Franklin's lost expedition was a failed British voyage of Arctic exploration led by Captain Sir John Franklin that departed England, United Kingdom in 1845 aboard two ships,  and , and was assigned to traverse the last unnavigated sections of the Northwest Passage in the Canadian Arctic and to record magnetic data to help determine whether a better understanding could aid navigation. The expedition met with disaster after both ships and their crews, a total of 129 officers and men, became icebound in Victoria Strait near King William Island in what is today the Canadian territory of Nunavut. After being icebound for more than a year Erebus and Terror were abandoned in April 1848, by which point two dozen men, including Franklin, had died. The survivors, now led by Franklin's second-in-command, Francis Crozier, and Erebuss captain, James Fitzjames, set out for the Canadian mainland and disappeared, presumably having perished.

Pressed by Franklin's wife, Jane, and others, the Admiralty launched a search for the missing expedition in 1848. In the many subsequent searches in the decades afterwards, several artefacts from the expedition were discovered, including the remains of two men, which were returned to Britain. A series of scientific studies in modern times suggested that the men of the expedition did not all die quickly. Hypothermia, starvation, lead poisoning or zinc deficiency and diseases including scurvy, along with general exposure to a hostile environment while lacking adequate clothing and nutrition, killed everyone on the expedition in the years after it was last sighted by Europeans in 1845. Cut marks on some of the bones recovered during these studies also supported allegations of cannibalism reported by Franklin searcher John Rae in 1854.

Despite the expedition's notorious failure, it did succeed in exploring the vicinity of what was one of the many Northwest Passages to eventually be discovered. Robert McClure led one of the expeditions that investigated the fate of Franklin's expedition, a voyage which was also beset by great challenges and later controversies. McClure's expedition returned after finding an ice-bound route that connected the Atlantic Ocean to the Pacific Ocean. The Northwest Passage was not navigated by boat until 1906, when Roald Amundsen traversed the passage on the Gjøa.

In 2014, a search team led by Parks Canada located the wreck of Erebus in the eastern portion of Queen Maud Gulf. Two years later, the Arctic Research Foundation found the wreck of Terror south of King William Island, in the body of water named Terror Bay. Research and dive expeditions are an annual occurrence at the wreck sites, now protected as a combined National Historic Site.

Background
The search by Europeans for a western shortcut by sea from Europe to Asia began with the voyages of Portuguese and Spanish explorers such as Bartolomeu Dias, Vasco da Gama and Christopher Columbus in the 15th century. By the mid-19th century numerous exploratory expeditions had been mounted, originating mainly from the Kingdom of England (England was a part of the Kingdom of Great Britain from 1707, and a part of the United Kingdom from 1801). These voyages, when successful, added to the sum of European geographic knowledge about the Western Hemisphere, particularly North America. As that knowledge grew, exploration gradually shifted towards the Arctic.

Sixteenth- and seventeenth-century voyagers who made geographic discoveries about North America included Martin Frobisher, John Davis, Henry Hudson and William Baffin. In 1670 the incorporation of the Hudson's Bay Company (HBC) led to further exploration of the Canadian coastlines, interior and adjacent Arctic seas. In the 18th century explorers of this region included James Knight, Christopher Middleton, Samuel Hearne, James Cook, Alexander MacKenzie and George Vancouver. By 1800 their discoveries had conclusively demonstrated that no Northwest Passage between the Pacific and Atlantic oceans existed in the temperate latitudes.

In 1804 Sir John Barrow became Second Secretary of the Admiralty, a post he held until 1845. Barrow began pushing for the Royal Navy to find a Northwest Passage over the top of Canada and to navigate toward the North Pole, organising a major series of expeditions. Over those four decades explorers including John Ross, David Buchan, William Edward Parry, Frederick William Beechey, James Clark Ross (nephew of John Ross), George Back, Peter Warren Dease and Thomas Simpson led productive expeditions to the Canadian Arctic. Among those explorers was John Franklin, who first travelled to the region in 1818 as second-in-command of an expedition towards the North Pole on the ships Dorothea and Trent. Franklin was subsequently leader of two overland expeditions to and along the Canadian Arctic coast, in 1819–22 and 1825–27.

By 1845 the combined discoveries of all these expeditions had reduced the unknown parts of the Canadian Arctic that might contain a Northwest Passage to a quadrilateral area of about . It was in this unexplored area that the next expedition was to sail, heading west through Lancaster Sound, then west and south – however ice, land and other obstacles might allow – with the goal of finding a Northwest Passage. The distance to be navigated was roughly .

Preparations

Command
Barrow was now 82 years old and nearing the end of his career. He felt that the expeditions were close to finding a Northwest Passage, perhaps through what Barrow believed to be an ice-free Open Polar Sea around the North Pole. Barrow deliberated over who should command the next expedition. Parry, his first choice, was tired of the Arctic and politely declined. His second choice, James Clark Ross, also declined because he had promised his new wife that he had finished polar exploration. His third choice, James Fitzjames, was rejected by the Admiralty for his youth. Barrow also considered Back but thought he was too argumentative. Francis Crozier, another possibility, was of humble birth and Irish, which counted against him. Reluctantly, Barrow settled on the 59-year-old Franklin.

The expedition was to consist of two ships,  and , both of which had been used for James Clark Ross' expedition to the Antarctic in 1839-1843, during which Crozier had commanded Terror. Franklin was given command of Erebus, with Fitzjames as the vessel's second-in-command; Crozier was appointed his executive officer and was again made commander of Terror. Franklin received command of the expedition on 7 February 1845, and his official instructions on 5 May 1845.

Ships, provisions and personnel

Erebus (378 tons bm) and Terror (331 tons bm) were sturdily built and well equipped, including several recent inventions. Steam engines were fitted, driving a single screw propeller in each vessel; these engines were converted former locomotives from the London & Croydon Railway. The ships could make  on steam power, or travel under wind power to reach higher speeds and/or save fuel.

Other advanced technology in the ships included reinforced bows constructed of heavy beams and iron plates, an internal steam heating system for the comfort of the crew in polar conditions, and a system of iron wells that allowed the screw propellers and iron rudders to be withdrawn into the hull to protect them from damage. The ships also carried libraries of more than 1,000 books and three years' supply of food, which included tinned soup and vegetables, salt-cured meat, pemmican and several live cattle. The tinned food was supplied from a provisioner, Stephen Goldner, who was awarded the contract on 1 April 1845, a mere seven weeks before Franklin set sail. Goldner worked frantically on the large order of 8,000 tins. The haste required affected quality control of some of the tins, which were later found to have  that was "thick and sloppily done, and dripped like melted candle wax down the inside surface".

Most of the crew were English, many from Northern England, with smaller numbers of Irish, Welsh and Scottish members. Two of the sailors were not born in the British Isles: Charles Johnson was from Halifax, Nova Scotia, Canada, and Henry Lloyd was from Kristiansand, Norway. The only officers with prior experience of the Arctic were Franklin, Crozier, Erebus First Lieutenant Graham Gore, Terror assistant surgeon Alexander McDonald and the two ice-masters, James Reid (Erebus) and Thomas Blanky (Terror).

Outward journey and loss

The expedition set sail from Greenhithe, Kent, on the morning of 19 May 1845, with a crew of 24 officers and 110 men. The ships stopped briefly in Stromness, Orkney Islands, in northern Scotland. From there they sailed to Greenland with  and a transport ship, Barretto Junior; the passage to Greenland took 30 days.

At the Whalefish Islands in Disko Bay, on the west coast of Greenland, ten oxen carried on Barretto Junior were slaughtered for fresh meat which was transferred to Erebus and Terror. Crew members then wrote their last letters home, which recorded that Franklin had banned swearing and drunkenness. Five men were discharged due to sickness and sent home on Rattler and Barretto Junior, reducing the final crew to 129 men. In late July 1845 the whalers Prince of Wales (Captain Dannett) and Enterprise (Captain Robert Martin) encountered Terror and Erebus in Baffin Bay, where they were waiting for good conditions to cross to Lancaster Sound. The expedition was never seen again by Europeans.

Only limited information is available for subsequent events, pieced together over the next 150 years by other expeditions, explorers, scientists and interviews with Inuit. The only first-hand information on expedition's progress is the two-part Victory Point Note  found in the aftermath on King William Island. Franklin's men spent the winter of 1845–46 on Beechey Island, where three crew members died and were buried. After travelling down Peel Sound through the summer of 1846, Terror and Erebus became trapped in ice off King William Island in September 1846 and are thought never to have sailed again. According to the second part of the Victory Point Note dated 25 April 1848 and signed by Fitzjames and Crozier, the crew had wintered off King William Island in 1846–47 and 1847–48 and Franklin had died on 11 June 1847. The remaining crew had abandoned the ships and planned to walk over the island and across the sea ice towards the Back River on the Canadian mainland, beginning on 26 April 1848. In addition to Franklin, eight further officers and 15 men had also died by this point. The Victory Point Note is the last known communication of the expedition.

