary to make the alterations, however, and Congress failed to reach a consensus. The weakness of the Articles in establishing an effective unifying government was underscored by the threat of internal conflict both within and between the states, especially after Shays's Rebellion threatened to topple the state government of Massachusetts.
Historian Ralph Ketcham commented on the opinions of Patrick Henry, George Mason, and other Anti-Federalists who were not so eager to give up the local autonomy won by the revolution:
Historians have given many reasons for the perceived need to replace the articles in 1787. Jillson and Wilson (1994) point to the financial weakness as well as the norms, rules and institutional structures of the Congress, and the propensity to divide along sectional lines.
Rakove identifies several factors that explain the collapse of the Confederation. The lack of compulsory direct taxation power was objectionable to those wanting a strong centralized state or expecting to benefit from such power. It could not collect customs after the war because tariffs were vetoed by Rhode Island. Rakove concludes that their failure to implement national measures "stemmed not from a heady sense of independence but rather from the enormous difficulties that all the states encountered in collecting taxes, mustering men, and gathering supplies from a war-weary populace." The second group of factors Rakove identified derived from the substantive nature of the problems the Continental Congress confronted after 1783, especially the inability to create a strong foreign policy. Finally, the Confederation's lack of coercive power reduced the likelihood for profit to be made by political means, thus potential rulers were uninspired to seek power.
When the war ended in 1783, certain special interests had incentives to create a new "merchant state", much like the British state people had rebelled against. In particular, holders of war scrip and land speculators wanted a central government to pay off scrip at face value and to legalize western land holdings with disputed claims. Also, manufacturers wanted a high tariff as a barrier to foreign goods, but competition among states made this impossible without a central government. |
Articles of Confederation | Legitimacy of closing down | Legitimacy of closing down
Two prominent political leaders in the Confederation, John Jay of New York and Thomas Burke of North Carolina believed that "the authority of the congress rested on the prior acts of the several states, to which the states gave their voluntary consent, and until those obligations were fulfilled, neither nullification of the authority of congress, exercising its due powers, nor secession from the compact itself was consistent with the terms of their original pledges."
According to Article XIII of the Confederation, any alteration had to be approved unanimously:
[T]he Articles of this Confederation shall be inviolably observed by every State, and the Union shall be perpetual; nor shall any alteration at any time hereafter be made in any of them; unless such alteration be agreed to in a Congress of the United States, and be afterwards confirmed by the legislatures of every State.
On the other hand, Article VII of the proposed Constitution stated that it would become effective after ratification by a mere nine states, without unanimity:
The Ratification of the Conventions of nine States, shall be sufficient for the Establishment of this Constitution between the States so ratifying the Same.
The apparent tension between these two provisions was addressed at the time, and remains a topic of scholarly discussion. In 1788, James Madison remarked (in Federalist No. 40) that the issue had become moot: "As this objection ... has been in a manner waived by those who have criticised the powers of the convention, I dismiss it without further observation." Nevertheless, it is a historical and legal question whether opponents of the Constitution could have plausibly attacked the Constitution on that ground. At the time, there were state legislators who argued that the Constitution was not an alteration of the Articles of Confederation, but rather would be a complete replacement so the unanimity rule did not apply. Moreover, the Confederation had proven woefully inadequate and therefore was supposedly no longer binding.
Modern scholars such as Francisco Forrest Martin agree that the Articles of Confederation had lost its binding force because many states had violated it, and thus "other states-parties did not have to comply with the Articles' unanimous consent rule". In contrast, law professor Akhil Amar suggests that there may not have really been any conflict between the Articles of Confederation and the Constitution on this point; Article VI of the Confederation specifically allowed side deals among states, and the Constitution could be viewed as a side deal until all states ratified it. |
Articles of Confederation | Final months | Final months
On July 3, 1788, the Congress received New Hampshire's all-important ninth ratification of the proposed Constitution, thus, according to its terms, establishing it as the new framework of governance for the ratifying states. The following day delegates considered a bill to admit Kentucky into the Union as a sovereign state. The discussion ended with Congress making the determination that, in light of this development, it would be "unadvisable" to admit Kentucky into the Union, as it could do so "under the Articles of Confederation" only, but not "under the Constitution".
By the end of July 1788, 11 of the 13 states had ratified the new Constitution. Congress continued to convene under the Articles with a quorum until October. On Saturday, September 13, 1788, the Confederation Congress voted the resolve to implement the new Constitution, and on Monday, September 15 published an announcement that the new Constitution had been ratified by the necessary nine states, set the first Wednesday in January 1789 for appointing electors, set the first Wednesday in February 1789 for the presidential electors to meet and vote for a new president, and set the first Wednesday of March 1789 as the day "for commencing proceedings" under the new Constitution. On that same September 13, it determined that New York would remain the national capital. |
Articles of Confederation | See also | See also
Court of Appeals in Cases of Capture
Founding Fathers of the United States
Journals of the Continental Congress
History of the United States (1776–1789)
Libertarianism
Perpetual Union
Vetocracy |
Articles of Confederation | Citations | Citations |
Articles of Confederation | General and cited references | General and cited references
(Collection published 1995.)
Rakove, Jack N. (1991) "The Articles of Confederation, 1775–1783. In Jack P. Green and J.R. Pole, eds. The Blackwell Encyclopedia of the American Revolution. Oxford: Blackwell pp. 280–95.
|
Articles of Confederation | External links | External links
Text version of the Articles of Confederation
Articles of Confederation and Perpetual Union
Articles of Confederation and related resources, Library of Congress
Today in History: November 15, Library of Congress
United States Constitution Online—The Articles of Confederation
Free Download of Articles of Confederation Audio
Mobile friendly version of the Articles of Confederation
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Articles of Confederation | Table of Content | Short description, Background and context, Drafting, Ratification, Article summaries, Congress under the Articles, Army, Foreign policy, Taxation and commerce, Accomplishments, Presidents of Congress, U.S. under the Articles, Signatures, Signers, Parchment pages, Revision and replacement, Legitimacy of closing down, Final months, See also, Citations, General and cited references, External links |
Asia Minor (disambiguation) | Wiktionary | Asia Minor is an alternative name for Anatolia, the westernmost protrusion of Asia, comprising the majority of the Republic of Turkey.
Asia Minor may also refer to:
Asia Minor (album), an album by Jamaican-born jazz trumpeter Dizzy Reece
"Asia Minor" (instrumental), a 1961 instrumental recording by Jimmy Wisner (operating under the name Kokomo) |
Asia Minor (disambiguation) | See also | See also
Asia Major (disambiguation) |
Asia Minor (disambiguation) | Table of Content | Wiktionary, See also |
Atlantic Ocean | Short description | thumb|This video was taken by the crew of Expedition 29 on board the ISS. The pass starts from just northeast of the island of Newfoundland over the North Atlantic Ocean to central Africa, over South Sudan.
The Atlantic Ocean is the second largest of the world's five oceanic divisions, with an area of about . It covers approximately 17% of Earth's surface and about 24% of its water surface area. During the Age of Discovery, it was known for separating the New World of the Americas (North America and South America) from the Old World of Afro-Eurasia (Africa, Asia, and Europe).
Through its separation of Afro-Eurasia from the Americas, the Atlantic Ocean has played a central role in the development of human society, globalization, and the histories of many nations. While the Norse were the first known humans to cross the Atlantic, it was the expedition of Christopher Columbus in 1492 that proved to be the most consequential. Columbus' expedition ushered in an age of exploration and colonization of the Americas by European powers, most notably Portugal, Spain, France, and the United Kingdom. From the 16th to 19th centuries, the Atlantic Ocean was the center of both an eponymous slave trade and the Columbian exchange while occasionally hosting naval battles. Such naval battles, as well as growing trade from regional American powers like the United States and Brazil, both increased in degree during the early 20th century, and while no major military conflicts have taken place in the Atlantic recently, the ocean remains a core component of trade around the world.
The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Europe and Africa to the east, and the Americas to the west. As one component of the interconnected World Ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south. Other definitions describe the Atlantic as extending southward to Antarctica. The Atlantic Ocean is divided in two parts, the northern and southern Atlantic, by the Equator.International Hydrographic Organization, Limits of Oceans and Seas, 3rd ed. (1953) , pages 4 and 13. |
Atlantic Ocean | Toponymy | Toponymy
thumb|The Aethiopian Ocean depicted in a 1710 French map of Africa
The oldest known mentions of an "Atlantic" sea come from Stesichorus around mid-sixth century BC (Sch. A. R. 1. 211): (, , . ) and in The Histories of Herodotus around 450 BC (Hdt. 1.202.4): (, or ) where the name refers to "the sea beyond the pillars of Hercules" which is said to be part of the sea that surrounds all land. In these uses, the name refers to Atlas, the Titan in Greek mythology, who supported the heavens and who later appeared as a frontispiece in medieval maps and also lent his name to modern atlases. On the other hand, to early Greek sailors and in ancient Greek mythological literature such as the Iliad and the Odyssey, this all-encompassing ocean was instead known as Oceanus, the gigantic river that encircled the world; in contrast to the enclosed seas well known to the Greeks: the Mediterranean and the Black Sea. In contrast, the term "Atlantic" originally referred specifically to the Atlas Mountains in Morocco and the sea off the Strait of Gibraltar and the West African coast.
The term "Aethiopian Ocean", derived from Ancient Ethiopia, was applied to the southern Atlantic as late as the mid-19th century. During the Age of Discovery, the Atlantic was also known to English cartographers as the Great Western Ocean.
thumb|The Atlantic as seen from the shores of Clare Island, Ireland in 1981.
The pond is a term often used by British and American speakers in reference to the northern Atlantic Ocean, as a form of meiosis, or ironic understatement. It is used mostly when referring to events or circumstances "on this side of the pond" or "on the other side of the pond" or "across the pond", rather than to discuss the ocean itself. The term dates to 1640, first appearing in print in a pamphlet released during the reign of Charles I, and reproduced in 1869 in Nehemiah Wallington's Historical Notices of Events Occurring Chiefly in The Reign of Charles I, where "great Pond" is used in reference to the Atlantic Ocean by Francis Windebank, Charles I's Secretary of State. |
Atlantic Ocean | Extent and data | Extent and data
The International Hydrographic Organization (IHO) defined the limits of the oceans and seas in 1953, but some of these definitions have been revised since then and some are not recognized by various authorities, institutions, and countries, for example the CIA World Factbook. Correspondingly, the extent and number of oceans and seas vary.
The Atlantic Ocean is bounded on the west by North and South America. It connects to the Arctic Ocean through the Labrador Sea, Denmark Strait, Greenland Sea, Norwegian Sea and Barents Sea with the northern divider passing through Iceland and Svalbard. To the east, the boundaries of the ocean proper are Europe and Africa: the Strait of Gibraltar (where it connects with the Mediterranean Seaone of its marginal seasand, in turn, the Black Sea, both of which also touch upon Asia).
In the southeast, the Atlantic merges into the Indian Ocean. The 20° East meridian, running south from Cape Agulhas to Antarctica defines its border. In the 1953 definition it extends south to Antarctica, while in later maps it is bounded at the 60° parallel by the Southern Ocean.
The Atlantic has irregular coasts indented by numerous bays, gulfs and seas. These include the Baltic Sea, Black Sea, Caribbean Sea, Davis Strait, Denmark Strait, part of the Drake Passage, Gulf of Mexico, Labrador Sea, Mediterranean Sea, North Sea, Norwegian Sea, almost all of the Scotia Sea, and other tributary water bodies. Including these marginal seas the coast line of the Atlantic measures compared to for the Pacific.
Including its marginal seas, the Atlantic covers an area of or 23.5% of the global ocean and has a volume of or 23.3% of the total volume of the Earth's oceans. Excluding its marginal seas, the Atlantic covers and has a volume of . The North Atlantic covers (11.5%) and the South Atlantic (11.1%). The average depth is and the maximum depth, the Milwaukee Deep in the Puerto Rico Trench, is . |
Atlantic Ocean | Biggest seas in Atlantic Ocean | Biggest seas in Atlantic Ocean
Top large seas:
Sargasso Sea3.5 million km2
Caribbean Sea2.754 million km2
Mediterranean Sea2.510 million km2
Gulf of Guinea2.35 million km2
Gulf of Mexico1.550 million km2
Norwegian Sea1.383 million km2
Greenland Sea1.205 million km2
Argentine Sea1 million km2
Labrador Sea841,000 km2
Irminger Sea780,000 km2
Baffin Bay689,000 km2
North Sea575,000 km2
Black Sea436,000 km2
Baltic Sea377,000 km2
Libyan Sea350,000 km2
Levantine Sea320,000 km2
Celtic Sea300,000 km2
Tyrrhenian Sea275,000 km2
Gulf of Saint Lawrence226,000 km2
Bay of Biscay223,000 km2
Aegean Sea214,000 km2
Ionian Sea169,000 km2
Balearic Sea150,000 km2
Adriatic Sea138,000 km2
Gulf of Bothnia116,300 km2
Sea of Crete95,000 km2
Gulf of Maine93,000 km2
Ligurian Sea80,000 km2
English Channel75,000 km2
James Bay68,300 km2
Bothnian Sea66,000 km2
Gulf of Sidra57,000 km2
Sea of the Hebrides47,000 km2
Irish Sea46,000 km2
Sea of Azov39,000 km2
Bothnian Bay36,800 km2
Gulf of Venezuela17,840 km2
Bay of Campeche16,000 km2
Gulf of Lion15,000 km2
Sea of Marmara11,350 km2
Wadden Sea10,000 km2
Archipelago Sea8,300 km2 |
Atlantic Ocean | Bathymetry | Bathymetry
thumb|False color map of ocean depth in the Atlantic basin
The bathymetry of the Atlantic is dominated by a submarine mountain range called the Mid-Atlantic Ridge (MAR). It runs from 87°N or south of the North Pole to the subantarctic Bouvet Island at 54°S. Expeditions to explore the bathymertry of the Atlantic include the Challenger expedition and the German Meteor expedition; , Columbia University's Lamont–Doherty Earth Observatory and the United States Navy Hydrographic Office conduct research on the ocean. |
Atlantic Ocean | Mid-Atlantic Ridge | Mid-Atlantic Ridge
The MAR divides the Atlantic longitudinally into two halves, in each of which a series of basins are delimited by secondary, transverse ridges. The MAR reaches above along most of its length, but is interrupted by larger transform faults at two places: the Romanche Trench near the Equator and the Gibbs fracture zone at 53°N. The MAR is a barrier for bottom water, but at these two transform faults deep water currents can pass from one side to the other.
The MAR rises above the surrounding ocean floor and its rift valley is the divergent boundary between the North American and Eurasian plates in the North Atlantic and the South American and African plates in the South Atlantic. The MAR produces basaltic volcanoes in Eyjafjallajökull, Iceland, and pillow lava on the ocean floor. The depth of water at the apex of the ridge is less than in most places, while the bottom of the ridge is three times as deep.
The MAR is intersected by two perpendicular ridges: the Azores–Gibraltar transform fault, the boundary between the Nubian and Eurasian plates, intersects the MAR at the Azores triple junction, on either side of the Azores microplate, near the 40°N. A much vaguer, nameless boundary, between the North American and South American plates, intersects the MAR near or just north of the Fifteen-Twenty fracture zone, approximately at 16°N.
In the 1870s, the Challenger expedition discovered parts of what is now known as the Mid-Atlantic Ridge, or:
The remainder of the ridge was discovered in the 1920s by the German Meteor expedition using echo-sounding equipment. The exploration of the MAR in the 1950s led to the general acceptance of seafloor spreading and plate tectonics.
Most of the MAR runs under water but where it reaches the surfaces it has produced volcanic islands. While nine of these have collectively been nominated a World Heritage Site for their geological value, four of them are considered of "Outstanding Universal Value" based on their cultural and natural criteria: Þingvellir, Iceland; Landscape of the Pico Island Vineyard Culture, Portugal; Gough and Inaccessible Islands, United Kingdom; and Brazilian Atlantic Islands: Fernando de Noronha and Atol das Rocas Reserves, Brazil. |
Atlantic Ocean | Ocean floor | Ocean floor
Continental shelves in the Atlantic are wide off Newfoundland, southernmost South America, and northeastern Europe.
In the western Atlantic carbonate platforms dominate large areas, for example, the Blake Plateau and Bermuda Rise.
The Atlantic is surrounded by passive margins except at a few locations where active margins form deep trenches: the Puerto Rico Trench ( maximum depth) in the western Atlantic and South Sandwich Trench () in the South Atlantic. There are numerous submarine canyons off northeastern North America, western Europe, and northwestern Africa. Some of these canyons extend along the continental rises and farther into the abyssal plains as deep-sea channels.
In 1922, a historic moment in cartography and oceanography occurred. The USS Stewart used a Navy Sonic Depth Finder to draw a continuous map across the bed of the Atlantic. This involved little guesswork because the idea of sonar is straightforward with pulses being sent from the vessel, which bounce off the ocean floor, then return to the vessel. The deep ocean floor is thought to be fairly flat with occasional deeps, abyssal plains, trenches, seamounts, basins, plateaus, canyons, and some guyots. Various shelves along the margins of the continents constitute about 11% of the bottom topography with few deep channels cut across the continental rise.
The mean depth between 60°N and 60°S is , or close to the average for the global ocean, with a modal depth between .
In the South Atlantic the Walvis Ridge and Rio Grande Rise form barriers to ocean currents.
The Laurentian Abyss is found off the eastern coast of Canada. |
Atlantic Ocean | Water characteristics | Water characteristics
thumb|upright=1.8|As the Gulf Stream meanders across the North Atlantic from the North American east coast to Western Europe its temperature drops by .|alt=Visualisation of the Gulf Stream stretching from the Gulf of Mexico to Western Europe
Path of the thermohaline circulation. Purple paths represent deep-water currents, while blue paths represent surface currents.|thumb|alt=Map displaying a looping line with arrows indicating that water flows eastward in the far Southern Ocean, angling northeast of Australia, turning sough-after passing Alaska, then crossing the mid-Pacific to flow north of Australia, continuing west below Africa, then turning northwest until reaching eastern Canada, then angling east to southern Europe, then finally turning south just below Greenland and flowing down the Americas' eastern coast, and resuming its flow eastward to complete the circle
Surface water temperatures, which vary with latitude, current systems, and season and reflect the latitudinal distribution of solar energy, range from below to over . Maximum temperatures occur north of the equator, and minimum values are found in the polar regions. In the middle latitudes, the area of maximum temperature variations, values may vary by .
From October to June the surface is usually covered with sea ice in the Labrador Sea, Denmark Strait, and Baltic Sea.
The Coriolis effect circulates North Atlantic water in a clockwise direction, whereas South Atlantic water circulates counter-clockwise. The south tides in the Atlantic Ocean are semi-diurnal; that is, two high tides occur every 24 lunar hours. In latitudes above 40° North some east–west oscillation, known as the North Atlantic oscillation, occurs. |
Atlantic Ocean | Salinity | Salinity
On average, the Atlantic is the saltiest major ocean; surface water salinity in the open ocean ranges from 33 to 37 parts per thousand (3.3–3.7%) by mass and varies with latitude and season. Evaporation, precipitation, river inflow and sea ice melting influence surface salinity values. Although the lowest salinity values are just north of the equator (because of heavy tropical rainfall), in general, the lowest values are in the high latitudes and along coasts where large rivers enter. Maximum salinity values occur at about 25° north and south, in subtropical regions with low rainfall and high evaporation.
The high surface salinity in the Atlantic, on which the Atlantic thermohaline circulation is dependent, is maintained by two processes: the Agulhas Leakage/Rings, which brings salty Indian Ocean waters into the South Atlantic, and the "Atmospheric Bridge", which evaporates subtropical Atlantic waters and exports it to the Pacific. |
Atlantic Ocean | Water masses | Water masses
+ Temperature-salinity characteristics for Atlantic water masses Water mass Temperature Salinity Upper waters () Atlantic SubarcticUpper Water (ASUW) 0.0–4.0 °C 34.0–35.0 Western North AtlanticCentral Water (WNACW) 7.0–20 °C 35.0–36.7 Eastern North AtlanticCentral Water (ENACW) 8.0–18.0 °C 35.2–36.7 South AtlanticCentral Water (SACW) 5.0–18.0 °C 34.3–35.8 Intermediate waters () Western Atlantic SubarcticIntermediate Water (WASIW) 3.0–9.0 °C 34.0–35.1 Eastern Atlantic SubarcticIntermediate Water (EASIW) 3.0–9.0 °C 34.4–35.3 Mediterranean Water (MW) 2.6–11.0 °C 35.0–36.2 Arctic Intermediate Water (AIW) −1.5–3.0 °C 34.7–34.9 Deep and abyssal waters (1,500 m–bottom or 4,900 ft–bottom) North AtlanticDeep Water (NADW) 1.5–4.0 °C 34.8–35.0 Antarctic Bottom Water (AABW) −0.9–1.7 °C 34.6–34.7 Arctic Bottom Water (ABW) −1.8 to −0.5 °C 34.9–34.9
The Atlantic Ocean consists of four major, upper water masses with distinct temperature and salinity. The Atlantic subarctic upper water in the northernmost North Atlantic is the source for subarctic intermediate water and North Atlantic intermediate water. North Atlantic central water can be divided into the eastern and western North Atlantic central water since the western part is strongly affected by the Gulf Stream and therefore the upper layer is closer to underlying fresher subpolar intermediate water. The eastern water is saltier because of its proximity to Mediterranean water. North Atlantic central water flows into South Atlantic central water at 15°N.
There are five intermediate waters: four low-salinity waters formed at subpolar latitudes and one high-salinity formed through evaporation. Arctic intermediate water flows from the north to become the source for North Atlantic deep water, south of the Greenland-Scotland sill. These two intermediate waters have different salinity in the western and eastern basins. The wide range of salinities in the North Atlantic is caused by the asymmetry of the northern subtropical gyre and a large number of contributions from a wide range of sources: Labrador Sea, Norwegian-Greenland Sea, Mediterranean, and South Atlantic Intermediate Water.
The North Atlantic deep water (NADW) is a complex of four water masses, two that form by deep convection in the open oceanclassical and upper Labrador sea waterand two that form from the inflow of dense water across the Greenland-Iceland-Scotland sillDenmark Strait and Iceland-Scotland overflow water. Along its path across Earth the composition of the NADW is affected by other water masses, especially Antarctic bottom water and Mediterranean overflow water.
The NADW is fed by a flow of warm shallow water into the northern North Atlantic which is responsible for the anomalous warm climate in Europe. Changes in the formation of NADW have been linked to global climate changes in the past. Since human-made substances were introduced into the environment, the path of the NADW can be traced throughout its course by measuring tritium and radiocarbon from nuclear weapon tests in the 1960s and CFCs. |
Atlantic Ocean | Gyres | Gyres
The clockwise warm-water North Atlantic Gyre occupies the northern Atlantic, and the counter-clockwise warm-water South Atlantic Gyre appears in the southern Atlantic.
In the North Atlantic, surface circulation is dominated by three inter-connected currents: the Gulf Stream which flows north-east from the North American coast at Cape Hatteras; the North Atlantic Current, a branch of the Gulf Stream which flows northward from the Grand Banks; and the Subpolar Front, an extension of the North Atlantic Current, a wide, vaguely defined region separating the subtropical gyre from the subpolar gyre. This system of currents transports warm water into the North Atlantic, without which temperatures in the North Atlantic and Europe would plunge dramatically.
thumb|In the subpolar gyre of the North Atlantic warm subtropical waters are transformed into colder subpolar and polar waters. In the Labrador Sea this water flows back to the subtropical gyre.
North of the North Atlantic Gyre, the cyclonic North Atlantic Subpolar Gyre plays a key role in climate variability. It is governed by ocean currents from marginal seas and regional topography, rather than being steered by wind, both in the deep ocean and at sea level.
The subpolar gyre forms an important part of the global thermohaline circulation. Its eastern portion includes eddying branches of the North Atlantic Current which transport warm, saline waters from the subtropics to the northeastern Atlantic. There this water is cooled during winter and forms return currents that merge along the eastern continental slope of Greenland where they form an intense (40–50 Sv) current which flows around the continental margins of the Labrador Sea. A third of this water becomes part of the deep portion of the North Atlantic Deep Water (NADW). The NADW, in turn, feeds the meridional overturning circulation (MOC), the northward heat transport of which is threatened by anthropogenic climate change. Large variations in the subpolar gyre on a decade-century scale, associated with the North Atlantic oscillation, are especially pronounced in Labrador Sea Water, the upper layers of the MOC.
The South Atlantic is dominated by the anti-cyclonic southern subtropical gyre. The South Atlantic Central Water originates in this gyre, while Antarctic Intermediate Water originates in the upper layers of the circumpolar region, near the Drake Passage and the Falkland Islands. Both these currents receive some contribution from the Indian Ocean. On the African east coast, the small cyclonic Angola Gyre lies embedded in the large subtropical gyre.
The southern subtropical gyre is partly masked by a wind-induced Ekman layer. The residence time of the gyre is 4.4–8.5 years. North Atlantic Deep Water flows southward below the thermocline of the subtropical gyre. |
Atlantic Ocean | Sargasso Sea | Sargasso Sea
The Sargasso Sea in the western North Atlantic can be defined as the area where two species of Sargassum (S. fluitans and natans) float, an area wide and encircled by the Gulf Stream, North Atlantic Drift, and North Equatorial Current. This population of seaweed probably originated from Tertiary ancestors on the European shores of the former Tethys Ocean and has, if so, maintained itself by vegetative growth, floating in the ocean for millions of years.
Other species endemic to the Sargasso Sea include the sargassum fish, a predator with algae-like appendages which hovers motionless among the Sargassum. Fossils of similar fishes have been found in fossil bays of the former Tethys Ocean, in what is now the Carpathian region, that were similar to the Sargasso Sea. It is possible that the population in the Sargasso Sea migrated to the Atlantic as the Tethys closed at the end of the Miocene around 17 Ma. The origin of the Sargasso fauna and flora remained enigmatic for centuries. The fossils found in the Carpathians in the mid-20th century often called the "quasi-Sargasso assemblage", finally showed that this assemblage originated in the Carpathian Basin from where it migrated over Sicily to the central Atlantic where it evolved into modern species of the Sargasso Sea.
The location of the spawning ground for European eels remained unknown for decades. In the early 19th century it was discovered that the southern Sargasso Sea is the spawning ground for both the European and American eel and that the former migrate more than and the latter . Ocean currents such as the Gulf Stream transport eel larvae from the Sargasso Sea to foraging areas in North America, Europe, and northern Africa. Recent but disputed research suggests that eels possibly use Earth's magnetic field to navigate through the ocean both as larvae and as adults. |
Atlantic Ocean | Climate | Climate
thumb|Waves in the trade winds in the Atlantic Oceanareas of converging winds that move along the same track as the prevailing windcreate instabilities in the atmosphere that may lead to the formation of hurricanes.|alt=Map of Caribbean showing seven approximately parallel westward-pointing arrows that extend from east of the Virgin Islands to Cuba. The southern arrows bend northward just east of the Dominican Republic before straightening out again.
The climate is influenced by the temperatures of the surface waters and water currents as well as winds. Because of the ocean's great capacity to store and release heat, maritime climates are more moderate and have less extreme seasonal variations than inland climates. Precipitation can be approximated from coastal weather data and air temperature from water temperatures.
The oceans are the major source of atmospheric moisture that is obtained through evaporation. Climatic zones vary with latitude; the warmest zones stretch across the Atlantic north of the equator. The coldest zones are in high latitudes, with the coldest regions corresponding to the areas covered by sea ice. Ocean currents influence the climate by transporting warm and cold waters to other regions. The winds that are cooled or warmed when blowing over these currents influence adjacent land areas.
The Gulf Stream and its northern extension towards Europe, the North Atlantic Drift is thought to have at least some influence on climate. For example, the Gulf Stream helps moderate winter temperatures along the coastline of southeastern North America, keeping it warmer in winter along the coast than inland areas. The Gulf Stream also keeps extreme temperatures from occurring on the Florida Peninsula. In the higher latitudes, the North Atlantic Drift, warms the atmosphere over the oceans, keeping the British Isles and northwestern Europe mild and cloudy, and not severely cold in winter, like other locations at the same high latitude. The cold water currents contribute to heavy fog off the coast of eastern Canada (the Grand Banks of Newfoundland area) and Africa's northwestern coast. In general, winds transport moisture and air over land areas. |
Atlantic Ocean | Natural hazards | Natural hazards
thumb|Iceberg A22A in the South Atlantic Ocean
Every winter, the Icelandic Low produces frequent storms. Icebergs are common from early February to the end of July across the shipping lanes near the Grand Banks of Newfoundland. The ice season is longer in the polar regions, but there is little shipping in those areas.
Hurricanes are a hazard in the western parts of the North Atlantic during the summer and autumn. Due to a consistently strong wind shear and a weak Intertropical Convergence Zone, South Atlantic tropical cyclones are rare. |
Atlantic Ocean | Geology and plate tectonics | Geology and plate tectonics
The Atlantic Ocean is underlain mostly by dense mafic oceanic crust made up of basalt and gabbro and overlain by fine clay, silt and siliceous ooze on the abyssal plain. The continental margins and continental shelf mark lower density, but greater thickness felsic continental rock that is often much older than that of the seafloor. The oldest oceanic crust in the Atlantic is up to 145 million years and is situated off the west coast of Africa and the east coast of North America, or on either side of the South Atlantic.
In many places, the continental shelf and continental slope are covered in thick sedimentary layers. For instance, on the North American side of the ocean, large carbonate deposits formed in warm shallow waters such as Florida and the Bahamas, while coarse river outwash sands and silt are common in shallow shelf areas like the Georges Bank. Coarse sand, boulders, and rocks were transported into some areas, such as off the coast of Nova Scotia or the Gulf of Maine during the Pleistocene ice ages. |
Atlantic Ocean | Central Atlantic | Central Atlantic
The break-up of Pangaea began in the central Atlantic, between North America and Northwest Africa, where rift basins opened during the Late Triassic and Early Jurassic. This period also saw the first stages of the uplift of the Atlas Mountains. The exact timing is controversial with estimates ranging from 200 to 170 Ma.