From archaeological finds it is believed that all of the remaining crew died on the subsequent  long march to Back River, most on the island. Thirty or forty men reached the northern coast of the mainland before dying, still hundreds of miles from the nearest outpost of Western civilisation.

The Victory Point Note

The Victory Point Note was found eleven years later in May 1859 by William Hobson (lieutenant on the McClintock Arctic expedition) placed in a cairn on the north-western coast of King William Island. It consists of two parts written on a pre-printed Admiralty form. The first part was written after the first overwintering in 1847 and the second part was added one year later. From the second part it can be inferred that the document was first deposited in a different cairn previously erected by James Clark Ross in 1830 during John Ross's Second Arctic expedition – at a location Ross named Victory Point. The document is therefore referred to as Victory Point Note.

The first message is written in the body of the form and dates from 28 May 1847.

The second and final part is written largely on the margins of the form owing to a lack of remaining space on the document. It was presumably written on 25 April 1848.

In 1859 Hobson found a second document using the same Admiralty form containing an almost identical duplicate of the first message from 1847 in a cairn a few miles southwest at Gore Point. This document did not contain the second message. From the handwriting it is assumed that all messages were written by Fitzjames. As he did not take part in the landing party that deposited the notes originally in 1847, it is inferred that both documents were originally filled in by Fitzjames on board the ships, with Lieutenant Graham Gore and Mate Charles Frederick Des Voeux adding their signatures as members of the landing party. This is further supported by the fact that both documents contain the same factual errors  namely the wrong date of the wintering on Beechey Island. In 1848, after the abandonment of the ships and subsequent recovery of the document from the Victory Point cairn, Fitzjames added the second message signed by him and Crozier and deposited the note in the cairn found by Hobson eleven years later.

19th century expeditions

Early searches

After two years had passed with no word from Franklin, public concern grew and Jane, Lady Franklin, as well as members of the Parliament of the United Kingdom and British newspapers, urged the Admiralty to send a search party. Although the Admiralty said it did not feel any reason to be alarmed, it responded by developing a three-pronged plan which in the spring of 1848 sent an overland rescue party, led by John Richardson and John Rae, down the Mackenzie River to the Canadian Arctic coast.

Two expeditions by sea were also launched  one, led by James Clark Ross, entering the Canadian Arctic archipelago through Lancaster Sound and the other, commanded by Henry Kellett, entering from the Pacific. In addition, the Admiralty offered a reward of £20,000 (£ as of ) "to any Party or Parties, of any country, who shall render assistance to the crews of the Discovery Ships under the command of Sir John Franklin". When the three-pronged effort failed, British national concern and interest in the Arctic increased until "finding Franklin became nothing less than a crusade." Ballads such as "Lady Franklin's Lament", commemorating Lady Franklin's search for her lost husband, became popular.

Many joined the search. In 1850, eleven British and two American ships cruised the Canadian Arctic, including the Breadalbane and her sister ship . Several converged off the east coast of Beechey Island, where the first relics of the expedition were found, including remnants of a winter camp from 1845 to 1846. Robert Goodsir, surgeon on the brig Lady Franklin, found the graves of John Torrington, John Hartnell and William Braine. No messages from the Franklin expedition were found at this site.

In the spring of 1851, passengers and crew aboard several ships observed a huge iceberg off Newfoundland, which bore two vessels, one upright and one on its beam ends. The ships were not examined closely. It was suggested at the time that the ships could have been Erebus and Terror but it is now known that they were not; it is likely that they were abandoned whaling ships.

In 1852 Edward Belcher was given command of the government Arctic expedition in search of Franklin. It was unsuccessful; Belcher's inability to render himself popular with his subordinates was peculiarly unfortunate on an Arctic voyage and he was not wholly suited to commanding vessels among ice. Four of the five ships (, Pioneer,  and Intrepid) were abandoned in pack ice, for which Belcher was court-martialled but acquitted.

One of these ships, HMS Resolute, was eventually recovered intact by an American whaler and returned to the United Kingdom. Timbers from the ship were later used to manufacture three desks, one of which, the Resolute desk, was presented by Queen Victoria to US President Rutherford B. Hayes; it has often been chosen by presidents for use in the Oval Office in the White House.

Overland searches

In 1854, Rae, while surveying the Boothia Peninsula for the HBC, discovered further evidence of the expedition's fate. Rae met an Inuk near Pelly Bay (now Kugaaruk, Nunavut) on 21 April 1854, who told him of a party of 35 to 40 white men who had died of starvation near the mouth of the Back River. Other Inuit confirmed this story, which included reports of cannibalism among the dying sailors.

The Inuit showed Rae many objects that were identified as having belonged to members of the Franklin expedition. In particular, Rae bought from the Inuit several silver forks and spoons later identified as belonging to Franklin; Fitzjames; Crozier; and James Walter Fairholme and Robert Orme Sargent, two crewmembers from Erebus. Rae's report was sent to the Admiralty, which in October 1854 urged the HBC to send an expedition down the Back River to search for other signs of Franklin and his men.

Next were Chief Factor James Anderson and HBC employee James Stewart, who travelled north by canoe to the mouth of the Back River. In July 1855, a band of Inuit told them of a group of qallunaat (Inuktitut for "whites" or "Europeans", perhaps best translated as "foreigners") who had starved to death along the coast. In August, Anderson and Stewart found a piece of wood inscribed with "Erebus" and another that said "Mr. Stanley" (surgeon aboard Erebus) on Montreal Island in Chantrey Inlet, where the Back River meets the sea.

Despite the findings of Rae and Anderson, the Admiralty did not plan another search of its own. The Royal Navy officially labelled the crew deceased in service on 31 March 1854. Lady Franklin, failing to convince the government to fund another search, personally commissioned one more expedition under Francis Leopold McClintock. The expedition ship, the steam schooner Fox, bought via public subscription, sailed from Aberdeen on 2 July 1857.

In April 1859, sled parties set out from Fox to search on King William Island. On 5 May, the party led by Lieutenant William Hobson discovered the Victory Point Note, which detailed the abandonment of Erebus and Terror, death of Franklin and other crewmembers, and the decision by the survivors to march south to the mainland. On the western extreme of King William Island, Hobson also discovered a lifeboat containing two human skeletons and relics from the Franklin expedition. In the boat was a large amount of abandoned equipment, including boots, silk handkerchiefs, scented soap, sponges, slippers, hair combs and many books, among them a copy of The Vicar of Wakefield by Oliver Goldsmith.

Elsewhere, on the island's southern coast, McClintock's searchers found another skeleton. Still clothed, it was searched, and some papers were found, including a seaman's certificate for Chief Petty Officer Harry Peglar of Terror. However, since the uniform was that of a ship's steward, it is more likely that the body was that of Thomas Armitage, gun-room steward on Terror and a shipmate of Peglar, whose papers he carried. McClintock himself took testimony from the Inuit about the expedition's disastrous end.

Two expeditions between 1860 and 1869 by Charles Francis Hall, who lived among the Inuit near Frobisher Bay on Baffin Island and later at Repulse Bay on the Canadian mainland, found camps, graves and relics on the southern coast of King William Island, but he believed none of the Franklin survivors would be found among the Inuit. In 1869, local Inuit took Hall to a shallow grave on the island containing well-preserved skeletal remains and fragments of clothing. These remains were taken to England and interred beneath the Franklin Memorial at Greenwich Old Royal Naval College, London.

The eminent biologist Thomas Henry Huxley examined the remains and concluded that they belonged to Henry Thomas Dundas Le Vesconte, second lieutenant on Erebus. An examination in 2009 suggested that these were actually the remains of Harry Goodsir, assistant surgeon on Erebus. Although Hall concluded that all of the Franklin crew were dead, he believed that the official expedition records would yet be found under a stone cairn. With the assistance of his guides Ipirvik and Taqulittuq, Hall gathered hundreds of pages of Inuit testimony.

Among these materials were accounts of visits to Franklin's ships, and an encounter with a party of white men on the southern coast of King William Island near Washington Bay. In the 1990s, this testimony was extensively researched by David C. Woodman and was the basis of two books, Unravelling the Franklin Mystery (1992) and Strangers Among Us (1995), in which he reconstructs the final months of the expedition. Woodman's narrative challenged existing theories that the survivors all perished over the remainder of 1848 as they marched south from Victory Point, arguing instead that Inuit accounts point strongly to most of the 105 survivors cited by Crozier in his final note actually surviving past 1848, re-manning at least one of the ships and managing to sail it down along the coast of King William Island before it sank, with some crew members surviving as late as 1851.

The hope of finding other additional expedition records led Lieutenant Frederick Schwatka of the United States Army to organise an expedition to King William Island between 1878 and 1880. Travelling to Hudson Bay on the schooner Eothen, Schwatka, assembling a team that included Inuit who had assisted Hall, continued north by foot and dog sled, interviewing Inuit, visiting known or likely sites of Franklin expedition remains, and wintering on the island. Although Schwatka failed to find the hoped-for papers, in a speech at a dinner given in his honour by the American Geographical Society in 1880, he said that his expedition had made "the longest sledge journey ever made both in regard to time and distance" of eleven months and four days and , that it was the first Arctic expedition on which the whites relied entirely on the same diet as the Inuit, and that it established the loss of the Franklin records "beyond all reasonable doubt". However, Schwatka was successful in locating the remains of one of Franklin's men, identified by personal effects as John Irving, third lieutenant aboard Terror. Schwatka had Irving's remains returned to Scotland, where they were buried with full honours at Dean Cemetery in Edinburgh on 7 January 1881.

The Schwatka expedition found no remnants of the Franklin expedition south of a place now known as Starvation Cove on the Adelaide Peninsula. This was about  north of Crozier's stated goal, the Back River, and several hundred miles away from the nearest Western outpost, on the Great Slave Lake. Woodman wrote of Inuit reports that between 1852 and 1858 Crozier and one other expedition member were seen in the Baker Lake area, about  to the south, where in 1948 Farley Mowat found "a very ancient cairn, not of normal Eskimo construction" inside which were shreds of a hardwood box with dovetail joints.

Contemporary search expeditions
1848
 East: James Clark Ross, (, ) only to Somerset Island because of ice.
 Centre: Rae–Richardson Arctic expedition Mackenzie River and along the coast.
 West: HMS Plover, HMS Herald to Bering Strait; William Pullen reaches Mackenzie by whaleboat.
1850
 West: Richard Collinson (HMS Enterprise), Robert McClure (HMS Investigator) to Bering Strait. McClure frozen in at Banks Island and Investigator abandoned after two winters, crew trek east to Belcher expedition ships, becoming first Europeans to cross the northwest passage. Collinson reaches Coronation Gulf, furthest east of any ship.
 East: Horatio Austin (), Erasmus Ommanney (), plus two steam tenders, Pioneer and Intrepid (Cpt. John Bertie Cator 1850). Ommanney finds Franklin's Beechey Island camp. Austin's four and the below ships gather around Beechey Island, are frozen in and in spring send out sledge expeditions in all directions. They left the Arctic before winter in 1851.
 East: Charles Forsyth (Prince Albert) financed by Lady Franklin; sledge on Somerset Island to Fury Beach.
 East: William Penny (Lady Franklin and Sophia)
 East: John Ross (schooner Felix)
 East: Edwin De Haven (, ) mounted the First Grinnell expedition.
1851
 William Kennedy (Prince Albert again) finds Bellot Strait proving that Somerset Island is an island.
1852
 Edward Augustus Inglefield in northern Baffin Bay.
 Edward Belcher in five ships: HMS Assistance (Belcher), HMS Resolute (Henry Kellett), Pioneer (Sherard Osborn), Intrepid (Francis Leopold McClintock) and depot ship  (William Pullen); much sledge exploration; rescues crew of HMS Investigator; all frozen in and abandoned except for North Star. Joined by supply ships Breadalbane, which would be crushed by ice, and , which with North Star took off crews of the other ships, including that of McClure's HMS Investigator, in 1854.
 Elisha Kane led the Second Grinnell expedition.
 Boat expedition up the Wellington Channel under the command of R. M'Cormick, R.N., in HMB Forlorn Hope.
1854
 John Rae learns where Franklin lost his ship.
1855
 Anderson and Stewart descend the Back River and find relics in Chantrey Inlet.
1857
 Francis McClintock finds relics at King William Island, including the sole surviving written records of the Franklin expedition (the Victory Point and Gore Point records), and a ship's boat on runners containing two corpses.
1869
 Charles Francis Hall at King William Island
1875
 Allen Young blocked at Peel Sound
1878
 Frederick Schwatka at King William Island

Modern expeditions

King William Island excavations (1981–1982)
In June 1981, Owen Beattie, a professor of anthropology at the University of Alberta (UAlberta), began the 1845–48 Franklin Expedition Forensic Anthropology Project (FEFAP) when he and his team of researchers and field assistants travelled from Edmonton to King William Island, traversing the island's western coast as Franklin's men did 132 years before. FEFAP hoped to find artefacts and skeletal remains in order to use modern forensics to establish identities and causes of death among the lost 129 crewmembers.

Although the trek found archaeological artefacts related to 19th-century Europeans and undisturbed disarticulated human remains, Beattie was disappointed that more remains were not found. Examining the bones of Franklin crewmen, he noted areas of pitting and scaling often found in cases of Vitamin C deficiency, the cause of scurvy. After returning to Edmonton, he compared notes from the survey with James Savelle, an Arctic archaeologist, and noticed skeletal patterns suggesting cannibalism. Seeking information about the Franklin crew's health and diet, he sent bone samples to the Alberta Soil and Feed Testing Laboratory for trace element analysis and assembled another team to visit King William Island. The analysis would find an unexpected level of 226 parts per million (ppm) of lead in the crewman's bones, which was ten times higher than the control samples, taken from Inuit skeletons from the same geographic area, of 26–36 ppm.

In June 1982, a team made up of Beattie and three students (Walt Kowall, a graduate student in anthropology at UAlberta; Arne Carlson, an archaeology and geography student from Simon Fraser University in British Columbia; and Arsien Tungilik, an Inuk student and field assistant) was flown to the west coast of King William Island where they retraced some of the steps of McClintock in 1859 and Schwatka in 1878–79. Discoveries during this expedition included the remains of between six and fourteen men in the vicinity of McClintock's "boat place" and artefacts including a complete boot sole fitted with makeshift cleats for better traction.

Beechey Island excavations and exhumations (1984–1986)
After returning to Edmonton in 1982 and learning of the lead level findings from the 1981 expedition, Beattie struggled to find a cause. Possibilities included the lead solder used to seal the expedition's food tins, other food containers lined with lead foil, food colouring, tobacco products, pewter tableware and lead-wicked candles. He came to suspect that the problems of lead poisoning compounded by the effects of scurvy could have been lethal for the Franklin crew. However, because skeletal lead might reflect lifetime exposure rather than exposure limited to the voyage, Beattie's theory could be tested only by forensic examination of preserved soft tissue as opposed to bone. Beattie decided to examine the graves of the buried crewmen on Beechey Island.

After obtaining legal permission, Beattie's team visited Beechey Island in August 1984 to perform autopsies on the three crewmen buried there. They started with John Torrington, the first crew member to die. After completing Torrington's autopsy and exhuming and briefly examining the body of John Hartnell, the team, pressed for time and threatened by weather, returned to Edmonton with tissue and bone samples. Trace element analysis of Torrington's bones and hair indicated that the crewman "would have suffered severe mental and physical problems caused by lead poisoning". Although the autopsy indicated that pneumonia had been the ultimate cause of the crewman's death, lead poisoning was cited as a contributing factor.

During the expedition, the team visited a place about  north of the gravesite to examine fragments of hundreds of food tins discarded by Franklin's men. Beattie noted that the seams were poorly soldered with lead, which had likely come in direct contact with the food. The release of findings from the 1984 expedition and the photo of Torrington, a 138-year-old corpse well preserved by Arctic permafrost, led to wide media coverage and renewed interest in the Franklin expedition.

Subsequent research has suggested that another potential source for the lead may have been the ships' distilled water systems rather than the tinned food. K. T. H. Farrer argued that "it is impossible to see how one could ingest from the canned food the amount of lead, 3.3 mg per day over eight months, required to raise the PbB to the level 80 μg/dL at which symptoms of lead poisoning begin to appear in adults and the suggestion that bone lead in adults could be 'swamped' by lead ingested from food over a period of a few months, or even three years, seems scarcely tenable." In addition, tinned food was in widespread use within the Royal Navy at that time and its use did not lead to any significant increase in lead poisoning elsewhere.

However, and uniquely for this expedition only, the ships were fitted with converted railway locomotive engines for auxiliary propulsion which required an estimated one tonne of fresh water per hour when steaming. It is highly probable that it was for this reason that the ships were fitted with a unique desalination system which, given the materials in use at the time, would have produced large quantities of water with a very high lead content. William Battersby has argued that this is a much more likely source for the high levels of lead observed in the remains of expedition members than the tinned food.

A further survey of the graves was undertaken in 1986. A camera crew filmed the procedure, shown in a 1988 episode of the American programme Nova. Under difficult field conditions, Derek Notman, a radiologist and medical doctor from the University of Minnesota, and radiology technician Larry Anderson took many X-rays of the crewmen prior to autopsy. Barbara Schweger, an Arctic clothing specialist, and Roger Amy, a pathologist, assisted in the investigation.