The opening of the Atlantic Ocean coincided with the initial break-up of the supercontinent Pangaea, both of which were initiated by the eruption of the Central Atlantic Magmatic Province (CAMP), one of the most extensive and voluminous large igneous provinces in Earth's history associated with the Triassic–Jurassic extinction event, one of Earth's major extinction events.
Theoliitic dikes, sills, and lava flows from the CAMP eruption at 200 Ma have been found in West Africa, eastern North America, and northern South America. The extent of the volcanism has been estimated to of which covered what is now northern and central Brazil.
The formation of the Central American Isthmus closed the Central American Seaway at the end of the Pliocene 2.8 Ma ago. The formation of the isthmus resulted in the migration and extinction of many land-living animals, known as the Great American Interchange, but the closure of the seaway resulted in a "Great American Schism" as it affected ocean currents, salinity, and temperatures in both the Atlantic and Pacific. Marine organisms on both sides of the isthmus became isolated and either diverged or went extinct. |
Atlantic Ocean | North Atlantic | North Atlantic
Geologically, the North Atlantic is the area delimited to the south by two conjugate margins, Newfoundland and Iberia, and to the north by the Arctic Eurasian Basin. The opening of the North Atlantic closely followed the margins of its predecessor, the Iapetus Ocean, and spread from the central Atlantic in six stages: Iberia–Newfoundland, Porcupine–North America, Eurasia–Greenland, Eurasia–North America. Active and inactive spreading systems in this area are marked by the interaction with the Iceland hotspot.
Seafloor spreading led to the extension of the crust and the formation of troughs and sedimentary basins. The Rockall Trough opened between 105 and 84 million years ago although the rift failed along with one leading into the Bay of Biscay.
Spreading began opening the Labrador Sea around 61 million years ago, continuing until 36 million years ago. Geologists distinguish two magmatic phases. One from 62 to 58 million years ago predates the separation of Greenland from northern Europe while the second from 56 to 52 million years ago happened as the separation occurred.
Iceland began to form 62 million years ago due to a particularly concentrated mantle plume. Large quantities of basalt erupted at this time period are found on Baffin Island, Greenland, the Faroe Islands, and Scotland, with ash falls in Western Europe acting as a stratigraphic marker. The opening of the North Atlantic caused a significant uplift of continental crust along the coast. For instance, despite 7 km thick basalt, Gunnbjorn Field in East Greenland is the highest point on the island, elevated enough that it exposes older Mesozoic sedimentary rocks at its base, similar to old lava fields above sedimentary rocks in the uplifted Hebrides of western Scotland.
The North Atlantic Ocean contains about 810 seamounts, most of them situated along the Mid-Atlantic Ridge.Gubbay S. 2003. Seamounts of the northeast Atlantic. OASIS (Oceanic Seamounts: an Integrated Study). Hamburg & WWF, Frankfurt am Main, Germany The OSPAR database (Convention for the Protection of the Marine Environment of the North-East Atlantic) mentions 104 seamounts: 74 within national exclusive economic zones. Of these seamounts, 46 are located close to the Iberian Peninsula. |
Atlantic Ocean | South Atlantic | South Atlantic
West Gondwana (South America and Africa) broke up in the Early Cretaceous to form the South Atlantic. The apparent fit between the coastlines of the two continents was noted on the first maps that included the South Atlantic and it was also the subject of the first computer-assisted plate tectonic reconstructions in 1965. This magnificent fit, however, has since then proven problematic and later reconstructions have introduced various deformation zones along the shorelines to accommodate the northward-propagating break-up. Intra-continental rifts and deformations have also been introduced to subdivide both continental plates into sub-plates.
Geologically, the South Atlantic can be divided into four segments: equatorial segment, from 10°N to the Romanche fracture zone (RFZ); central segment, from RFZ to Florianopolis fracture zone (FFZ, north of Walvis Ridge and Rio Grande Rise); southern segment, from FFZ to the Agulhas–Falkland fracture zone (AFFZ); and Falkland segment, south of AFFZ.
In the southern segment the Early Cretaceous (133–130 Ma) intensive magmatism of the Paraná–Etendeka Large Igneous Province produced by the Tristan hotspot resulted in an estimated volume of . It covered an area of in Brazil, Paraguay, and Uruguay and in Africa. Dyke swarms in Brazil, Angola, eastern Paraguay, and Namibia, however, suggest the LIP originally covered a much larger area and also indicate failed rifts in all these areas. Associated offshore basaltic flows reach as far south as the Falkland Islands and South Africa. Traces of magmatism in both offshore and onshore basins in the central and southern segments have been dated to 147–49 Ma with two peaks between 143 and 121 Ma and 90–60 Ma.
In the Falkland segment rifting began with dextral movements between the Patagonia and Colorado sub-plates between the Early Jurassic (190 Ma) and the Early Cretaceous (126.7 Ma). Around 150 Ma sea-floor spreading propagated northward into the southern segment. No later than 130 Ma rifting had reached the Walvis Ridge–Rio Grande Rise.
In the central segment, rifting started to break Africa in two by opening the Benue Trough around 118 Ma. Rifting in the central segment, however, coincided with the Cretaceous Normal Superchron (also known as the Cretaceous quiet period), a 40 Ma period without magnetic reversals, which makes it difficult to date sea-floor spreading in this segment.
The equatorial segment is the last phase of the break-up, but, because it is located on the Equator, magnetic anomalies cannot be used for dating. Various estimates date the propagation of seafloor spreading in this segment and consequent opening of the Equatorial Atlantic Gateway (EAG) to the period 120–96 Ma. This final stage, nevertheless, coincided with or resulted in the end of continental extension in Africa.
About 50 Ma the opening of the Drake Passage resulted from a change in the motions and separation rate of the South American and Antarctic plates. First, small ocean basins opened and a shallow gateway appeared during the Middle Eocene. 34–30 Ma a deeper seaway developed, followed by an Eocene–Oligocene climatic deterioration and the growth of the Antarctic ice sheet. |
Atlantic Ocean | Closure of the Atlantic | Closure of the Atlantic
An embryonic subduction margin is potentially developing west of Gibraltar. The Gibraltar Arc in the western Mediterranean is migrating westward into the central Atlantic where it joins the converging African and Eurasian plates. Together these three tectonic forces are slowly developing into a new subduction system in the eastern Atlantic Basin. Meanwhile, the Scotia Arc and Caribbean plate in the western Atlantic Basin are eastward-propagating subduction systems that might, together with the Gibraltar system, represent the beginning of the closure of the Atlantic Ocean and the final stage of the Atlantic Wilson cycle. |
Atlantic Ocean | History | History |
Atlantic Ocean | Old World | Old World
Mitochondrial DNA (mtDNA) studies indicate that 80–60,000 years ago a major demographic expansion within Africa, derived from a single, small population, coincided with the emergence of behavioral complexity and the rapid MIS 5–4 environmental changes. This group of people not only expanded over the whole of Africa, but also started to disperse out of Africa into Asia, Europe, and Australasia around 65,000 years ago and quickly replaced the archaic humans in these regions. During the Last Glacial Maximum (LGM) 20,000 years ago humans had to abandon their initial settlements along the European North Atlantic coast and retreat to the Mediterranean. Following rapid climate changes at the end of the LGM this region was repopulated by Magdalenian culture. Other hunter-gatherers followed in waves interrupted by large-scale hazards such as the Laacher See volcanic eruption, the inundation of Doggerland (now the North Sea), and the formation of the Baltic Sea. The European coasts of the North Atlantic were permanently populated about 9–8.5 thousand years ago.
This human dispersal left abundant traces along the coasts of the Atlantic Ocean. 50 kya-old, deeply stratified shell middens found in Ysterfontein on the western coast of South Africa are associated with the Middle Stone Age (MSA). The MSA population was small and dispersed and the rate of their reproduction and exploitation was less intense than those of later generations. While their middens resemble 12–11 kya-old Late Stone Age (LSA) middens found on every inhabited continent, the 50–45 kya-old Enkapune Ya Muto in Kenya probably represents the oldest traces of the first modern humans to disperse out of Africa.
thumb|Excavation of the Ertebølle middens in 1880
The same development can be seen in Europe. In La Riera Cave (23–13 kya) in Asturias, Spain, only some 26,600 molluscs were deposited over 10 kya. In contrast, 8–7 kya-old shell middens in Portugal, Denmark, and Brazil generated thousands of tons of debris and artefacts. The Ertebølle middens in Denmark, for example, accumulated of shell deposits representing some 50 million molluscs over only a thousand years. This intensification in the exploitation of marine resources has been described as accompanied by new technologiessuch as boats, harpoons, and fish hooks because many caves found in the Mediterranean and on the European Atlantic coast have increased quantities of marine shells in their upper levels and reduced quantities in their lower. The earliest exploitation, however, took place on the now submerged shelves, and most settlements now excavated were then located several kilometers from these shelves. The reduced quantities of shells in the lower levels can represent the few shells that were exported inland. |
Atlantic Ocean | New World | New World
During the LGM the Laurentide Ice Sheet covered most of northern North America while Beringia connected Siberia to Alaska. In 1973, late American geoscientist Paul S. Martin proposed a "blitzkrieg" colonization of the Americas by which Clovis hunters migrated into North America around 13,000 years ago in a single wave through an ice-free corridor in the ice sheet and "spread southward explosively, briefly attaining a density sufficiently large to overkill much of their prey." Others later proposed a "three-wave" migration over the Bering Land Bridge. These hypotheses remained the long-held view regarding the settlement of the Americas, a view challenged by more recent archaeological discoveries: the oldest archaeological sites in the Americas have been found in South America; sites in northeast Siberia report virtually no human presence there during the LGM; and most Clovis artefacts have been found in eastern North America along the Atlantic coast. Furthermore, colonisation models based on mtDNA, yDNA, and atDNA data respectively support neither the "blitzkrieg" nor the "three-wave" hypotheses but they also deliver mutually ambiguous results. Contradictory data from archaeology and genetics will most likely deliver future hypotheses that will, eventually, confirm each other. A proposed route across the Pacific to South America could explain early South American finds and another hypothesis proposes a northern path, through the Canadian Arctic and down the North American Atlantic coast.
Early settlements across the Atlantic have been suggested by alternative theories, ranging from purely hypothetical to mostly disputed, including the Solutrean hypothesis and some of the Pre-Columbian trans-oceanic contact theories.
thumb|Based on the medieval sagas, including the Grœnlendinga saga, this interpretative map of the "Norse World" shows that Norse knowledge of the Americas and the Atlantic remained limited.
The Norse settlement of the Faroe Islands and Iceland began during the 9th and 10th centuries. A settlement on Greenland was established before 1000 CE, but contact with it was lost in 1409 and it was finally abandoned during the early Little Ice Age. This setback was caused by a range of factors: an unsustainable economy resulted in erosion and denudation, while conflicts with the local Inuit resulted in the failure to adapt their Arctic technologies; a colder climate resulted in starvation, and the colony got economically marginalized as the Great Plague harvested its victims on Iceland in the 15th century.
Iceland was initially settled 865–930 CE following a warm period when winter temperatures hovered around which made farming favorable at high latitudes. This did not last, however, and temperatures quickly dropped; at 1080 CE summer temperatures had reached a maximum of . The (Book of Settlement) records disastrous famines during the first century of settlement"men ate foxes and ravens" and "the old and helpless were killed and thrown over cliffs"and by the early 1200s hay had to be abandoned for short-season crops such as barley. |
Atlantic Ocean | Atlantic World | Atlantic World
thumb|left|The Atlantic Gyres influenced the Portuguese discoveries and trading port routes, here shown in the India Run ("Carreira da Índia"), which would be developed in subsequent years.
Christopher Columbus reached the Americas in 1492, sailing under the Spanish flag. Six years later Vasco da Gama reached India under the Portuguese flag, by navigating south around the Cape of Good Hope, thus proving that the Atlantic and Indian Oceans are connected. In 1500, in his voyage to India following Vasco da Gama, Pedro Álvares Cabral reached Brazil, taken by the currents of the South Atlantic Gyre. Following these explorations, Spain and Portugal quickly conquered and colonized large territories in the New World and forced the Amerindian population into slavery in order to exploit the vast quantities of silver and gold they found. Spain and Portugal monopolized this trade in order to keep other European nations out, but conflicting interests nevertheless led to a series of Spanish-Portuguese wars. A peace treaty mediated by the Pope divided the conquered territories into Spanish and Portuguese sectors while keeping other colonial powers away. England, France, and the Dutch Republic enviously watched the Spanish and Portuguese wealth grow and allied themselves with pirates such as Henry Mainwaring and Alexandre Exquemelin. They could explore the convoys leaving the Americas because prevailing winds and currents made the transport of heavy metals slow and predictable.
thumb|Embarked and disembarked slaves in the Atlantic slave trade 1525–1863 (first and last slave voyages)
In the colonies of the Americas, depredation, smallpox and other diseases, and slavery quickly reduced the indigenous population of the Americas to the extent that the Atlantic slave trade was introduced by colonists to replace thema trade that became the norm and an integral part of the colonization. Between the 15th century and 1888, when Brazil became the last part of the Americas to end the slave trade, an estimated 9.5 million enslaved Africans were shipped into the New World, most of them destined for agricultural labor. The slave trade was officially abolished in the British Empire and the United States in 1808, and slavery itself was abolished in the British Empire in 1838 and in the United States in 1865 after the Civil War.
From Columbus to the Industrial Revolution trans-Atlantic trade, including colonialism and slavery, became crucial for Western Europe. For European countries with direct access to the Atlantic (including Britain, France, the Netherlands, Portugal, and Spain) 1500–1800 was a period of sustained growth during which these countries grew richer than those in Eastern Europe and Asia. Colonialism evolved as part of the trans-Atlantic trade, but this trade also strengthened the position of merchant groups at the expense of monarchs. Growth was more rapid in non-absolutist countries, such as Britain and the Netherlands, and more limited in absolutist monarchies, such as Portugal, Spain, and France, where profit mostly or exclusively benefited the monarchy and its allies.
Trans-Atlantic trade also resulted in increasing urbanization: in European countries facing the Atlantic, urbanization grew from 8% in 1300, 10.1% in 1500, to 24.5% in 1850; in other European countries from 10% in 1300, 11.4% in 1500, to 17% in 1850. Likewise, GDP doubled in Atlantic countries but rose by only 30% in the rest of Europe. By the end of the 17th century, the volume of the Trans-Atlantic trade had surpassed that of the Mediterranean trade. |
Atlantic Ocean | Economy | Economy
The Atlantic has contributed significantly to the development and economy of surrounding countries. Besides major transatlantic transportation and communication routes, the Atlantic offers abundant petroleum deposits in the sedimentary rocks of the continental shelves.
thumb|right|Cod fishery in Norway
The Atlantic harbors petroleum and gas fields, fish, marine mammals (seals and whales), sand and gravel aggregates, placer deposits, polymetallic nodules, and precious stones.