Beattie and his team had noticed that someone else had attempted to exhume Hartnell. In the effort, a pickaxe had damaged the wooden lid of his coffin, and the coffin plaque was missing. Research in Edmonton later showed that Sir Edward Belcher, commander of one of the Franklin rescue expeditions, had ordered the exhumation of Hartnell in October 1852, but was thwarted by the permafrost. One month later, Edward A. Inglefield, commander of another rescue expedition, succeeded with the exhumation and removed the coffin's plaque.

Unlike Hartnell's grave, the grave of Private William Braine was largely intact. When he was exhumed, the survey team saw signs that his burial had been hasty. His arms, body and head had not been positioned carefully in the coffin, and one of his undershirts had been put on backwards. The coffin seemed too small for him; its lid had pressed down on his nose. A large copper plaque with his name and other personal data punched into it adorned his coffin lid.

NgLj-2 excavations (1992)
In 1992, Franklin scholar Barry Ranford and his colleague, Mike Yarascavitch, discovered human skeletal remains and artefacts of what they suspected to be some of the lost crewmen of the expedition. The site matches the physical description of McClintock's "boat place". In 1993, a team of archaeologists and forensic anthropologists returned to the site, which they referenced as "NgLj-2", on the western shores of King William Island, to excavate these remains. These excavations uncovered nearly 400 bones and bone fragments, and physical artefacts ranging from pieces of clay pipes to buttons and brass fittings. Examination of these bones by Anne Keenleyside, the expedition's forensic scientist, showed elevated levels of lead and many cut-marks "consistent with de-fleshing". On the basis of this expedition, it has become generally accepted that at least some of Franklin's men resorted to cannibalism in their final distress.

A study published in the International Journal of Osteoarchaeology in 2015 concluded that in addition to the de-fleshing of bones, thirty-five "bones had signs of breakage and 'pot polishing,' which occurs when the ends of bones heated in boiling water rub against the cooking pot they are placed in", which "typically occurs in the end stage of cannibalism, when starving people extract the marrow to eke out the last bit of calories and nutrition they can."

King William Island (1994–1995)
In 1994, Woodman organised and led a land search of the area from Collinson Inlet to (modern) Victory Point in search of the buried "vaults" spoken of in the testimony of the contemporary Inuit hunter Supunger. A ten-person team spent ten days in the search, sponsored by the Royal Canadian Geographical Society and filmed by the Canadian Broadcasting Corporation (CBC). No trace of the vaults was found.

In 1995, an expedition was jointly organised by Woodman, George Hobson and American adventurer Steven Trafton  with each party planning a separate search. Trafton's group travelled to the Clarence Islands to investigate Inuit stories of a "white man's cairn" there but found nothing. Hobson's party, accompanied by archaeologist Margaret Bertulli, investigated the "summer camp" found a few miles to the south of Cape Felix, where some minor Franklin relics were found. Woodman, with two companions, travelled south from Wall Bay to Victory Point and investigated all likely campsites along this coast, finding only some rusted cans at a previously unknown campsite near Cape Maria Louisa.

Wreck searches (1997–2013)
In 1997, a "Franklin 150" expedition was mounted by the Canadian film company Eco-Nova to use sonar to investigate more of the priority magnetic targets found in 1992. The senior archaeologist was Robert Grenier, assisted by Margaret Bertulli, and Woodman again acted as expedition historian and search coordinator. Operations were conducted from the Canadian Coast Guard icebreaker Laurier. Approximately  were surveyed, without result, near Kirkwall Island. When detached parties found Franklin relics – primarily copper sheeting and small items – on the beaches of islets to the north of O'Reilly Island the search was diverted to that area, but poor weather prevented significant survey work before the expedition ended. A documentary, Oceans of Mystery: Search for the Lost Fleet, was produced by Eco-Nova about this expedition.

Three expeditions were mounted by Woodman to continue the magnetometer mapping of the proposed wreck sites: a privately sponsored expedition in 2001, and the Irish-Canadian Franklin Search Expeditions of 2002 and 2004. These made use of sled-drawn magnetometers working on the sea ice and completed the unfinished survey of the northern (Kirkwall Island) search area in 2001, and the entire southern O'Reilly Island area in 2002 and 2004. All of the high-priority magnetic targets were identified by sonar through the ice as geological in origin. In 2002 and 2004, small Franklin artefacts and characteristic explorer tent sites were found on a small islet northeast of O'Reilly Island during shore searches.

In August 2008 a new search by Parks Canada was announced, to be led by Grenier. This search hoped to take advantage of the improved ice conditions, using side-scan sonar from a boat in open water. Grenier also hoped to draw from newly published Inuit testimony collected by oral historian Dorothy Harley Eber. Some of Eber's informants placed the location of one of Franklin's ships in the vicinity of the Royal Geographical Society Island, an area not searched by previous expeditions. The search was to also include local Inuit historian Louie Kamookak, who had found other significant remains of the expedition and would represent the indigenous culture.

HMS Investigator became icebound in 1853 while searching for Franklin's expedition and was subsequently abandoned. It was found in shallow water in Mercy Bay on 25 July 2010, along the northern coast of Banks Island in Canada's western Arctic. The Parks Canada team reported that it was in good shape, upright in about  of water.

A new search was announced by Parks Canada in August 2013.

Victoria Strait Expedition: wreck of Erebus (2014)

On 1 September 2014, a larger search by a Canadian team under the banner of the "Victoria Strait Expedition" found two items on Hat Island in the Queen Maud Gulf near King William Island: a wooden object, possibly a plug for a deck hawse, the iron pipe through which the ship's chain cable would descend into the chain locker below; and part of a boat-launching davit bearing the stamps of two Royal Navy broad arrows.

On 9 September 2014, the expedition announced that on 7 September it had located one of Franklin's two ships. The ship is preserved in good condition, with side-scan sonar picking up even the deck planking. The wreck lies in about  of water at the bottom of Wilmot and Crampton Bay in the eastern part of Queen Maud Gulf, west of O'Reilly Island. On 1 October at the House of Commons, Canadian Prime Minister Stephen Harper confirmed the wreck was that of HMS Erebus. A documentary, Hunt for the Arctic Ghost Ship, was produced by Lion Television for Channel 4's Secret History series in 2015.

In September 2018, Parks Canada announced that Erebus had deteriorated significantly. "An upwards buoyant force acting on the decking combined with storm swell in relatively shallow water caused the displacement," according to a spokesperson. The underwater exploration in 2018 totalled only a day and a half due to weather and ice conditions and was to continue in 2019. Also in September 2018, a report provided specifics as to ownership of the ships and contents: the United Kingdom will own the first 65 artefacts brought up from Erebus, while the wreck of both ships and other artefacts will be jointly owned by Canada and the Inuit.

Arctic Research Foundation Expedition: wreck of Terror (2016)
On 12 September 2016, it was announced that the Arctic Research Foundation expedition had found the wreck of HMS Terror to the south of King William Island in Terror Bay, at  at a depth of , and in "pristine" condition.

In 2018, a team examined the wreck of Terror using a remotely operated underwater vehicle (ROV) that collected photos and video clips of the ship and a number of artefacts. The group concluded that Terror had not been left at anchor, since anchor cables were seen to be secured along the bulwarks.

Scientific conclusions

Reasons for failure
The FEFAP field surveys, excavations and exhumations spanned more than ten years. The results of this study showed that the Beechey Island crew had most probably died of pneumonia and perhaps tuberculosis, which was suggested by the evidence of Pott disease discovered in Braine. Toxicological reports pointed to lead poisoning as a likely contributing factor. Blade cut marks found on bones from some of the crew were seen as signs of cannibalism. Evidence suggested that a combination of cold, starvation and disease including scurvy, pneumonia and tuberculosis, all made worse by lead poisoning, killed everyone in the Franklin party.

More recent chemical re-examination of bone and nail samples taken from Hartnell and other crew members has cast doubt on the role of lead poisoning. A 2013 study determined that the levels of lead present in the crew members' bones had been consistent during their lives, and that there was no isotopic difference between lead concentrated within older and younger bone materials. Had the crew been poisoned by lead from the solder used to seal the canned food or from the ships' water supplies, both the concentration of lead and its isotopic composition would have been expected to have "spiked" during their last few months. This interpretation was supported by a 2016 study that suggested the crew's ill health may in fact have been due to malnutrition, and specifically zinc deficiency, probably due to a lack of meat in their diet. This study used micro-X-ray fluorescence to map the levels of lead, copper and zinc in Hartnell's thumbnail over the final months of his life, and found that apart from during his last few weeks lead concentrations within Hartnell's body were within healthy limits. In contrast, levels of zinc were far lower than normal and indicated that Hartnell would have been suffering from chronic zinc deficiency, sufficient to have severely suppressed his immune system and left him highly vulnerable to a worsening of the tuberculosis with which he was already infected. In the last few weeks of his life, his illness would have caused his body to start breaking down bone, fat and muscle tissues, releasing lead previously stored there into his bloodstream and giving rise to the high lead levels noted in previous analysis of soft tissues and hair.

Franklin's chosen passage down the west side of King William Island took Erebus and Terror into "a ploughing train of ice ... [that] does not always clear during the short summers", whereas the route along the island's east coast regularly clears in summer and was later used by Roald Amundsen in his successful navigation of the Northwest Passage. The Franklin expedition, locked in ice for two winters in Victoria Strait, was naval in nature and therefore not well-equipped or trained for land travel. Some of the crewmembers heading south from Erebus and Terror hauled in many items not needed for Arctic survival. McClintock noted a large quantity of heavy goods in the lifeboat at the "boat place" and thought them "a mere accumulation of dead weight, of little use, and very likely to break down the strength of the sledge-crews".

Other findings
In 2017, Douglas Stenton, an adjunct professor of anthropology at the University of Waterloo and former director of Nunavut's Department of Heritage and Culture, suggested that four sets of human remains found on King William Island could possibly be women. He initially suspected that DNA testing would not offer up anything more, but to his surprise they registered that there was no 'Y' chromosomal element to the DNA. Stenton acknowledged that women were known to have served in the Royal Navy in the 17th, 18th and early 19th centuries, but he also pointed out that it could be that the DNA had simply degraded as further tests proved ambiguous and he concluded the initial findings were "almost certainly incorrect".

In 1993, three bodies were found at site NgLj-3 near Erebus Bay. The remains had originally been found by McClintock's expedition in 1859, and were rediscovered and buried by Schwatka two decades later. In 2013, a team led by Stenton had the remains exhumed for DNA testing and forensic facial reconstruction. The team's report, published in Polar Journal in 2015, indicated that the reconstructions of the two intact skulls from the remains resembled Lieutenant Gore and Ice-Master Reid of the Erebus; however, it was determined the remains could not have belonged to Gore, as the Victory Point note stated that Gore had died before the abandonment of the ships in April 1848.

In May 2021, one of the bodies was positively identified as that of Warrant Officer John Gregory, an engineer aboard Erebus. A genealogy team tracked down Gregory's great-great-great-grandson, Jonathan Gregory, residing in Port Elizabeth, South Africa, and confirmed the familial match through DNA testing.

Timeline

Legacy

Historical
The most meaningful outcome of the Franklin expedition was the mapping of several thousand miles of hitherto unsurveyed coastline by expeditions searching for Franklin's lost ships and crew. As Richard Cyriax noted, "the loss of the expedition probably added much more [geographical] knowledge than its successful return would have done". At the same time, it largely quelled the Admiralty's appetite for Arctic exploration. There was a gap of many years before the Nares expedition and Sir George Nares' declaration there was "no thoroughfare" to the North Pole; his words marked the end of the Royal Navy's historical involvement in Arctic exploration, the end of an era in which such exploits were widely seen by the British public as worthy expenditures of human effort and monetary resources. Given how difficult and risky it was for professional explorers to cross the Northwest Passage, it would be impossible for the average merchant ships of the day to use this route for trade.

As a writer for The Athenaeum put it, "We think that we can fairly make out the account between the cost and results of these Arctic Expeditions, and ask whether it is worth while to risk so much for that which is so difficult of attainment, and when attained, is so worthless." The navigation of the Northwest Passage in 1903–05 by Roald Amundsen with the Gjøa expedition ended the centuries-long quest for the route.

The Northwest Passage discovered

Franklin's expedition explored the vicinity of what was ultimately one of many Northwest Passages to be discovered. While the more famous search expeditions were underway in 1850, Robert McClure set out on the little-known McClure Arctic expedition on HMS Investigator to also investigate the fate of Franklin's voyage. While he did not find much evidence of Franklin's fate, he did finally ascertain an ice-bound route that connected the Atlantic Ocean to the Pacific Ocean. This was the Prince of Wales Strait, which was far to the north of Franklin's ships.

On 21 October 1850, the following entry was recorded in 's log:

"October 31st, the Captain returned at 8.30. A.M., and at 11.30. A.M., the remainder of the parting, having, upon the 26th instant, ascertained that the waters we are now in communicate with those of Barrow Strait, the north-eastern limit being in latitude 73°31′, N. longitude 114°39′, W. thus establishing the existence of a NORTH-WEST PASSAGE between the Atlantic and Pacific Oceans."

McClure was knighted for his discovery. While the McClure expedition obviously fared much better than Franklin's voyage, it was similarly beset by immense challenges (including the loss of Investigator and four winters on the ice) and a number of controversies, including allegations of selfishness and poor planning on McClure's part. His decision to place numerous message cairns along his route ultimately saved his expedition, who were ultimately found and rescued by the crew of .

In 1855, a British parliamentary committee concluded that McClure "deserved to be rewarded as the discoverer of a Northwest Passage". Today, the question of who actually discovered the Northwest Passage is a subject of controversy, as all the different Passages have varying degrees of navigability. Although he did confirm the first geographical Northwest Passage that is navigable by ship under ideal conditions, McClure is rarely credited in modern times due to his troubled expedition, his poor personal reputation, the fact that his expedition was after Franklin's (who has a claim to be the first discoverer, see below) and the fact that he never traversed the strait that he found, instead choosing to portage over Banks Island.

Simpson Strait
Members of the Franklin expedition crossed the southern shore of King William Island and made it onto the Canadian mainland; this is evident by the fact that human remains from the expedition have been found inland on the Adelaide Peninsula. This may have involved walking across the Simpson Strait, which has since been recognised as one of the Northwest Passages to the Pacific. As none of the members of the expedition survived, it is not known whether any member of the party had realised this. George Back had discovered the strait in 1834 but did not realise it was a Northwest Passage. In any case, by 1854, it was widely believed that the remnants of the expedition had crossed the strait, and Lady Franklin was informed of such on 12 January by the Admiralty.

Franklin's claim to having discovered the Passage was strengthened by Charles Richard Weld's assertion that Franklin had long suspected that the Simpson Strait did connect the two oceans. In 1860, McClintock ascertained that the strait was indeed a Northwest Passage. Following this discovery, to honour Franklin's legacy, the Royal Geographical Society declared that his lost expedition was the first expedition to discover the Passage. Lady Franklin was given a medal in his name.

The Northwest Passage would not be fully navigated by boat until 1906, when Roald Amundsen famously traversed the passage on the Gjøa via the Simpson Strait.

Cultural depictions

Commemoration

For years after the loss of the Franklin expedition, the Victorian media portrayed Franklin as a hero who led his men in the quest for the Northwest Passage. A statue of Franklin in his hometown bears the inscription "Sir John Franklin – Discoverer of the North West Passage", and statues of Franklin outside the Athenaeum in London and in Tasmania bear similar inscriptions. Although the expedition's fate, including the possibility of cannibalism, was widely reported and debated, Franklin's standing with the Victorian public was undiminished. The expedition has been the subject of numerous works of non-fiction.

The mystery surrounding the expedition was the subject of three episodes of the PBS programme Nova, broadcast in 1988, 2006 and 2015; a 2007 television documentary, "Franklin's Lost Expedition", on Discovery HD Theatre; as well as a 2008 Canadian documentary, Passage. In a 2009 episode of the ITV travel documentary series Billy Connolly: Journey to the Edge of the World, presenter Billy Connolly and his crew visited Beechey Island, filmed the grave site and gave details of the expedition.

In memory of the lost expedition, one of Canada's Northwest Territories subdivisions was known as the District of Franklin. Including the high Arctic islands, this jurisdiction was abolished when the area was set off into the newly created Nunavut Territory on 1 April 1999.

On 29 October 2009, a special service of thanksgiving was held in the chapel at the Old Royal Naval College in Greenwich, to accompany the rededication of the national monument to Franklin there. The service also included the solemn re-interment of the only remains from Erebus to be repatriated to England, entombed within the monument in 1873 (previously thought to be Le Vesconte, but may actually have been Goodsir). The following day, a group of polar authors went to London's Kensal Green Cemetery to pay their respects to the Arctic explorers buried there.

Many other veterans of the searches for Franklin are buried there too, including Admiral Sir Horatio Thomas Austin, Admiral Sir George Back, Admiral Sir Edward Augustus Inglefield, Admiral Bedford Pim, and Admiral Sir John Ross. Franklin's wife, Lady Franklin, is also interred at Kensal Green in the vault and commemorated on a marble cross dedicated to her niece, Sophia Cracroft.