Gold deposits are a mile or two underwater on the ocean floor, however, the deposits are also encased in rock that must be mined through. Currently, there is no cost-effective way to mine or extract gold from the ocean to make a profit.
Various international treaties attempt to reduce pollution caused by environmental threats such as oil spills, marine debris, and the incineration of toxic wastes at sea. |
Atlantic Ocean | Fisheries | Fisheries
The shelves of the Atlantic hosts one of the world's richest fishing resources. The most productive areas include the Grand Banks of Newfoundland, the Scotian Shelf, Georges Bank off Cape Cod, the Bahama Banks, the waters around Iceland, the Irish Sea, the Bay of Fundy, the Dogger Bank of the North Sea, and the Falkland Banks.
Fisheries have, however, undergone significant changes since the 1950s and global catches can now be divided into three groups of which only two are observed in the Atlantic: fisheries in the eastern-central and southwest Atlantic oscillate around a globally stable value, the rest of the Atlantic is in overall decline following historical peaks. The third group, "continuously increasing trend since 1950", is only found in the Indian Ocean and western Pacific.
UN FAO partitioned the Atlantic into major fishing areas:
thumb|Banks of the northeast Atlantic
Northeast Atlantic
Northeast Atlantic is schematically limited to the 40°00' west longitude (except around Greenland), south to the 36°00' north latitude, and to the 68°30' east longitude, with both the west and east longitude limits reaching to the north pole. The Atlantic's subareas include: Barents Sea; Norwegian Sea, Spitzbergen, and Bear Island; Skagerrak, Kattegat, Sound, Belt Sea, and Baltic Sea; North Sea; Iceland and Faroes Grounds; Rockall, Northwest Coast of Scotland, and North Ireland; Irish Sea, West of Ireland, Porcupine Bank, and eastern and western English Channel; Bay of Biscay; Portuguese Waters; Azores Grounds and Northeast Atlantic South; North of Azores; and East Greenland. There are also two defunct subareas.
In the Northeast Atlantic total catches decreased between the mid-1970s and the 1990s and reached 8.7 million tons in 2013. Blue whiting reached a 2.4 million tons peak in 2004 but was down to 628,000 tons in 2013. Recovery plans for cod, sole, and plaice have reduced mortality in these species. Arctic cod reached its lowest levels in the 1960s–1980s but is now recovered. Arctic saithe and haddock are considered fully fished; Sand eel is overfished as was capelin which has now recovered to fully fished. Limited data makes the state of redfishes and deep-water species difficult to assess but most likely they remain vulnerable to overfishing. Stocks of northern shrimp and Norwegian lobster are in good condition. In the Northeast Atlantic, 21% of stocks are considered overfished.
This zone makes almost three-quarters (72.8%) of European Union fishing catches in 2020. Main fishing EU countries are Denmark, France, the Netherlands and Spain. Most common species include herring, mackerel, and sprats.
thumb|Banks of the northwest Atlantic
Northwest Atlantic In the Northwest Atlantic landings have decreased from 4.2 million tons in the early 1970s to 1.9 million tons in 2013. During the 21st century, some species have shown weak signs of recovery, including Greenland halibut, yellowtail flounder, Atlantic halibut, haddock, spiny dogfish, while other stocks shown no such signs, including cod, witch flounder, and redfish. Stocks of invertebrates, in contrast, remain at record levels of abundance. 31% of stocks are overfished in the northwest Atlantic.
thumb|left|Capture of Atlantic northwest cod in million tons
In 1497, John Cabot became the first Western European since the Vikings to explore mainland North America and one of his major discoveries was the abundant resources of Atlantic cod off Newfoundland. Referred to as "Newfoundland Currency" this discovery yielded some 200 million tons of fish over five centuries. In the late 19th and early 20th centuries, new fisheries started to exploit haddock, mackerel, and lobster. From the 1950s to the 1970s, the introduction of European and Asian distant-water fleets in the area dramatically increased the fishing capacity and the number of exploited species. It also expanded the exploited areas from near-shore to the open sea and to great depths to include deep-water species such as redfish, Greenland halibut, witch flounder, and grenadiers. Overfishing in the area was recognized as early as the 1960s but, because this was occurring on international waters, it took until the late 1970s before any attempts to regulate was made. In the early 1990s, this finally resulted in the collapse of the Atlantic northwest cod fishery. The population of a number of deep-sea fishes also collapsed in the process, including American plaice, redfish, and Greenland halibut, together with flounder and grenadier.
Eastern central-Atlantic In the eastern central-Atlantic small pelagic fishes constitute about 50% of landings with sardine reaching 0.6–1.0 million tons per year. Pelagic fish stocks are considered fully fished or overfished, with sardines south of Cape Bojador the notable exception. Almost half of the stocks are fished at biologically unsustainable levels. Total catches have been fluctuating since the 1970s; reaching 3.9 million tons in 2013 or slightly less than the peak production in 2010.
thumb|upright|Bahama Banks
Western central-Atlantic In the western central-Atlantic, catches have been decreasing since 2000 and reached 1.3 million tons in 2013. The most important species in the area, Gulf menhaden, reached a million tons in the mid-1980s but only half a million tons in 2013 and is now considered fully fished. Round sardinella was an important species in the 1990s but is now considered overfished. Groupers and snappers are overfished and northern brown shrimp and American cupped oyster are considered fully fished approaching overfished. 44% of stocks are being fished at unsustainable levels.
thumb|left|Agulhas Bank
Southeast Atlantic In the southeast Atlantic catches have decreased from 3.3 million tons in the early 1970s to 1.3 million tons in 2013. Horse mackerel and hake are the most important species, together representing almost half of the landings. Off South Africa and Namibia deep-water hake and shallow-water Cape hake have recovered to sustainable levels since regulations were introduced in 2006 and the states of southern African pilchard and anchovy have improved to fully fished in 2013.
Southwest Atlantic In the southwest Atlantic, a peak was reached in the mid-1980s and catches now fluctuate between 1.7 and 2.6 million tons. The most important species, the Argentine shortfin squid, which reached half a million tons in 2013 or half the peak value, is considered fully fished to overfished. Another important species was the Brazilian sardinella, with a production of 100,000 tons in 2013 it is now considered overfished. Half the stocks in this area are being fished at unsustainable levels: Whitehead's round herring has not yet reached fully fished but Cunene horse mackerel is overfished. The sea snail perlemoen abalone is targeted by illegal fishing and remains overfished. |
Atlantic Ocean | Environmental issues | Environmental issues |
Atlantic Ocean | Endangered species | Endangered species
Endangered marine species include the manatee, seals, sea lions, turtles, and whales. Drift net fishing can kill dolphins, albatrosses and other seabirds (petrels, auks), hastening the fish stock decline and contributing to international disputes. |
Atlantic Ocean | Waste and pollution | Waste and pollution
Marine pollution is a generic term for the entry into the ocean of potentially hazardous chemicals or particles. The biggest culprits are rivers and with them many agriculture fertilizer chemicals as well as livestock and human waste. The excess of oxygen-depleting chemicals leads to hypoxia and the creation of a dead zone.Sebastian A. Gerlach "Marine Pollution", Springer, Berlin (1975)
thumb|Marine debris strewn over the beaches of the South Atlantic Inaccessible Island
Marine debris, which is also known as marine litter, describes human-created waste floating in a body of water. Oceanic debris tends to accumulate at the center of gyres and coastlines, frequently washing aground where it is known as beach litter. The North Atlantic garbage patch is estimated to be hundreds of kilometers across in size.
Other pollution concerns include agricultural and municipal waste. Municipal pollution comes from the eastern United States, southern Brazil, and eastern Argentina; oil pollution in the Caribbean Sea, Gulf of Mexico, Lake Maracaibo, Mediterranean Sea, and North Sea; and industrial waste and municipal sewage pollution in the Baltic Sea, North Sea, and Mediterranean Sea.
A USAF C-124 aircraft from Dover Air Force Base, Delaware was carrying three nuclear bombs over the Atlantic Ocean when it experienced a loss of power. For their own safety, the crew jettisoned two nuclear bombs, which were never recovered. |
Atlantic Ocean | Climate change | Climate change
North Atlantic hurricane activity has increased over past decades because of increased sea surface temperature (SST) at tropical latitudes, changes that can be attributed to either the natural Atlantic Multidecadal Oscillation (AMO) or to anthropogenic climate change.
A 2005 report indicated that the Atlantic meridional overturning circulation (AMOC) slowed down by 30% between 1957 and 2004. In 2024, the research highlighted a significant weakening of the AMOC by approximately 12% over the past two decades. If the AMO were responsible for SST variability, the AMOC would have increased in strength, which is apparently not the case. Furthermore, it is clear from statistical analyses of annual tropical cyclones that these changes do not display multidecadal cyclicity. Therefore, these changes in SST must be caused by human activities.
The ocean mixed layer plays an important role in heat storage over seasonal and decadal time scales, whereas deeper layers are affected over millennia and have a heat capacity about 50 times that of the mixed layer. This heat uptake provides a time-lag for climate change but it also results in thermal expansion of the oceans which contributes to sea level rise. 21st-century global warming will probably result in an equilibrium sea-level rise five times greater than today, whilst melting of glaciers, including that of the Greenland ice sheet, expected to have virtually no effect during the 21st century, will likely result in a sea-level rise of over a millennium. |
Atlantic Ocean | Theories of natural delimitation between the Atlantic and Pacific oceans | Theories of natural delimitation between the Atlantic and Pacific oceans
thumb|300px|right|Map showing the proposal presented by the thesis entitled "Natural delimitation between the Pacific and South Atlantic oceans by the Shackleton Fracture Zone"
Scientific researchers have proposed delimiting the boundary between the Atlantic and Pacific oceans by two different natural boundaries, by the Shackleton fracture zone and by the Scotia Arc the former being more current than the latter. |
Atlantic Ocean | See also | See also
Atlantic Revolutions
List of countries and territories bordering the Atlantic Ocean
Seven Seas
Shipwrecks in the Atlantic Ocean
Atlantic hurricanes
Piracy in the Atlantic World
Transatlantic crossing
South Atlantic Peace and Cooperation Zone
Natural delimitation between the Pacific and South Atlantic oceans by the Scotia Arc |
Atlantic Ocean | References | References |
Atlantic Ocean | Sources | Sources
map
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Atlantic Ocean | Further reading | Further reading
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Atlantic Ocean | External links | External links
Atlantic Ocean. Cartage.org.lb (archived)
"Map of Atlantic Coast of North America from the Chesapeake Bay to Florida" from 1639 via the Library of Congress
Category:Oceans
Category:Articles containing video clips
Category:Oceans surrounding Antarctica |
Atlantic Ocean | Table of Content | Short description, Toponymy, Extent and data, Biggest seas in Atlantic Ocean, Bathymetry, Mid-Atlantic Ridge, Ocean floor, Water characteristics, Salinity, Water masses, Gyres, Sargasso Sea, Climate, Natural hazards, Geology and plate tectonics, Central Atlantic, North Atlantic, South Atlantic, Closure of the Atlantic, History, Old World, New World, Atlantic World, Economy, Fisheries, Environmental issues, Endangered species, Waste and pollution, Climate change, Theories of natural delimitation between the Atlantic and Pacific oceans, See also, References, Sources, Further reading, External links |
Angola | Short description | Angola, officially the Republic of Angola, is a country on the west-central coast of Southern Africa. It is the second-largest Portuguese-speaking (Lusophone) country in both total area and population and is the seventh-largest country in Africa. It is bordered by Namibia to the south, the Democratic Republic of the Congo to the north, Zambia to the east, and the Atlantic Ocean to the west. Angola has an exclave province, the province of Cabinda, that borders the Republic of the Congo and the Democratic Republic of the Congo. The capital and most populous city is Luanda.
Angola has been inhabited since the Paleolithic Age. After the Bantu expansion reached the region, states were formed by the 13th century and organised into confederations. The Kingdom of Kongo ascended to achieve hegemony among the other kingdoms from the 14th century. Portuguese explorers established relations with Kongo in 1483. To the south were the kingdoms of Ndongo and Matamba, with the Ovimbundu kingdoms further south, and the Mbunda Kingdom in the east.
The Portuguese began colonising the coast in the 16th century. Kongo fought three wars against the Portuguese, ending in the Portuguese conquest of Ndongo. The banning of the slave trade in the 19th century severely disrupted Kongo's undiversified economic system and European settlers gradually began to establish their presence in the interior of the region. The Portuguese colony that became Angola did not achieve its present borders until the early 20th century and experienced strong resistance from native groups such as the Cuamato, the Kwanyama, and the Mbunda.
After a protracted anti-colonial struggle (1961–1974), Angola achieved independence in 1975 as a one-party Republic, but the country descended into a devastating civil war the same year, between the ruling People's Movement for the Liberation of Angola (MPLA), backed by the Soviet Union and Cuba; the insurgent National Union for the Total Independence of Angola, an originally Maoist and later anti-communist group supported by the United States and South Africa; the militant organization National Liberation Front of Angola, backed by Zaire; and the Front for the Liberation of the Enclave of Cabinda seeking the independence of the Cabinda exclave, also backed by Zaire.
Since the end of the civil war in 2002, Angola has emerged as a relatively stable constitutional republic, and its economy is among the fastest-growing in the world, with China, the European Union, and the United States being the country's largest investment and trade partners. However, the economic growth is highly uneven, with most of the nation's wealth concentrated in a disproportionately small part of the population as most Angolans have a low standard of living; life expectancy is among the lowest in the world, while infant mortality is among the highest.
Angola is a member of the United Nations, African Union, the Community of Portuguese Language Countries, and the Southern African Development Community. , the Angolan population is estimated at 37.2 million. Angolan culture reflects centuries of Portuguese influence, namely the predominance of the Portuguese language and of the Catholic Church, intermingled with a variety of indigenous customs and traditions. |
Angola | Etymology | Etymology
The name Angola comes from the Portuguese colonial name ('Kingdom of Angola'), which appeared as early as Paulo Dias de Novais's 1571 charter. The toponym was derived by the Portuguese from the title ngola, held by the kings of Ndongo and Matamba. Ndongo in the highlands, between the Kwanza and Lucala rivers, was nominally a possession of the Kingdom of Kongo. But in the 16th century it was seeking greater independence. |
Angola | History | History |
Angola | Early migrations and political units | Early migrations and political units
thumb|upright|left|King João I, Manikongo of the Kingdom of Kongo
Modern Angola was populated predominantly by nomadic Khoi and San peoples prior to the first Bantu migrations. The Khoi and San peoples were hunter-gatherers, rather than practicing pastoralism or cultivation of crops.
In the first millennium BC, they were displaced by Bantu peoples arriving from the north, most of whom likely originated in what is today northwestern Nigeria and southern Niger. Bantu speakers introduced the cultivation of bananas and taro, as well as maintenance of large cattle herds, to Angola's central highlands and the Luanda plain. Due to a number of inhibiting geographic factors throughout the territory of Angola, namely harshly traversable land, hot/humid climate, and a plethora of deadly diseases, intermingling of pre-colonial tribes in Angola had been rare.