Literary works
From the 1850s through to the present day, Franklin's lost expedition inspired numerous literary works. Among the first was a play, The Frozen Deep, written by Wilkie Collins with assistance and production by Charles Dickens. The play was performed for private audiences at Tavistock House early in 1857, as well as at the Royal Gallery of Illustration (including a command performance for Queen Victoria) and for the public at the Manchester Trade Union Hall. News of Franklin's death in 1859 inspired elegies, including one by Algernon Charles Swinburne.

Fictional treatments of the expedition begin with Jules Verne's Journeys and Adventures of Captain Hatteras, (1866), in which the novel's hero seeks to retrace Franklin's footsteps and discovers that the North Pole is dominated by an enormous volcano. Verne also remembers the efforts of Lady Franklin to discover the fate of her husband in Mistress Branican (1891), which stages a similar plot but situated in Oceania and Australia instead of the North Pole. Mark Twain briefly satirised the fate of the expedition and its subsequent searches in the beginning of the story "Some Learned Fables for Good Old Boys and Girls" (1875). The German novelist Sten Nadolny's The Discovery of Slowness (1983; English translation 1987) takes on the entirety of Franklin's life, touching only briefly on his last expedition.

Other recent novelistic treatments of Franklin include William T. Vollmann's The Rifles (1994), John Wilson's North With Franklin: The Journals of James Fitzjames (1999); and Dan Simmons's The Terror (2007), the third of which was developed as a 2018 AMC television series of the same name. The expedition has also been the subject of a horror role-playing game supplement for Call of Cthulhu, The Walker in the Wastes. Most recently, Clive Cussler's 2008 novel Arctic Drift incorporates the ordeal of the expedition as a central element in the story, and Richard Flanagan's Wanting (2009) deals with Franklin's deeds in both Tasmania and the Arctic. On 12 January 2012, BBC Radio 4 broadcast Erebus, a radio play based on the expedition by British poet Jo Shapcott. Kassandra Alvarado's 2013 novel The White Passage presents a vaguely science-fiction take on an alternative history of the expedition.

Michael Palin's 2018 book, Erebus, The Story of a Ship, was described by The Guardian newspaper as 'lively and diligent.' He also produced a one man show based on his book. A children's novel, Chasing Ghosts – An Arctic Adventure by Nicola Pierce featuring the expedition was published in 2020.

In 2017, The Breathing Hole, a play written by Colleen Murphy, premiered at the Stratford Festival, directed by Reneltta Arluk. In this play, the fates of the crew of Erebus and Terror are featured within the context of an epic saga spanning five-hundred years. Commissioned to mark Canada's 150th Anniversary and met with critical acclaim, the work involved artists from both Nunavut and the rest of Canada, including collaborations with Qaggiavuut Nunavut Performing Arts. In 2020, the play was published in a dual-language edition in English and in Natsilingmiutut syllabics—the Inuktitut dialect from where the story takes place in the central Arctic.

Artistic works
In the visual arts, the loss of Franklin's expedition inspired a number of paintings in both the United States and Britain. In 1861, Frederic Edwin Church unveiled his great canvas The Icebergs; later that year, prior to taking it to England for exhibition, he added an image of a broken ship's mast in silent tribute to Franklin. In 1864, Sir Edwin Landseer's Man Proposes, God Disposes caused a stir at the annual Royal Academy exhibition; its depiction of two polar bears, one chewing on a tattered ship's ensign, the other gnawing on a human ribcage, was seen at the time as in poor taste, but has remained one of the most powerful imaginings of the expedition's final fate. The expedition also inspired numerous popular engravings and illustrations, along with many panoramas, dioramas and magic lantern shows.

Musical works
Franklin's last expedition also inspired a great deal of music, beginning with the ballad "Lady Franklin's Lament" (also known as "Lord Franklin"), which originated in the 1850s and has been recorded by dozens of artists, among them Martin Carthy, Pentangle, Sinéad O'Connor, and The Pearlfishers. The Scottish pirate metal band Alestorm's song "Magnetic North" is dedicated to the expedition . Other Franklin-inspired songs include James Taylor's "Frozen Man" (based on Beattie's photographs of John Torrington) and Iron Maiden's "Stranger In A Strange Land". German band  Janus in 2021 released an over 30 minutes long song "Terror" and later an audiobook "Terror - Das Hörbuch" which contains Franklin's log entries.

Significance in Canada
The influence of the Franklin expedition on Canadian literature and culture has been especially significant. Among the best-known modern Franklin ballads is "Northwest Passage" by the late Ontario folksinger Stan Rogers (1981), which has been referred to as the unofficial Canadian national anthem. The distinguished Canadian novelist Margaret Atwood has also spoken of Franklin's expedition as a sort of national myth of Canada, remarking that "In every culture many stories are told, (but) only some are told and retold, and these stories bear examining ... in Canadian literature, one such story is the Franklin expedition."

Notable treatments by Canadian poets include a verse play for radio, Terror and Erebus which was commissioned from Gwendolyn MacEwen, broadcast by CBC Radio (10 January 1965) and subsequently published in her collection Afterworlds (1987); and David Solway's verse cycle, Franklin's Passage (2003). The events have also featured prominently in Canadian novels, including Mordecai Richler's Solomon Gursky Was Here (1989) and Dominique Fortier's 2008 French language novel, Du bon usage des étoiles, which creatively considers the Franklin expedition from a variety of perspectives and genres and was both shortlisted and a finalist for several literary awards in Canada (2009 Governor General's Awards). Sheila Fischman's translation of Fortier's novel, On the Proper Use of Stars, was shortlisted for the 2010 Governor General's Awards for French to English Translation. Irish-Canadian writer Ed O'Loughlin's novel Minds of Winter was shortlisted for the 2017 Giller Prize.

See also
 List of people who disappeared mysteriously at sea

Notes
 The date given in the message is wrong, as Franklin wintered one year earlier at Beechey Island.

References

Works cited

Further reading

External links

 "Franklin's Last Voyage" at CanadianMysteries.ca
 Video of Parks Canada dive on the wreck of HMS Terror

1840s missing person cases
1845 in Canada
1845 in the British Empire
19th century in the Arctic
Arctic expeditions
Expeditions from the United Kingdom
Exploration of the Arctic
Formerly missing people

Geography of Canada
History of Nunavut
History of the Northwest Territories
Incidents of cannibalism
Lead poisoning incidents
Maritime history of Canada
Mass disappearances
Missing person cases in Canada
American Geographical Society

Franklin's lost expedition


"Baila Esta Cumbia" () is a song by American singer Selena. The song was the lead single from Ven Conmigo (1990). It peaked at number-one on the Mexican Singles Chart (1994), Italy Singles Chart (1996), Argentinian Singles Chart (1994) and France Singles Chart (1995). It peaked in the top 20 on the US Hot Latin Tracks (1990), Latin Regional Mexican Airplay (1991) chart and the Spanish Singles Chart (1996). It then became one of Selena's signature songs. Her brother, A.B. Quintanilla III remixed the song as "Baila Esta Kumbia". It peaked at number 44 on the US Hot Latin Tracks and number 16 on the Latin Regional Mexican Airplay chart. A.B. performed the song during the Selena ¡VIVE! tribute concert with his band.

Selena songs
1990 songs
Songs written by A.B. Quintanilla
Spanish-language songs

Baila Esta Cumbia


The Pageant of Labour was a large-scale musical and dramatic show held at The Crystal Palace, London, England, on 15–20 October 1934. With words by Matthew Anderson and music by Alan Bush, it celebrated the history of the British labour movement, and like most pageants of the era was a mixture of instrumental and choral music, drama and dance. It was organised by the Central Women's Organisation Committee of the London Trades Council and directed by Edward Genn. Bush and Michael Tippett conducted the choir and orchestra. Among the cast was the 15-year-old Nigel Stock.

References

Official Book and Programme of the Pageant of Labour, 1934

External links

Festivals in London
British trade unions history
1934 in England

Pageant of Labour


Patrik Ringborg (born 1 November 1965) is a Swedish conductor, member of the Royal Swedish Academy of Music.

Career
Born in Stockholm, as a student Ringborg attended the Adolf Fredrik's Music School in Stockholm. After studies at the Royal College of Music in Stockholm and with Kurt Bendix, Ringborg was a répétiteur at the Royal Swedish Opera in Stockholm from 1989 to 1993, also assisting the Music Director and conducting performances in the Royal Opera House. He also assisted the Music Directors at the Semperoper in Dresden (1988) and at the Canadian Opera Company (1992).

From 1993 to 1999, Ringborg worked as staff conductor with the Freiburg Opera, where his position in 1997 was elevated to Deputy Music Director. From 1997 to 2003, he conducted at the Aalto Theatre in Essen, where in 1999 he was appointed Principal Conductor. After Ringborg's first year in Essen, critics named him the "season's best conductor" together with John Fiore and Essen's music director Stefan Soltesz. Ringborg made his debut at the Gothenburg Opera in 1998 with Tannhäuser, and later was named its Principal Guest Conductor. There he also conducted the much acclaimed world premiere of Notorious by Hans Gefors in 2015. He also was the Artistic Director of the German Kurt Weill Festival 2000.