After settlement of the migrants, a number of political entities developed. The best-known of these was the Kingdom of Kongo, based in Angola. It extended northward to what are now the Democratic Republic of the Congo, the Republic of the Congo, and Gabon. It established trade routes with other city-states and civilisations up and down the coast of southwestern and western Africa. Its traders even reached Great Zimbabwe and the Mutapa Empire, although the kingdom engaged in little or no trans-oceanic trade. To its south lay the Kingdom of Ndongo, from which the area of the later Portuguese colony was sometimes known as Dongo. Next to that was the Kingdom of Matamba. The lesser Kingdom of Kakongo to the north was later a vassal of the Kingdom of Kongo. The people in all of these states spoke Kikongo as a common language. |
Angola | Portuguese colonization | Portuguese colonization
thumb|upright|left|Coat of arms granted to King Afonso I of Kongo by King Manuel I of Portugal
Portuguese explorer Diogo Cão reached the area in 1484. The previous year, the Portuguese had established relations with the Kingdom of Kongo, which stretched at the time from modern Gabon in the north to the Kwanza River in the south. The Portuguese established their primary early trading post at Soyo, which is now the northernmost city in Angola apart from the Cabinda exclave.
Paulo Dias de Novais founded São Paulo de Loanda (Luanda) in 1575 with a hundred families of settlers and four hundred soldiers. Benguela was fortified in 1587 and became a township in 1617. An authoritarian state, the Kingdom of Kongo was highly centralised around its monarch and controlled neighbouring states as vassals. It had a strong economy, based on the industries of copper, ivory, salt, hides, and, to a lesser extent, slaves. The transition from a feudal system of slavery to a capitalist one with Portugal would prove crucial to the history of the Kingdom of Kongo.
As relations between Kongo and Portugal grew in the early 16th century, trade between the kingdoms also increased. Most of the trade was in palm cloth, copper, and ivory, but also increasing numbers of slaves. Kongo exported few slaves, and its slave market had remained internal. But, following the development of a successful sugar-growing colony after Portuguese settlement of São Tomé, Kongo became a major source of slaves for the island's traders and plantations. Correspondence by King Afonso documents the purchase and sale of slaves within the country. His accounts also detail which slaves captured in war were given or sold to Portuguese merchants.
Afonso continued to expand the kingdom of Kongo into the 1540s, expanding its borders to the south and east. The expansion of Kongo's population, coupled with Afonso's earlier religious reforms, allowed the ruler to centralize power in his capital and increase the power of the monarchy. He also established a royal monopoly on some trade. To govern the growing slave trade, Afonso and several Portuguese kings claimed a joint monopoly on the external slave trade.
The slave trade increasingly became Kongo's primary, and arguably sole, economic sector. A major obstacle for the Kingdom of Kongo was that slaves were the only commodity for which the European powers were willing to trade. Kongo lacked an effective international currency. Kongolese nobles could buy slaves with the national currency of nzimbu shells, which could be traded for slaves. These could be sold to gain international currency.
As the slave trade was the only commodity in which Europeans were interested in the region during the 16th and 17th centuries, the Kongo economy was unable to diversify or later industrialise outside of sectors in which slavery was involved, such as the arms industry.Rinquist, John: Kongo Iron: Symbolic Power, Superior Technology and Slave Wisdom, African Diaspora Archaeology Newsletter, Volume 11, Issue 3, September 2008, Article 3, pp.14–15 The increased production and sale of guns within the kingdom was due to the salient issue of the slave trade, which had become an increasingly violent struggle. There was a constant need for slaves for the kings and queens to sell in exchange for foreign commodities, the absence of which would prevent them from having any influence with European powers such as Portugal and eventually the Dutch Republic.
Kongolese kings needed this influence to garner support from European powers for quelling internal rebellions. The situation became increasingly complicated during the rule of Garcia II, who needed the assistance of the Dutch military to drive out the Portuguese from Luanda, in spite of the fact that Portugal was Kongo's primary slave trading partner.
By the early 17th century, the supply of foreign slaves captured by the Kongolese externally was waning. The government began to approve the enslavement of freeborn Kongolese citizens for relatively minor infractions, nearly any disobeying of the authoritarian system and the aristocracy. If several villagers were deemed guilty of a crime, it became relatively common for the whole village to be enslaved. The resulting chaos and internal conflict from Garcia II's reign would lead into that of his son and successor, António I. He was killed in 1665 by Portuguese at the Battle of Mbwila 1665, together with a substantial proportion of the aristocracy. The colonists were expanding their power.Thornton, John K: Warfare in Atlantic Africa 1500–1800, 1999. Routledge. Page 103.
War broke out more widely in the Kingdom of Kongo after the death of António I. Much of the stability and access to iron ore and charcoal necessary for gunsmiths to maintain the arms industry was disrupted. From then on, in this period almost every Kongolese citizen was in danger of being enslaved.Thornton, John K: The Kongolese Saint Anthonty: Dona Beatriz Kimpa Vita and the Antonian Movement, 1684–1706, page 69. Cambridge University, 1998 Many Kongolese subjects were adroit in making guns, and they were enslaved to have their skills available to colonists in the New World, where they worked as blacksmiths, ironworkers, and charcoal makers.
The Portuguese established several other settlements, forts and trading posts along the Angolan coast, principally trading in Angolan slaves for plantations. Local slave dealers provided a large number of slaves for the Portuguese Empire, usually in exchange for manufactured goods from Europe. This part of the Atlantic slave trade continued until after Brazil's independence in the 1820s.
thumb|right|Queen Ana de Sousa of Ndongo meeting with the Portuguese, 1657
thumb|left|Depiction of Luanda from 1755
Despite Portugal's territorial claims in Angola, its control over much of the country's vast interior was minimal. In the 16th century Portugal gained control of the coast through a series of treaties and wars. Life for European colonists was difficult and progress was slow. John Iliffe notes that "Portuguese records of Angola from the 16th century show that a great famine occurred on average every seventy years; accompanied by epidemic disease, it might kill one-third or one-half of the population, destroying the demographic growth of a generation and forcing colonists back into the river valleys".Iliffe, John (2007) Africans: the history of a continent . Cambridge University Press. p. 68. . For valuable complements for the 16th and 17th centuries see Beatrix Heintze, Studien zur Geschichte Angolas im 16. und 17. Jahrhundert, Colónia/Alemanha: Köppe, 1996
During the Portuguese Restoration War, the Dutch West India Company occupied the principal settlement of Luanda in 1641, using alliances with local peoples to carry out attacks against Portuguese holdings elsewhere. A fleet under Salvador de Sá retook Luanda in 1648; reconquest of the rest of the territory was completed by 1650. New treaties with the Kongo were signed in 1649; others with Njinga's Kingdom of Matamba and Ndongo followed in 1656. The conquest of Pungo Andongo in 1671 was the last major Portuguese expansion from Luanda, as attempts to invade Kongo in 1670 and Matamba in 1681 failed. Colonial outposts also expanded inward from Benguela, but until the late 19th century the inroads from Luanda and Benguela were very limited. Hamstrung by a series of political upheavals in the early 1800s, Portugal was slow to mount a large scale annexation of Angolan territory.
thumb|right|upright|History of Angola; written in Luanda in 1680.
The slave trade was abolished in Angola in 1836, and in 1854 the colonial government freed all its existing slaves. Four years later, a more progressive administration appointed by Portugal abolished slavery altogether. However, these decrees remained largely unenforceable, and the Portuguese depended on assistance from the British Royal Navy and what became known as the Blockade of Africa to enforce their ban on the slave trade. This coincided with a series of renewed military expeditions into the bush.
By the mid-nineteenth century Portugal had established its dominion as far north as the Congo River and as far south as Mossâmedes. Until the late 1880s, Portugal entertained proposals to link Angola with its colony in Mozambique but was blocked by British and Belgian opposition. In this period, the Portuguese came up against different forms of armed resistance from various peoples in Angola.See René Pélissier, Les guerres grises: Résistance et revoltes en Angola, (1845-1941), Éditions Pélissier, Montamets, 78630 Orgeval (France), 1977
The Berlin Conference in 1884–1885 set the colony's borders, delineating the boundaries of Portuguese claims in Angola, although many details were unresolved until the 1920s.See René Pélissier, La colonie du Minotaure. Nationalismes et révoltes en Angola (1926–1961), éditions Pélissier, Montamets, 78630 Orgeval (France), 1979 Trade between Portugal and its African territories rapidly increased as a result of protective tariffs, leading to increased development, and a wave of new Portuguese immigrants.
In 1925, an expedition to Angola was conducted by American naturalist explorer Arthur Stannard Vernay.
Between 1939 and 1943, Portuguese army operations against the Mucubal, who they accused of rebellion and cattle-thieving, resulted in hundreds of Mucubal killed. During the campaign, 3,529 were taken prisoner, 20% of whom were women and children, and imprisoned in concentration camps. Many died in captivity from undernourishment, violence and forced labor. Around 600 were sent to Sao Tome and Principe. Hundreds were also sent to a camp in Damba, where 26% died. |
Angola | Angolan War of Independence | Angolan War of Independence
thumb|left|Portuguese Armed Forces marching in Luanda during the Portuguese Colonial Wars (1961–74).
Under colonial law, black Angolans were forbidden from forming political parties or labour unions. The first nationalist movements did not take root until after World War II, spearheaded by a largely Westernised and Portuguese-speaking urban class, which included many mestiços. During the early 1960s they were joined by other associations stemming from ad hoc labour activism in the rural workforce. Portugal's refusal to address increasing Angolan demands for self-determination provoked an armed conflict, which erupted in 1961 with the Baixa de Cassanje revolt and gradually evolved into a protracted war of independence that persisted for the next twelve years. Throughout the conflict, three militant nationalist movements with their own partisan guerrilla wings emerged from the fighting between the Portuguese government and local forces, supported to varying degrees by the Portuguese Communist Party.
The National Front for the Liberation of Angola (FNLA) recruited from Bakongo refugees in Zaire. Benefiting from particularly favourable political circumstances in Léopoldville, and especially from a common border with Zaire, Angolan political exiles were able to build up a power base among a large expatriate community from related families, clans, and traditions. People on both sides of the border spoke mutually intelligible dialects and enjoyed shared ties to the historical Kingdom of Kongo. Though as foreigners skilled Angolans could not take advantage of Mobutu Sese Seko's state employment programme, some found work as middlemen for the absentee owners of various lucrative private ventures. The migrants eventually formed the FNLA with the intention of making a bid for political power upon their envisaged return to Angola.
thumb|upright|Members of the National Liberation Front of Angola training in 1973.
A largely Ovimbundu guerrilla initiative against the Portuguese in central Angola from 1966 was spearheaded by Jonas Savimbi and the National Union for the Total Independence of Angola (UNITA). It remained handicapped by its geographic remoteness from friendly borders, the ethnic fragmentation of the Ovimbundu, and the isolation of peasants on European plantations where they had little opportunity to mobilise.
During the late 1950s, the rise of the Marxist–Leninist Popular Movement for the Liberation of Angola (MPLA) in the east and Dembos hills north of Luanda came to hold special significance. Formed as a coalition resistance movement by the Angolan Communist Party, the organisation's leadership remained predominantly Ambundu and courted public sector workers in Luanda. Although both the MPLA and its rivals accepted material assistance from the Soviet Union or the People's Republic of China, the former harboured strong anti-imperialist views and was openly critical of the United States and its support for Portugal. This allowed it to win important ground on the diplomatic front, soliciting support from nonaligned governments in Morocco, Ghana, Guinea, Mali, and the United Arab Republic.
The MPLA attempted to move its headquarters from Conakry to Léopoldville in October 1961, renewing efforts to create a common front with the FNLA, then known as the Union of Angolan Peoples (UPA) and its leader Holden Roberto. Roberto turned down the offer. When the MPLA first attempted to insert its own insurgents into Angola, the cadres were ambushed and annihilated by UPA partisans on Roberto's orders—setting a precedent for the bitter factional strife which would later ignite the Angolan Civil War. |
Angola | Angolan Civil War | Angolan Civil War
thumb|left|upright|Agostinho Neto, first President of Angola.
Throughout the war of independence, the three rival nationalist movements were severely hampered by political and military factionalism, as well as their inability to unite guerrilla efforts against the Portuguese. Between 1961 and 1975 the MPLA, UNITA, and the FNLA competed for influence in the Angolan population and the international community. The Soviet Union and Cuba became especially sympathetic towards the MPLA and supplied that party with arms, ammunition, funding, and training. They also backed UNITA militants until it became clear that the latter was at irreconcilable odds with the MPLA.
The collapse of Portugal's Estado Novo government following the 1974 Carnation Revolution suspended all Portuguese military activity in Africa and the brokering of a ceasefire pending negotiations for Angolan independence. Encouraged by the Organisation of African Unity, Holden Roberto, Jonas Savimbi, and MPLA chairman Agostinho Neto met in Mombasa in early January 1975 and agreed to form a coalition government. This was ratified by the Alvor Agreement later that month, which called for general elections and set the country's independence date for 11 November 1975. All three factions, however, followed up on the ceasefire by taking advantage of the gradual Portuguese withdrawal to seize various strategic positions, acquire more arms, and enlarge their militant forces. The rapid influx of weapons from numerous external sources, especially the Soviet Union and the United States, as well as the escalation of tensions between the nationalist parties, fueled a new outbreak of hostilities. With tacit American and Zairean support the FNLA began massing large numbers of troops in northern Angola in an attempt to gain military superiority. Meanwhile, the MPLA began securing control of Luanda, a traditional Ambundu stronghold. Sporadic violence broke out in Luanda over the next few months after the FNLA attacked the MPLA's political headquarters in March 1975. The fighting intensified with street clashes in April and May, and UNITA became involved after over two hundred of its members were massacred by an MPLA contingent that June. An upswing in Soviet arms shipments to the MPLA influenced a decision by the Central Intelligence Agency to likewise provide substantial covert aid to the FNLA and UNITA.
In August 1975, the MPLA requested direct assistance from the Soviet Union in the form of ground troops. The Soviets declined, offering to send advisers but no troops; however, Cuba was more forthcoming and in late September dispatched nearly five hundred combat personnel to Angola, along with sophisticated weaponry and supplies. By independence, there were over a thousand Cuban soldiers in the country. They were kept supplied by a massive airbridge carried out with Soviet aircraft. The persistent buildup of Cuban and Soviet military aid allowed the MPLA to drive its opponents from Luanda and blunt an abortive intervention by Zairean and South African troops, which had deployed in a belated attempt to assist the FNLA and UNITA. The FNLA was largely annihilated after the decisive Battle of Quifangondo, although UNITA managed to withdraw its civil officials and militia from Luanda and seek sanctuary in the southern provinces. From there, Savimbi continued to mount a determined insurgent campaign against the MPLA.
thumb|Soviet made Cuban PT-76 tank in Luanda during the Cuban intervention in Angola, 1976
Between 1975 and 1991, the MPLA implemented an economic and political system based on the principles of scientific socialism, incorporating central planning and a Marxist–Leninist one-party state. It embarked on an ambitious programme of nationalisation, and the domestic private sector was essentially abolished. Privately owned enterprises were nationalised and incorporated into a single umbrella of state-owned enterprises known as Unidades Economicas Estatais (UEE). Under the MPLA, Angola experienced a significant degree of modern industrialisation. However, corruption and graft also increased and public resources were either allocated inefficiently or simply embezzled by officials for personal enrichment. The ruling party survived an attempted coup d'état by the Maoist-oriented Communist Organisation of Angola (OCA) in 1977, which was suppressed after a series of bloody political purges left thousands of OCA supporters dead.