Until July 2007, Ringborg was chief conductor with the Freiburg Opera. With the 2007/2008 season, Ringborg became music director at the Staatstheater Kassel, where he also was the artistic director of the "Mahler-Festtage" (celebrated every second year in honour of the late Music Director in Kassel, Gustav Mahler) until 2017.

Ringborg led the Royal Stockholm Philharmonic Orchestra at the Nobel Prize Award Ceremony 2008, the last opera performances of Dame Kiri Te Kanawa in Cologne (Der Rosenkavalier, 2010), and conducted Elektra with the Stockholm Royal Opera at the Savonlinna Opera Festival in 2010.

As first conductor ever, Patrik Ringborg was awarded the Opera Prize, founded by renowned Swedish newspaper Svenska Dagbladet for the Swedish productions of Das Rheingold and Parsifal.

Selected opera productions
Salome: Freiburg Theatre (concert), 1997
Cavalleria rusticana/Pagliacci: Gothenburg Opera, 1999
Faust: Aalto Theatre, Essen, 2000
Hänsel und Gretel: Aalto Theatre, Essen, 2000
Orpheus by Hans Werner Henze: Aalto Theatre, Essen, 2001
Manon Lescaut: Gothenburg Opera, 2002
Andrea Chénier: Aalto Theatre, Essen, 2003
Tristan und Isolde: Gothenburg Opera, 2003
Die Walküre: Gothenburg Opera, 2004
Lady Macbeth of the Mtsensk District: Deutsches Nationaltheater Weimar, 2006
Das Rheingold: Freiburg Theatre, 2006
Elektra: Freiburg Theatre, 2007
Peter Grimes: Kassel State Theatre
Tosca: Deutsches Nationaltheater Weimar, 2008
Salome: Kassel State Theatre, 2008
Dialogues des Carmélites: Kassel State Theatre, 2009
Elektra: Oslo Opera, 2009
Die Meistersinger von Nürnberg: Kassel State Theatre, 2010
Der Rosenkavalier: Cologne Opera, 2010
Lear: Kassel State Theatre, 2010
Lohengrin: Kassel State Theatre, 2011
Salome: Gothenburg Opera, 2011
Lady Macbeth of the Mtsensk District: Kassel State Theatre, 2011
The Magic Flute: Kassel State Theatre, 2011
Parsifal: Kassel State Theatre, 2012
Così fan tutte: Kassel State Theatre, 2012
Tannhäuser: Kassel State Theatre, 2013
Parsifal: Royal Opera Stockholm, 2013
Die Frau ohne Schatten: Kassel State Theatre, 2014
Der Rosenkavalier: Kassel State Theatre, 2014
Turandot: Kassel State Theatre, 2015
Notorious: Gothenburg Opera, World Première 2015
Die tote Stadt: Kassel State Theatre, 2016
Elektra: Kassel State Theatre, 2017
Ariadna auf Naxos: Gothenburg Opera, 2018
Autumnsonata: Malmö Opera, 2019

Selected recordings
"Växlar". Stockholms Läns Blåsarsymfoniker. Conductor: Patrik Ringborg. Oeuvres for wind orchester from the 20th century by e.g. Hugo Alfvén, Anders Hillborg and Erland von Koch, Twin Music TMCD-18, 1993.
"Höga Visan". Sveriges Radios Symfoniorkester, Radiokören. Conductors: Patrik Ringborg, Mats Rondin and Manfred Honeck. Works by Natanael Berg, Phono Suecia PSCD 721, 2003.

References

Sources
 wagnerspectrum. Werktreue bei Wagner. Der Dirigent Patrik Ringborg im Gespräch mit Egon Voss. Koenigshausen + Neumann Verlag 2005.
 Nationalencyklopedin, Supplementband 3. Article "Patrik Ringborg". NE Förlag 1999.
 Die Walküre by Richard Wagner. Act II, Schott Music 2004. ISMN M-001-12529-1
 Die Walküre by Richard Wagner. Act III, Schott Music 2005. ISMN M-001-12974-9
 A Gallery Carol av Patrik Ringborg. SK Förlag 1985. ISMN M-070-01675-9
 Europa Publications: International Who's Who in Classical Music 2003, 19th edition, Routledge, 2003. 980 p.,
 Ruth Renée Reif: Die Stuttgarter Philharmoniker, ein historisches Porträt, Tübingen: Silberburg-Verlag, 1999.
 Swedish choral music, a selective catalogue, Stockholm: Svensk Musik, 1988, 60 p.

External links
 Staatstheater Kassel German-language biography of Ringborg
 Website on the conductor Patrik Ringborg
 Patrik Ringborgs official Facebook page

1965 births
Living people
Musicians from Stockholm
Royal College of Music, Stockholm alumni
Swedish conductors (music)
Male conductors (music)
21st-century conductors (music)
21st-century Swedish male musicians

Patrik Ringborg


The ozone–oxygen cycle is the process by which ozone is continually regenerated in Earth's stratosphere, converting ultraviolet radiation (UV) into heat. In 1930 Sydney Chapman resolved the chemistry involved. The process is commonly called the Chapman cycle by atmospheric scientists.

Most of the ozone production occurs in the tropical upper stratosphere and mesosphere. The total mass of ozone produced per day over the globe is about 400 million metric tons. The global mass of ozone is relatively constant at about 3 billion metric tons, meaning the Sun produces about 12% of the ozone layer each day.

Photochemistry

The Chapman cycle describes the main reactions that naturally determine, to first approximation, the concentration of ozone in the stratosphere. It includes four processes - and a fifth, less important one - all involving oxygen atoms and molecules, and UV radiation:

Creation
An oxygen molecule is split (photolyzed) by higher frequency UV light (top end of UV-B, UV-C and above) into two oxygen atoms (see figure):
1. oxygen photodissociation: O2 + ℎν(<242 nm) → 2 O
Each oxygen atom may then combine with an oxygen molecule to form an ozone molecule:
2. ozone creation: O + O2 + A → O3 + A
where A denotes an additional molecule or atom, such as N2 or O2, required to maintain the conservation of energy and momentum in the reaction. Any excess energy is produced as kinetic energy.

The ozone–oxygen cycle
The ozone molecules formed by the reaction (above) absorb radiation with an appropriate wavelength between UV-C and UV-B. The triatomic ozone molecule becomes diatomic molecular oxygen, plus a free oxygen atom (see figure):
3. ozone photodissociation: O3 + ℎν(240–310 nm) → O2 + O
The atomic oxygen produced may react with another oxygen molecule to reform ozone via the ozone creation reaction (reaction 2 above).

These two reactions thus form the ozone–oxygen cycle, wherein the chemical energy released by ozone creation becomes molecular kinetic energy. The net result of the cycle is the conversion of penetrating UV-B light into heat, without any net loss of ozone. While keeping the ozone layer in stable balance, and protecting the lower atmosphere from harmful UV radiation, the cycle also provides one of two major heat sources in the stratosphere (the other being kinetic energy, released when  O2 is photolyzed into individual O atoms).

Removal
If an oxygen atom and an ozone molecule meet, they recombine to form two oxygen molecules:
4. ozone conversion: O3 + O → 2 O2
Two oxygen atoms may react to form one oxygen molecule:
5. oxygen recombination: 2O + A → O2 + A
as in reaction 2 (above), A denotes another molecule or atom, like N2 or O2 required for the conservation of energy and momentum.
Note that reaction 5 is of the least importance in the stratosphere, since, under normal conditions, the concentration of oxygen atoms is much lower than that of diatomic oxygen molecules. This reaction is therefore less common than ozone creation (reaction 2).

The overall amount of ozone in the stratosphere is determined by the balance between production from solar radiation and its removal. The removal rate is slow, since the concentration of free O atoms is very low.

Additional reactions
In addition to these five reactions, certain free radicals - the most important being hydroxyl (OH), nitric oxide (NO), and atomic chlorine (Cl) and bromine (Br) -  catalyze the recombination reaction, leading to an ozone layer that is thinner than it would be if the catalysts were not present.

Most OH and NO are naturally present in the stratosphere, but human activity - especially emissions of chlorofluorocarbons (CFCs) and halons - has greatly increased the concentration of Cl and Br, leading to ozone depletion. Each Cl or Br atom can catalyze tens of thousands of decomposition reactions before it is removed from the stratosphere.