The MPLA abandoned its former Marxist ideology at its third party congress in 1990, and declared social democracy to be its new platform. Angola subsequently became a member of the International Monetary Fund; restrictions on the market economy were also reduced in an attempt to draw foreign investment. By May 1991 it reached a peace agreement with UNITA, the Bicesse Accords, which scheduled new general elections for September 1992. When the MPLA secured a major electoral victory, UNITA objected to the results of both the presidential and legislative vote count and returned to war. Following the election, the Halloween massacre occurred from 30 October to 1 November, where MPLA forces killed thousands of UNITA supporters. |
Angola | 21st century | 21st century
thumb|right|Luanda is experiencing widespread urban renewal and redevelopment in the 21st century, backed largely by profits from the oil and diamond industries.
On 22 February 2002, government troops killed Savimbi in a skirmish in the Moxico province. UNITA and the MPLA consented to the Luena Memorandum of Understanding in April; UNITA agreed to give up its armed wing. With the elections in 2008 and 2012, an MPLA-ruled dominant-party system emerged, with UNITA and the FNLA as opposition parties.
Angola has a serious humanitarian crisis; the result of the prolonged war, of the abundance of minefields, and the continued political agitation in favour of the independence of the exclave of Cabinda (carried out in the context of the protracted Cabinda conflict by the FLEC). While most of the internally displaced have now squatted around the capital, in musseques (shanty towns) the general situation for Angolans remains desperate.Lari (2004), Human Rights Watch (2005)For an overall analysis see Ricardo Soares de Oliveira, Magnificent and Beggar Land: Angola since the Civil War, London: Hurst, 2015
A drought in 2016 caused the worst food crisis in Southern Africa in 25 years, affecting 1.4 million people across seven of Angola's eighteen provinces. Food prices rose and acute malnutrition rates doubled, impacting over 95,000 children.
José Eduardo dos Santos stepped down as President of Angola after 38 years in 2017, being peacefully succeeded by João Lourenço, Santos' chosen successor. Some members of the dos Santos family were later linked to high levels of corruption. In July 2022, ex-president José Eduardo dos Santos died in Spain.
In August 2022, the ruling party, MPLA, won another majority and President Lourenço won a second five-year term in the election. However, the election was the tightest in Angola's history. |
Angola | Geography | Geography
thumb|upright|Topography of Angola
At , Angola is the world's twenty-second largest country – comparable in size to Mali, or twice the size of France or of Texas. It lies mostly between latitudes 4° and 18°S, and longitudes 12° and 24°E.
Angola borders Namibia to the south, Zambia to the east, the Democratic Republic of the Congo to the north-east and the South Atlantic Ocean to the west.
The coastal exclave of Cabinda in the north has borders with the Republic of the Congo to the north and with the Democratic Republic of the Congo to the south. Angola has a favorable coastline for maritime trade, with four natural harbors: Luanda, Lobito, Moçâmedes, and Porto Alexandre. These natural indentations contrast with Africa's typical coastline of rocky cliffs and deep bays. Angola's capital, Luanda, lies on the Atlantic coast in the northwest of the country.
Angola had a 2018 Forest Landscape Integrity Index mean score of 8.35/10, ranking it 23rd globally out of 172 countries. In Angola forest cover is around 53% of the total land area, equivalent to 66,607,380 hectares (ha) of forest in 2020, down from 79,262,780 hectares (ha) in 1990. In 2020, naturally regenerating forest covered 65,800,190 hectares (ha) and planted forest covered 807,200 hectares (ha). Of the naturally regenerating forest 40% was reported to be primary forest (consisting of native tree species with no clearly visible indications of human activity) and around 3% of the forest area was found within protected areas. For the year 2015, 100% of the forest area was reported to be under public ownership.
thumb|right|300px|Satellite imagery of Angola, 2022 |
Angola | Climate | Climate
thumb|300px|Angola map of Köppen climate classification.
Like the rest of tropical Africa, Angola experiences distinct, alternating rainy and dry seasons. In the north, the rainy season may last for as long as seven months—usually from September to April, with perhaps a brief slackening in January or February. In the south, the rainy season begins later, in November, and lasts until about February. The dry season (cacimbo) is often characterized by a heavy morning mist. In general, precipitation is higher in the north, but at any latitude it is greater in the interior than along the coast and increases with altitude. Temperatures fall with distance from the equator and with altitude and tend to rise closer to the Atlantic Ocean. Thus, at Soyo, at the mouth of the Congo River, the average annual temperature is about 26 °C, but it is under 16 °C at Huambo on the temperate central plateau. The coolest months are July and August (in the middle of the dry season), when frost may sometimes form at higher altitudes.
Due to climate change, Angola's annual average temperature has increased by 1.4.°C since 1951, and is expected to keep rising while rainfall is becoming more variable. Angola is highly vulnerable to climate change impacts. Natural hazards such as floods, erosion, droughts, and epidemics (e.g.: malaria, cholera and typhoid fever) are expected to worsen with climate change. Rising sea levels also pose a significant risk to Angola's coastal areas, where around 50% of the population lives.
In 2023 Angola emitted 174.71 million tonnes of greenhouse gases, around 0.32% of the world's total emissions, making it the 46th highest emitting country. In its Nationally Determined Contribution, Angola has pledged a 14% reduction in its greenhouse gas emissions by 2025 and an additional 10% reduction conditional on international support. According to the World Bank, achieving climate resilience in Angola requires diversifying the country's economy away from its dependence on oil. |
Angola | Wildlife | Wildlife |
Angola | Government and politics | Government and politics
thumb|right|The National Assembly of Angola
The Angolan government is composed of three branches of government: executive, legislative and judicial. The executive branch of the government is composed of the President, the vice-presidents and the Council of Ministers.
The legislative branch comprises a 220-seat unicameral legislature, the National Assembly of Angola, elected from multi-member province-wide and nationwide constituencies using party-list proportional representation. For decades, political power has been concentrated in the presidency.
After 38 years of rule, in 2017 President dos Santos stepped down from MPLA leadership.Angolan Leader Dos Santos to Step Down After 38 Years in Power . Bloomberg (3 February 2017). Retrieved 26 April 2017. The leader of the winning party at the parliamentary elections in August 2017 would become the next president of Angola. The MPLA selected the former Defense Minister João Lourenço as Santos' chosen successor.
In what has been described as a political purge to cement his power and reduce the influence of the Dos Santos family, Lourenço subsequently sacked the chief of the national police, Ambrósio de Lemos, and the head of the intelligence service, Apolinário José Pereira. Both are considered allies of former president Dos Santos. He also removed Isabel dos Santos, daughter of the former president, as head of the country's state oil company Sonangol. In August 2020, José Filomeno dos Santos, son of Angola's former president, was sentenced for five years in jail for fraud and corruption. |
Angola | Constitution | Constitution
thumb|right|João Lourenço, President of Angola
The Constitution of 2010 establishes the broad outlines of government structure and delineates the rights and duties of citizens. The legal system is based on Portuguese law and customary law but is weak and fragmented, and courts operate in only 12 of more than 140 municipalities. A Supreme Court serves as the appellate tribunal; a Constitutional Court does not hold the powers of judicial review. Governors of the 18 provinces are appointed by the president. After the end of the civil war, the regime came under pressure from within as well as from the international community to become more democratic and less authoritarian. Its reaction was to implement a number of changes without substantially changing its character.Péclard, Didier (ed.) (2008) L'Angola dans la paix: Autoritarisme et reconversions, special issue of Politique africains (Paris), p. 110.
The new constitution, adopted in 2010, did away with presidential elections, introducing a system in which the president and the vice-president of the political party that wins the parliamentary elections automatically become president and vice-president. Directly or indirectly, the president controls all other organs of the state, so there is de facto no separation of powers.Miranda, Jorge (2010) "A Constituição de Angola de 2010", O Direito (Lisbon), vol. 142. In the classifications used in constitutional law, this government falls under the category of authoritarian regime. |
Angola | Justice | Justice
A Supreme Court serves as a court of appeal. The Constitutional Court is the supreme body of the constitutional jurisdiction, established with the approval of Law no. 2/08, of 17 June – Organic Law of the Constitutional Court and Law n. 3/08, of 17 June – Organic Law of the Constitutional Process. The legal system is based on Portuguese and customary law. There are 12 courts in more than 140 counties in the country. Its first task was the validation of the candidacies of the political parties to the legislative elections of 5 September 2008. Thus, on 25 June 2008, the Constitutional Court was institutionalized and its Judicial Counselors assumed the position before the President of the Republic. Currently, seven advisory judges are present, four men and three women.
In 2014, a new penal code took effect in Angola. The classification of money-laundering as a crime is one of the novelties in the new legislation.Angola com novo Código Penal ainda este ano , Notícias ao Minuto, 24 September 2014 |
Angola | Administrative divisions | Administrative divisions
thumb|upright|Map of Angola with the provinces numbered
thumb|right|Provincial Government of Huambo.
, Angola is divided into twenty-one provinces (províncias) and 162 municipalities. The municipalities are further divided into 559 communes (townships). The provinces are:
+NumberProvinceCapitalArea (km2)Population (2014 Census)1BengoCaxito31,371356,6412BenguelaBenguela39,8262,231,3853BiéCuíto70,3141,455,2554CabindaCabinda7,270716,0765CuandoMavinga??6Cuanza NorteN'dalatando24,110443,3867Cuanza SulSumbe55,6001,881,8738CubangoMenongue??9CuneneOndjiva87,342990,08710HuamboHuambo34,2702,019,55511HuílaLubango79,0232,497,42212Icolo e BengoCatete??13LuandaLuanda2,4176,945,38614Lunda Norte Dundo103,760862,56615Lunda SulSaurimo77,637537,58716MalanjeMalanje97,602986,36317Moxico LesteCazombo??18MoxicoLuena223,023758,56819NamibeMoçâmedes57,091495,32620UígeUíge58,6981,483,11821ZaireM'banza-Kongo40,130594,428 |
Angola | Exclave of Cabinda | Exclave of Cabinda
thumb|right|Provincial Government of Namibe.
With an area of approximately , the Northern Angolan province of Cabinda is unusual in being separated from the rest of the country by a strip, some wide, of the Democratic Republic of Congo along the lower Congo River. Cabinda borders the Congo Republic to the north and north-northeast and the DRC to the east and south. The city of Cabinda is the chief population centre.
According to a 1995 census, Cabinda had an estimated population of 600,000, approximately 400,000 of whom are citizens of neighboring countries. Population estimates are, however, highly unreliable. Consisting largely of tropical forest, Cabinda produces hardwoods, coffee, cocoa, crude rubber, and palm oil.
The product for which it is best known, however, is its oil, which has given it the nickname the Kuwait of Africa. Cabinda's petroleum production from its considerable offshore reserves now accounts for more than half of Angola's output. Most of the oil along its coast was discovered under Portuguese rule by the Cabinda Gulf Oil Company (CABGOC) from 1968 onwards.
Ever since Portugal handed over sovereignty of its former overseas province of Angola to the local independence groups (MPLA, UNITA and FNLA), the territory of Cabinda has been a focus of separatist guerrilla actions opposing the Government of Angola (which has employed its armed forces, the FAA—Forças Armadas Angolanas) and Cabindan separatists. |
Angola | Foreign relations | Foreign relations
thumb|upright|Foreign Minister of Angola Manuel Domingos Augusto.
Angola is a founding member state of the Community of Portuguese Language Countries (CPLP), also known as the Lusophone Commonwealth, an international organization and political association of Lusophone nations across four continents, where Portuguese is an official language.
On 16 October 2014, Angola was elected for the second time a non-permanent member of the United Nations Security Council, with 190 favorable votes out of a total of 193. The term of office began on 1 January 2015 and expired on 31 December 2016. Public, 16 October 2014
Since January 2014, the Republic of Angola has been chairing the International Conference for the Great Lakes Region (CIRGL). [80] In 2015, CIRGL Executive Secretary Ntumba Luaba said that Angola is the example to be followed by the members of the organization, due to the significant progress made during the 12 years of peace, namely in terms of socio-economic stability and political-military. Expansion, 8 January 2015 |
Angola | Military | Military
thumb|right|Soldiers of the Angolan Armed Forces in full dress uniform
The Angolan Armed Forces (Forças Armadas Angolanas, FAA) are headed by a Chief of Staff who reports to the Minister of Defence. There are three divisions—the Army (Exército), Navy (Marinha de Guerra, MGA) and National Air Force (Força Aérea Nacional, FAN). Total manpower is 107,000; plus paramilitary forces of 10,000 (2015 est.).
Its equipment includes Russian-manufactured fighters, bombers and transport planes. There are also Brazilian-made EMB-312 Tucanos for training, Czech-made L-39 Albatroses for training and bombing, and a variety of western-made aircraft such as the C-212\Aviocar, Sud Aviation Alouette III, etc. A small number of FAA personnel are stationed in the Democratic Republic of the Congo (Kinshasa) and 500 more were deployed in March 2023 due to the resurgence of the M23. The FAA has also participated in the Southern African Development Community (SADC)'s mission for peace in Cabo Delgado, Mozambique. |
Angola | Police | Police
thumb|right|Angolan National Police officers
The National Police departments are Public Order, Criminal Investigation, Traffic and Transport, Investigation and Inspection of Economic Activities, Taxation and Frontier Supervision, Riot Police and the Rapid Intervention Police. The National Police are in the process of standing up an air wing, to provide helicopter support for operations. The National Police are developing their criminal investigation and forensic capabilities. The force consists of an estimated 6,000 patrol officers, 2,500 taxation and frontier supervision officers, 182 criminal investigators, 100 financial crimes detectives, and approximately 90 economic activity inspectors.
The National Police have implemented a modernisation and development plan to increase the capabilities and efficiency of the total force. In addition to administrative reorganisation, modernisation projects include procurement of new vehicles, aircraft and equipment, construction of new police stations and forensic laboratories, restructured training programmes and the replacement of AKM rifles with 9 mm Uzis for officers in urban areas. |
Angola | Human rights | Human rights
Angola was classified as 'not free' by Freedom House in the Freedom in the World 2014 report and the 2024 report, however the report has noted increases in freedoms under João Lourenço. The 2014 report noted that the August 2012 parliamentary elections, in which the ruling Popular Movement for the Liberation of Angola won more than 70% of the vote, suffered from serious flaws, including outdated and inaccurate voter rolls. Voter turnout dropped from 80% in 2008 to 60%.
A 2012 report by the U.S. Department of State said, "The three most important human rights abuses [in 2012] were official corruption and impunity; limits on the freedoms of assembly, association, speech, and press; and cruel and excessive punishment, including reported cases of torture and beatings as well as unlawful killings by police and other security personnel."
Angola ranked forty-two of forty-eight sub-Saharan African states on the 2007 Index of African Governance list and scored poorly on the 2013 Ibrahim Index of African Governance. It was ranked 39 out of 52 sub-Saharan African countries, scoring particularly badly in the areas of participation and human rights, sustainable economic opportunity and human development. The Ibrahim Index uses a number of variables to compile its list which reflects the state of governance in Africa.
In 2019, homosexual acts were decriminalized in Angola, and the government also prohibited discrimination based on sexual orientation. The vote was overwhelming: 155 for, 1 against, 7 abstaining. |
Angola | Economy | Economy
thumb|GDP per capita 1950 to 2018
Angola has diamonds, oil, gold, copper, rich wildlife (which was dramatically depleted during the civil war), forest, and fossil fuels. Since independence, oil and diamonds have been the most important economic resources. Smallholder and plantation agriculture dramatically dropped during the Angolan Civil War, but began to recover after 2002.
Angola's economy has in recent years moved on from the disarray caused by a quarter-century of Angolan civil war to become the fastest-growing economy in Africa and one of the fastest-growing in the world, with an average GDP growth of 20% between 2005 and 2007.Angola Financial Sector Profile: MFW4A – Making Finance Work for Africa . MFW4A. Retrieved 9 August 2013. In the period 2001–10, Angola had the world's highest annual average GDP growth, at 11.1%.
In 2004, the Exim Bank of China approved a $2 billion line of credit to Angola, to be used for rebuilding Angola's infrastructure, and to limit the influence of the International Monetary Fund there.
China is Angola's biggest trade partner and export destination as well as a significant source of imports. Bilateral trade reached $27.67 billion in 2011, up 11.5% year-on-year. China's imports, mainly crude oil and diamonds, increased 9.1% to $24.89 billion while China's exports to Angola, including mechanical and electrical products, machinery parts and construction materials, surged 38.8%. The oil glut led to a local price for unleaded gasoline of £0.37 a gallon.
As of 2021, the biggest import partners were the European Union, followed by China, Togo, the United States, and Brazil. More than half of Angola's exports go to China, followed by a significantly smaller amount to India, the European Union, and the United Arab Emirates.
The Angolan economy grew 18% in 2005, 26% in 2006 and 17.6% in 2007. Due to the global recession, the economy contracted an estimated −0.3% in 2009. The security brought about by the 2002 peace settlement has allowed the resettlement of 4 million displaced persons and a resulting large-scale increase in agriculture production. Angola's economy is expected to grow by 3.9 per cent in 2014 said the International Monetary Fund (IMF), robust growth in the non-oil economy, mainly driven by a very good performance in the agricultural sector, is expected to offset a temporary drop in oil production.
thumb|right|The National Bank of Angola.
Angola's financial system is maintained by the National Bank of Angola and managed by the governor Jose de Lima Massano. According to a study on the banking sector, carried out by Deloitte, the monetary policy led by Banco Nacional de Angola (BNA), the Angolan national bank, allowed a decrease in the inflation rate put at 7.96% in December 2013, which contributed to the sector's growth trend. Estimates released by Angola's central bank, said the country's economy should grow at an annual average rate of 5 per cent over the next four years, boosted by the increasing participation of the private sector. Angola was ranked 133rd in the Global Innovation Index in 2024.
Although the country's economy has grown significantly since Angola achieved political stability in 2002, mainly due to fast-rising earnings in the oil sector, Angola faces huge social and economic problems. These are in part a result of almost continual armed conflict from 1961 on, although the highest level of destruction and socio-economic damage took place after the 1975 independence, during the long years of civil war. However, high poverty rates and blatant social inequality chiefly stems from persistent authoritarianism, "neo-patrimonial" practices at all levels of the political, administrative, military and economic structures, and of a pervasive corruption.Anti-corruption watchdog Transparency International rates Angola one of the 10 most corrupt countries in the world.Dolan, Kerry A. (23 January 2013). "Isabel Dos Santos, Daughter Of Angola's President, Is Africa's First Woman Billionaire" . Forbes. The main beneficiaries are political, administrative, economic and military power holders, who have accumulated (and continue to accumulate) enormous wealth.This process is well analyzed by authors like Christine Messiant, Tony Hodges and others. For an eloquent illustration, see the Angolan magazine Infra-Estruturas África 7/2010.
thumb|left|Luanda Financial City
"Secondary beneficiaries" are the middle strata that are about to become social classes. However, almost half the population has to be considered poor, with dramatic differences between the countryside and the cities, where slightly more than 50% of the people reside.
A study carried out in 2008 by the Angolan Instituto Nacional de Estatística found that in rural areas roughly 58% must be classified as "poor" according to UN norms but in the urban areas only 19%, and an overall rate of 37%. In cities, a majority of families, well beyond those officially classified as poor, must adopt a variety of survival strategies.Udelsmann Rodrigues, Cristina (2006) O Trabalho Dignifica o Homem: Estratégias de Sobrevivência em Luanda, Lisbon: Colibri. In urban areas social inequality is most evident and it is extreme in Luanda.As an excellent illustration see Luanda: A vida na cidade dos extremos, in: Visão, 11 November 2010. In the Human Development Index Angola constantly ranks in the bottom group.The HDI 2010 lists Angola in the 146th position among 169 countries—one position below that of Haiti. MLP l Human Development Index and its components.
thumb|right|Tourism in Angola has grown with the country's economy and stability.
In January 2020, a leak of government documents known as the Luanda Leaks showed that U.S. consulting companies such as Boston Consulting Group, McKinsey & Company, and PricewaterhouseCoopers had helped members of the family of former President José Eduardo dos Santos (especially his daughter Isabel dos Santos) corruptly run Sonangol for their own personal profit, helping them use the company's revenues to fund vanity projects in France and Switzerland. After further revelations in the Pandora Papers, former generals Dias and do Nascimento and former presidential advisers were also accused of misappropriating significant public funds for personal benefit.
The enormous differences between the regions pose a serious structural problem for the Angolan economy, illustrated by the fact that about one third of economic activities are concentrated in Luanda and neighbouring Bengo province, while several areas of the interior suffer economic stagnation and even regression.Manuel Alves da Rocha (2010) Desigualdades e assimetrias regionais em Angola: Os factores da competitividade territorial , Luanda: Centro de Estudos e Investigação Científica da Universidade Católica de Angola.
One of the economic consequences of social and regional disparities is a sharp increase in Angolan private investments abroad. The small fringe of Angolan society where most of the asset accumulation takes place seeks to spread its assets, for reasons of security and profit. For the time being, the biggest share of these investments is concentrated in Portugal where the Angolan presence (including the family of the state president) in banks as well as in the domains of energy, telecommunications, and mass media has become notable, as has the acquisition of vineyards and orchards as well as of tourism enterprises."A força do kwanza", Visão (Lisbon), 993, 15 May 2012, pp. 50–54
thumb|Corporate headquarters in Luanda
Angola has upgraded critical infrastructure, an investment made possible by funds from the country's development of oil resources.The New Prosperity: Strategies for Improving Well-Being in Sub-Saharan Africa Tony Blair Africa Governance Initiative 1 May 2013 According to a report, just slightly more than ten years after the end of the civil war Angola's standard of living has overall greatly improved. Life expectancy, which was just 46 years in 2002, reached 51 in 2011. Mortality rates for children fell from 25 per cent in 2001 to 19 per cent in 2010 and the number of students enrolled in primary school has tripled since 2001.The New Prosperity: Strategies for Improving Well-Being in Sub-Saharan Africa Report by The Boston Consulting Group and Tony Blair Africa Governance Initiative, May 2013 However, at the same time the social and economic inequality that has characterised the country for so long has not diminished, but has deepened in all respects.
With a stock of assets corresponding to 70 billion Kz (US$6.8 billion), Angola is now the third-largest financial market in sub-Saharan Africa, surpassed only by Nigeria and South Africa. According to the Angolan Minister of Economy, Abraão Gourgel, the financial market of the country grew modestly since 2002 and now occupies third place in sub-Saharan Africa.Angola is the third-largest sub-Saharan financial market , MacauHub, 23 July 2014
On 19 December 2014, the Capital Market in Angola was launched. BODIVA (Angola Stock Exchange and Derivatives, in English) was allocated the secondary public debt market, and was expected to launch the corporate debt market by 2015, though the stock market itself was only expected to commence trading in 2016.CMC prepares launch of debt secondary market Angola Press Agency, 16 December 2014 |
Angola | Natural resources | Natural resources
thumb|right|An offshore oil drilling platform off the coast of central Angola
The Economist reported in 2008 that diamonds and oil make up 60% of Angola's economy, almost all of the country's revenue and all of its dominant exports."Marching towards riches and democracy?" The Economist. 30 August 2008. p. 46. Growth is almost entirely driven by rising oil production which surpassed in late 2005 and was expected to grow to by 2007. Control of the oil industry is consolidated in Sonangol Group, a conglomerate owned by the Angolan government. In December 2006, Angola was admitted as a member of OPEC. In 2022, the country produced an average of 1.165 million barrels of oil per day, according to Agência Nacional de Petróleo, Gás e Biocombustíveis (ANPG), the national oil, gas and biofuels agency.
According to the Heritage Foundation, a conservative American think tank, oil production from Angola has increased so significantly that Angola now is China's biggest supplier of oil. "China has extended three multi-billion dollar lines of credit to the Angolan government; two loans of $2 billion from China Exim Bank, one in 2004, the second in 2007, as well as one loan in 2005 of $2.9 billion from China International Fund Ltd."
Growing oil revenues also created opportunities for corruption: according to a recent Human Rights Watch report, US$32 billion disappeared from government accounts in 2007–2010. Furthermore, Sonangol, the state-run oil company, controls 51% of Cabinda's oil. Due to this market control, the company ends up determining the profit received by the government and the taxes it pays. The council of foreign affairs states that the World Bank mentioned that Sonangol is a taxpayer, it carries out quasi-fiscal activities, it invests public funds, and, as concessionaire, it is a sector regulator. This multifarious work program creates conflicts of interest and characterises a complex relationship between Sonangol and the government that weakens the formal budgetary process and creates uncertainty as regards the actual fiscal stance of the state."
In 2002, Angola demanded compensation for oil spills allegedly caused by Chevron Corporation, the first time it had fined a multinational corporation operating in its waters.
Operations in its diamond mines include partnerships between state-run Endiama and mining companies such as ALROSA which operate in Angola.
Access to biocapacity in Angola is higher than world average. In 2016, Angola had 1.9 global hectares of biocapacity per person within its territory, slightly more than world average of 1.6 global hectares per person. In 2016, Angola used 1.01 global hectares of biocapacity per person – their ecological footprint of consumption. This means they use about half as much biocapacity as Angola contains. As a result, Angola is running a biocapacity reserve. |
Angola | Agriculture | Agriculture
thumb|right|Capanda Dam on the Cuanza
Agriculture and forestry is an area of potential opportunity for the country. The African Economic Outlook organization states that "Angola requires 4.5 million tonnes a year of grain but grows only about 55% of the maize it needs, 20% of the rice and just 5% of its required wheat".Muzima, Joel. Mazivila, Domingos. "Angola 2014" Retrieved from www.africaneconomicoutlook.org
In addition, the World Bank estimates that "less than 3 per cent of Angola's abundant fertile land is cultivated and the economic potential of the forestry sector remains largely unexploited"."Country partnership strategy for the Republic of Angola" (15 August 2013). World Bank (Report No. 76225-A0)
Before independence in 1975, Angola was a bread-basket of southern Africa and a major exporter of bananas, coffee and sisal, but three decades of civil war destroyed fertile countryside, left it littered with landmines and drove millions into the cities. The country now depends on expensive food imports, mainly from South Africa and Portugal, while more than 90% of farming is done at the family and subsistence level. Thousands of Angolan small-scale farmers are trapped in poverty.Redvers, Louise POVERTY-ANGOLA: Inter Press Service News Agency – NGOs Sceptical of Govt's Rural Development Plans . |
Angola | Transport | Transport
thumb|right|TAAG Angola Airlines is the country's state-owned national carrier.
Transport in Angola consists of:
Three separate railway systems totalling
of highway of which is paved
1,295 navigable inland waterways
five major sea ports
243 airports, of which 32 are paved.
Angola centers its port trade in five main ports: Namibe, Lobito, Soyo, Cabinda and Luanda. The port of Luanda is the largest of the five, as well as being one of the busiest on the African continent.thumb|left|Catumbela Bridge in Benguela.
Two trans-African automobile routes pass through Angola: the Tripoli-Cape Town Highway and the Beira-Lobito Highway. Travel on highways outside of towns and cities in Angola (and in some cases within) is often not best advised for those without four-by-four vehicles. While reasonable road infrastructure has existed within Angola, time and war have taken their toll on the road surfaces, leaving many severely potholed, littered with broken asphalt. In many areas drivers have established alternative tracks to avoid the worst parts of the surface, although careful attention must be paid to the presence or absence of landmine warning markers by the side of the road. The Angolan government has contracted the restoration of many of the country's roads. The road between Lubango and Namibe, for example, was completed recently with funding from the European Union,ec.europa.eu: 1992 and is comparable to many European main routes. Completing the road infrastructure is likely to take some decades, but substantial efforts are already being made.
The old airport in Luanda, Quatro de Fevereiro Airport, will be replaced by the new Dr. Antonio Agostinho Neto International Airport. |
Angola | Telecommunications | Telecommunications
thumb|right|Lobito hosts a major seaport.
thumb|right|Luanda's construction boom is financed largely by oil and diamonds.
The telecommunications industry is considered one of the main strategic sectors in Angola.
In October 2014, the building of an optic fiber underwater cable was announced. This project aims to turn Angola into a continental hub, thus improving Internet connections both nationally and internationally.
On 11 March 2015, the First Angolan Forum of Telecommunications and Information Technology was held in Luanda under the motto "The challenges of telecommunications in the current context of Angola", to promote debate on topical issues on telecommunications in Angola and worldwide. A study of this sector, presented at the forum, said Angola had the first telecommunications operator in Africa to test LTE – with speeds up to 400 Mbit/s – and mobile penetration of about 75%; there are about 3.5 million smartphones in the Angolan market; There are about of optical fibre installed in the country.
The first Angolan satellite, AngoSat-1, was launched into orbit on 26 December 2017. It was launched from the Baikonur space center in Kazakhstan on board a Zenit 3F rocket. The satellite was built by Russia's RSC Energia, a subsidiary of the state-run space industry player Roscosmos. The satellite payload was supplied by Airbus Defence & Space. Due to an on-board power failure during solar panel deployment, on 27 December, RSC Energia revealed that they lost communications contact with the satellite. Although, subsequent attempts to restore communications with the satellite were successful, the satellite eventually stopped sending data and RSC Energia confirmed that AngoSat-1 was inoperable. The launch of AngoSat-1 was aimed at ensuring telecommunications throughout the country. According to Aristides Safeca, Secretary of State for Telecommunications, the satellite was aimed at providing telecommunications services, TV, internet and e-government and was expected to remain in operation "at best" for 18 years.
A replacement satellite named AngoSat-2 was pursued and was expected to be in service by 2020. As of February 2021, Ango-Sat-2 was about 60% ready. The officials reported the launch was expected in about 17 months, by July 2022.[ The launch of AngoSat-2 occurred on 12 October 2022. |
Angola | Technology | Technology
The management of the top-level domain '.ao' passed from Portugal to Angola in 2015, following new legislation.Angola to manage own internet domain from 2015 Telecompaper, 16 September 2014 A joint decree of Minister of Telecommunications and Information Technologies José Carvalho da Rocha and the minister of Science and Technology, Maria Cândida Pereira Teixeira, states that "under the massification" of that Angolan domain, "conditions are created for the transfer of the domain root '.ao' of Portugal to Angola".Angola manages its own Internet domain Macauhub, 16 September 2014 |
Angola | Demographics | Demographics
thumb|right|upright=1.2|Historical ethnic divisions of Angola
Angola has a population of 24,383,301 inhabitants according to the preliminary results of its 2014 census, the first one conducted or carried out since 15 December 1970. It is composed of Ovimbundu (language Umbundu) 37%, Ambundu (language Kimbundu) 23%, Bakongo 13%, and 32% other ethnic groups (including the Chokwe, the Ovambo, the Ganguela and the Xindonga) as well as about 2% mulattos (mixed European and African), 1.6% Chinese and 1% European. The Ambundu and Ovimbundu ethnic groups combined form a majority of the population, at 62%.As no reliable census data exist at this stage (2011), all these numbers are rough estimates only, subject to adjustments and updates.2050 Population as a Multiple of 2014 . PRB 2014 World Population Data Sheet However, on 23 March 2016, official data revealed by Angola's National Statistic Institute – Instituto Nacional de Estatística (INE), states that Angola has a population of 25,789,024 inhabitants.
It is estimated that Angola was host to 12,100 refugees and 2,900 asylum seekers by the end of 2007. 11,400 of those refugees were originally from the Democratic Republic of Congo, who arrived in the 1970s.U.S. Committee for Refugees and Immigrants. "World Refugee Survey 2008". p. 37 there were an estimated 400,000 Democratic Republic of the Congo migrant workers,World Refugee Survey 2008 – Angola , United Nations High Commission for Refugees. NB: This figure is highly doubtful, as it makes no clear distinction between migrant workers, refugees and immigrants. at least 220,000 Portuguese, and about 259,000 Chinese living in Angola. 1 million Angolans are mixed race (black and white). Also, 40,000 Vietnamese live in the country.
Since 2003, more than 400,000 Congolese migrants have been expelled from Angola."Calls for Angola to Investigate Abuse of Congolese Migrants ". Inter Press Service. 21 May 2012 Prior to independence in 1975, Angola had a community of approximately 350,000 Portuguese,"Flight from Angola ", The Economist , 16 August 1975, puts the number at 500,000, but this is an estimate lacking appropriate sources. . but the vast majority left after independence and the ensuing civil war. However, Angola has recovered its Portuguese minority in recent years; currently, there are about 200,000 registered with the consulates, and increasing due to the debt crisis in Portugal and the relative prosperity in Angola. The Chinese population stands at 258,920, mostly composed of temporary migrants. Also, there is a small Brazilian community of about 5,000 people. The Roma were deported to Angola from Portugal.
, the total fertility rate of Angola is 5.54 children born per woman (2012 estimates), the 11th highest in the world. |
Angola | Urbanization | Urbanization |
Angola | Languages | Languages
thumb|Situation of Portuguese in each province of Angola:
The languages in Angola are those originally spoken by the different ethnic groups and Portuguese, introduced during the Portuguese colonial era. The most widely spoken indigenous languages are Umbundu, Kimbundu and Kikongo, in that order. Portuguese is the official language of the country.
Although the exact numbers of those fluent in Portuguese or who speak Portuguese as a first language are unknown, a 2012 study mentions that Portuguese is the first language of 39% of the population.Silva, José António Maria da Conceição (2004) Angola . 7th World Urban Forum In 2014, a census carried out by the Instituto Nacional de Estatística in Angola mentions that 71.15% of the nearly 25.8 million inhabitants of Angola (meaning around 18.3 million people) use Portuguese as a first or second language.
According to the 2014 census, Portuguese is spoken by 71.1% of Angolans, Umbundu by 23%, Kikongo by 8.2%, Kimbundu by 7.8%, Chokwe by 6.5%, Nyaneka by 3.4%, Ngangela by 3.1%, Fiote by 2.4%, Kwanyama by 2.3%, Muhumbi by 2.1%, Luvale by 1%, and other languages by 4.1%. |
Angola | Religion | Religion
left|thumb|Catholic church of Uaco Cungo
There are about 1,000 religious communities, mostly Christian, in Angola.Viegas, Fátima (2008) Panorâmica das Religiões em Angola Independente (1975–2008), Ministério da Cultura/Instituto Nacional para os Assuntos Religiosos, Luanda While reliable statistics are nonexistent, estimates have it that more than half of the population are Catholics, while about a quarter adhere to the Protestant churches introduced during the colonial period: the Congregationalists mainly among the Ovimbundu of the Central Highlands and the coastal region to its west, the Methodists concentrating on the Kimbundu speaking strip from Luanda to Malanje, the Baptists almost exclusively among the Bakongo of the north-west (now present in Luanda as well) and dispersed Adventists, Reformed, and Lutherans.
In Luanda and region there subsists a nucleus of the "syncretic" Tocoists and in the north-west a sprinkling of Kimbanguism can be found, spreading from the Congo/Zaïre. Since independence, hundreds of Pentecostal and similar communities have sprung up in the cities, whereby now about 50% of the population is living; several of these communities/churches are of Brazilian origin.
the U.S. Department of State estimates the Muslim population at 80,000–90,000, less than 1% of the population, while the Islamic Community of Angola puts the figure closer to 500,000.Surgimento do Islão em Angola . O Pais. 2 September 2011. p. 18 Muslims consist largely of migrants from West Africa and the Middle East (especially Lebanon), although some are local converts.Oyebade, Adebayo O. Culture And Customs of Angola, 2006. pp. 45–46. The Angolan government does not legally recognize any Muslim organizations and often shuts down mosques or prevents their construction.
In a study assessing nations' levels of religious regulation and persecution with scores ranging from 0 to 10 where 0 represented low levels of regulation or persecution, Angola was scored 0.8 on Government Regulation of Religion, 4.0 on Social Regulation of Religion, 0 on Government Favoritism of Religion and 0 on Religious Persecution.Angola: Religious Freedom Profile at the Association of Religion Data Archives Brian J Grim and Roger Finke. "International Religion Indexes: Government Regulation, Government Favoritism and Social Regulation of Religion". Interdisciplinary Journal of Research on Religion. 2 (2006) Article 1: religjournal.com.
Foreign missionaries were very active prior to independence in 1975, although since the beginning of the anti-colonial fight in 1961 the Portuguese colonial authorities expelled a series of Protestant missionaries and closed mission stations based on the belief that the missionaries were inciting pro-independence sentiments. Missionaries have been able to return to the country since the early 1990s, although security conditions due to the civil war have prevented them until 2002 from restoring many of their former inland mission stations.
The Catholic Church and some major Protestant denominations mostly keep to themselves in contrast to the "New Churches" which actively proselytize. Catholics, as well as some major Protestant denominations, provide help for the poor in the form of crop seeds, farm animals, medical care and education. |
Angola | Health | Health
thumb|right|Lucrécia Paím Maternity Hospital
Epidemics of cholera, malaria, rabies and African hemorrhagic fevers like Marburg hemorrhagic fever, are common diseases in several parts of the country. Many regions in this country have high incidence rates of tuberculosis and high HIV prevalence rates. Dengue, filariasis, leishmaniasis and onchocerciasis (river blindness) are other diseases carried by insects that also occur in the region. Angola has one of the highest infant mortality rates in the world and one of the world's lowest life expectancies. A 2007 survey concluded that low and deficient niacin status was common in Angola. Demographic and Health Surveys is currently conducting several surveys in Angola on malaria, domestic violence and more.Angola Surveys , measuredhs.com
In September 2014, the Angolan Institute for Cancer Control (IACC) was created by presidential decree, and it will integrate the National Health Service in Angola.Novo instituto oncológico de Angola quer ser referência em África , Notícias ao Minuto (Source: Lusa Agency), 9 September 2014 The purpose of this new centre is to ensure health and medical care in oncology, policy implementation, programmes and plans for prevention and specialised treatment.Novo instituto oncológico de Angola quer ser referência em África , Diário Digital (Source: Lusa Agency), 9 September 2014 This cancer institute will be assumed as a reference institution in the central and southern regions of Africa.Novo instituto oncológico angolano quer ser instituição de referência no continente , Ver Angola, 11 September 2014
In 2014, Angola launched a national campaign of vaccination against measles, extended to every child under ten years old and aiming to go to all 18 provinces in the country.Angola: Over 30,000 Children Vaccinated Against Measles in Huila , All Africa, 30 September 2014 The measure is part of the Strategic Plan for the Elimination of Measles 2014–2020 created by the Angolan Ministry of Health which includes strengthening routine immunisation, a proper dealing with measles cases, national campaigns, introducing a second dose of vaccination in the national routine vaccination calendar and active epidemiological surveillance for measles. This campaign took place together with the vaccination against polio and vitamin A supplementation.
A yellow fever outbreak, the worst in the country in three decades began in December 2015. By August 2016, when the outbreak began to subside, nearly 4,000 people were suspected of being infected. As many as 369 may have died. The outbreak began in the capital, Luanda, and spread to at least 16 of the 18 provinces. In the 2024 Global Hunger Index (GHI), Angola has a serious level of hunger and ranks 103rd out of 127 countries. Angola's GHI score is 26.6 |
Angola | Education | Education
thumb|right|Agostinho Neto University
Although by law education in Angola is compulsory and free for eight years, the government reports that a percentage of pupils are not attending due to a lack of school buildings and teachers."Botswana". 2005 Findings on the Worst Forms of Child Labor. Bureau of International Labor Affairs, U.S. Department of Labor (2006). This article incorporates text from this source, which is in the public domain. Pupils are often responsible for paying additional school-related expenses, including fees for books and supplies.
In 1999, the gross primary enrollment rate was 74 per cent and in 1998, the most recent year for which data are available, the net primary enrollment rate was 61 per cent. Gross and net enrollment ratios are based on the number of pupils formally registered in primary school and therefore do not necessarily reflect actual school attendance. There continue to be significant disparities in enrollment between rural and urban areas. In 1995, 71.2 per cent of children ages 7 to 14 years were attending school. It is reported that higher percentages of boys attend school than girls. During the Angolan Civil War (1975–2002), nearly half of all schools were reportedly looted and destroyed, leading to current problems with overcrowding.
thumb|upright|A primary school in Province of Cuanza Sul
The Ministry of Education recruited 20,000 new teachers in 2005 and continued to implement teacher training. Teachers tend to be underpaid, inadequately trained and overworked (sometimes teaching two or three shifts a day). Some teachers may reportedly demand payment or bribes directly from their pupils. Other factors, such as the presence of landmines, lack of resources and identity papers, and poor health prevent children from regularly attending school. Although budgetary allocations for education were increased in 2004, the education system in Angola continues to be extremely under-funded.
According to estimates by the UNESCO Institute for Statistics, the adult literacy rate in 2011 was 70.4%. By 2015, this had increased to 71.1%. 82.9% of men and 54.2% of women are literate as of 2001. Since independence from Portugal in 1975, a number of Angolan students continued to be admitted every year at high schools, polytechnical institutes and universities in Portugal and Brazil through bilateral agreements; in general, these students belong to the elites.
thumb|left|Mutu-ya Kevela Prep. School
In September 2014, the Angolan Ministry of Education announced an investment of 16 million Euros in the computerisation of over 300 classrooms across the country. The project also includes training teachers at a national level, "as a way to introduce and use new information technologies in primary schools, thus reflecting an improvement in the quality of teaching".Angola investe 16 milhões na informatização de 300 salas de aula em todo o país , jornal i (28 September 2014)
In 2010, the Angolan government started building the Angolan Media Libraries Network, distributed throughout several provinces in the country to facilitate the people's access to information and knowledge. Each site has a bibliographic archive, multimedia resources and computers with Internet access, as well as areas for reading, researching and socialising. The plan envisages the establishment of one media library in each Angolan province by 2017. The project also includes the implementation of several media libraries, in order to provide the several contents available in the fixed media libraries to the most isolated populations in the country.Government to open digital libraries in every province Angola Press Agency, 8 January 2015 At this time, the mobile media libraries are already operating in the provinces of Luanda, Malanje, Uíge, Cabinda and Lunda South. As for REMA, the provinces of Luanda, Benguela, Lubango and Soyo have currently working media libraries.Mediateca móvel aberta ao público Jornal de Angola, 9 January 2015 |
Angola | Culture | Culture
thumb|upright|Agostinho Neto National Memorial in Luanda
Angolan culture has been heavily influenced by Portuguese culture, especially in language and religion, and the culture of the indigenous ethnic groups of Angola, predominantly Bantu culture.
The diverse ethnic communities—the Ovimbundu, Ambundu, Bakongo, Chokwe, Mbunda and other peoples—to varying degrees maintain their own cultural traits, traditions and languages, but in the cities, where slightly more than half of the population now lives, a mixed culture has been emerging since colonial times; in Luanda, since its foundation in the 16th century.
In this urban culture, Portuguese heritage has become more and more dominant. African roots are evident in music and dance and is moulding the way in which Portuguese is spoken. This process is well reflected in contemporary Angolan literature, especially in the works of Angolan authors.
In 2014, Angola resumed the National Festival of Angolan Culture after a 25-year break. The festival took place in all the provincial capitals and lasted for 20 days, with the theme "Culture as a Factor of Peace and Development.Retrospect2014: Fenacult marks cultural year Angola Press Agency, 18 December 2014 |
Angola | Media | Media |
Angola | Cinema | Cinema
In 1972, one of Angola's first feature films, Sarah Maldoror's internationally co-produced Sambizanga, was released at the Carthage Film Festival to critical acclaim, winning the Tanit d'Or, the festival's highest prize. |
Angola | Sports | Sports
thumb|upright=1.15|The National Stadium in Benguela
Basketball is the second most popular sport in Angola. Its national team has won the AfroBasket 11 times and holds the record of most titles. As a top team in Africa, it is a regular competitor at the Summer Olympic Games and the FIBA World Cup. Angola is home to one of Africa's first competitive leagues. Bruno Fernando, a player for the Atlanta Hawks, is the only current NBA player from Angola.
In football, Angola hosted the 2010 Africa Cup of Nations. The Angola national football team qualified for the 2006 FIFA World Cup, their first appearance in the World Cup finals. They were eliminated after one defeat and two draws in the group stage. They won three COSAFA Cups and finished runner-up in the 2011 African Nations Championship.
Angola has participated in the World Women's Handball Championship for several years. The country has also appeared in the Summer Olympics for seven years and both regularly competes in and once has hosted the FIRS Roller Hockey World Cup, where the best finish is sixth. Angola is also often believed to have historic roots in the martial art "Capoeira Angola" and "Batuque" which were practised by enslaved African Angolans transported as part of the Atlantic slave trade. |
Angola | See also | See also
Outline of Angola
Index of Angola-related articles |
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