Main reactions in different atmospheric layers

Thermosphere
For given relative reactants concentrations, The rates of ozone creation and oxygen recombination (reactions 2 and 5) are proportional to the air density cubed, while the rate of ozone conversion (reaction 4) is proportional to the air density squared, and the photodissociation reactions (reactions 1 and 3) have a linear dependence on air density. Thus, at the upper thermosphere, where air density is very low and photon flux is high, oxygen photodissociation is fast while ozone creation is low, thus its concentration is low. Thus the most important reactions are oxygen photodissociation and oxygen recombination, with most of the oxygen molecules dissociated to oxygen atoms.

As we go to the lower thermosphere (e.g. 100 km height and below), the photon flux in the <170 nm wavelengths drops sharply due to absorption by oxygen in the oxygen photodissociation reaction (reaction 1). This wavelength regime has the highest cross section for this reaction (10-17 cm2 per oxygen molecule), and thus the rate of oxygen photodissociation per oxygen molecule decreases significantly at these altitudes, from more than 10-7 per second (about once a month) at 100 km to 10-8 per second (about once every few years) at 80 km . As a result, the atomic oxygen concentration (both relative and absolute) decreases sharply, and ozone creation (reaction 2) is ongoing, leading to a small but non-negligible ozone presence.

Note that temperatures also drop as altitude decreases, because lower photon photodissociation rates mean lower heat production per air molecule.

Below thermosphere: Reaction rates at steady state
Odd oxygen species (atomic oxygen and ozone) have net creation rate only by oxygen dissociation (reaction 1), and net destruction by either ozone conversion or oxygen recombination (reactions 4 and 5). At steady state these processes are balanced, so the rates of these reactions obey:
(rate of reaction 1) = (rate of reaction 4) + (rate of reaction 5).

At steady state, ozone creation is also balanced with its removal. so:
(rate of reaction 2) = (rate of reaction 3) + (rate of reaction 4).

It thus follows that:
(rate of reaction 2) + (rate of reaction 5) = (rate of reaction 3) + (rate of reaction 1).
The right-hand side is the total photodissociation rate, of either oxygen or ozone.

Below the thermosphere, the atomic oxygen concentration is very low compared to molecular oxygen. Therefore, oxygen atoms are much more likely to hit oxygen (diatomic) molecules than to hit other oxygen atoms, making oxygen recombination (reaction 5) far rarer than ozone creation (reaction 2). Following the steady-state relation between the reaction rates, we may therefore approximate:
(rate of reaction 2) = (rate of reaction 3) + (rate of reaction 1)

Mesosphere

In the mesosphere, oxygen photodissociation dominates over ozone photodissociation, so we have approximately:
(rate of reaction 2) = (rate of reaction 1) =  (rate of reaction 4)

Thus, ozone is mainly removed by ozone conversion. Both ozone creation and conversion depend linearly on oxygen atom concentration, but in ozone creation an oxygen atom must encounter an oxygen molecule and another air molecule (typically nitrogen) simultaneously, while in ozone conversion an oxygen atom must only encounter an ozone molecule. Thus, when both reactions are balanced, the ratio between ozone and molecular oxygen concentrations is approximately proportional to air density.

Therefore, the relative ozone concentration is higher at lower altitudes, where air density is higher. This trend continues to some extent lower into the stratosphere, and thus as we go from 60 km to 30 km altitude, both air density and ozone relative concentration increase by ~40-50-fold.

Stratosphere
Absorption by oxygen in the mesosphere and thermosphere (in the oxygen photodissociation reaction) reduces photon flux at wavelengths below 200 nanometer, where oxygen photodissociation is dominated by Schumann–Runge bands and continuum, with cross-section of up to 10-17 cm2.
Due to this absorption, photon flux in these wavelengths is so low in the stratosphere, that oxygen photodissociation becomes dominated by the Hertzberg band of the 200-240 nm photon wavelength, even though the cross-section of this process is as low as 10-24 - 10-23 cm2. The ozone photodissociation rate per ozone molecule has a cross-section 6 orders of magnitude higher in the 220-300 nm wavelength range. With ozone concentrations in the order of 10-6-10-5 relative to molecular oxygen, ozone photodissociation becomes the dominant photodissociation reaction, and most of the stratosphere heat is generated through this procsees, with highest heat generation rate per molecule at the upper limit of the stratosphere (stratopause), where ozone concentration is already relatively high while UV flux is still high as well in those wavelengths, before being depleted by this same photodissociation process.

In addition to ozone photodissociation becoming a more dominant removal reaction, catalytic ozone destruction due to free radicals (mainly atomic hydrogen, hydroxyl, nitric oxide, chlorine and bromide) increases the effective ozone conversion reaction rate. Both processes act to increase ozone removal, leading to a more moderate increase of ozone relative concentration as altitude decreases, even though air density continues to increase.

Due to both ozone and oxygen growing density as we go to lower altitudes, UV photon flux at wavelengths below 300 nm decreases substantially, and oxygen photodissociation rates fall below 10-9 per second per molecule at 30 km. With decreasing oxygen photodissociation rates, odd-oxygen species (atomic oxygen and ozone molecules) are hardly formed de novo (rather than being transmuted to each other by the other reactions), and most atomic oxygen needed for ozone creation is derived almost exclusively from ozone removal by ozone photodissociation. Thus, ozone becomes depleted as we go below 30 km altitude and reaches very low concentrations at the tropopause.

Troposphere
In the troposphere, ozone formation and destruction are no longer controlled by the ozone-oxygen cycle. Rather, tropospheric ozone chemistry is dominated today by industrial pollutants other gases of volcanic source.

External links
Stratospheric Ozone: An Electronic Textbook
The Sun and the Earth's Climate

References

Cycle
Oxygen
Biogeochemical cycle
Atmospheric chemistry

Ozone–oxygen cycle


Liebeck v. McDonald's Restaurants is also known as the "McDonald's coffee case". It is a lawsuit between Stella Liebeck and McDonald's. Stella Liebeck was badly injured by hot coffee. She had bought the coffee from a McDonald's restaurant. A jury awarded her $2.86 million, but in the end she only got $640,000.

What happened to Stella Liebeck?
The accident with the hot coffee happened on February 27, 1992. Stella Liebeck was 79 years old. She bought a cup of coffee from the drive-through window of a McDonald's restaurant. When she opened the cup to add cream and sugar, she spilled the coffee on her lap. She was taken to the hospital and they found that she had bad burns. She had to stay in the hospital for eight days. She got skin grafting: they moved healthy skin to replace the burned skin. She lost a lot of weight. Her daughter had to care for her for 3 weeks when she came out of the hospital. The accident changed her body forever. She was disabled for 2 years.

What did she want?
Stella Liebeck wanted $20,000 from McDonald's. She needed to pay the hospital and her daughter. McDonald's offered only $800. Then Liebeck hired an attorney, Reed Morgan. Morgan said that the coffee was dangerous and asked $90,000, but McDonald's refused. That is why they needed a trial.

How did the trial go?
The attorney, Reed Morgan, showed examples of what McDonald's did wrong:

 Coffee from McDonald's had burned 700 people already.
 A doctor told that colder coffee causes less burns. And that the McDonald's coffee is too hot to drink.
 Other restaurants in the city serve colder coffee.

Then on August 18, 1994 the jury decided. They said that McDonald's was 80% wrong and Stella Liebeck was 20% wrong. The warning on the coffee cup was too small. Stella Liebeck got $160,000 to pay the hospital and her daughter. She also got $2,7 million so that McDonald's would not do it again. But the judge made it $640,000.

What happened then?

 Some people said that it was wrong that Stella Liebeck wanted a lawsuit. They said that it was wrong that she got so much money. But most of the money was to make McDonald's not do it again.
 McDonald's did not make their coffee colder.
 Stella Liebeck died on August 5, 2004. She was 91 years old. She paid a nurse with the money from the lawsuit.
 HBO made a film about this story: Hot Coffee.

United States law
1994 in the United States
1990s in law

Liebeck v. McDonald's Restaurants


In Christian theology, Dyophysitism (Greek: δυοφυσιτισμός, from δύο (dyo), meaning "two" and φύσις (physis), meaning "nature") is the Christological position that two natures, divine and human, co-exist in the unique person of Jesus Christ God.

According to Saint Athanasius of Alexandria, Jesus was true man and true God.

Beliefs

Dyophysite Christians believe that there is complete and perfect unity of the two natures in one hypostasis and one person of Jesus Christ. For the Chalcedonians, the hypostatic union was the center of Jesus's unity (his divinity and humanity being described as natures) whereas those who rejected the Chalcedonian definition saw his nature as the point of unity. The miaphysites upheld the idea of one nature in Christ based on their understanding of Cyril of Alexandria's Twelve Anathemas, namely number 4 which states "If anyone shall divide between two persons or subsistences those expressions which are contained in the Evangelical and Apostolical writings, or which have been said concerning Christ by the Saints, or by himself, and shall apply some to him as to a man separate from the Word of God, and shall apply others to the only Word of God the Father, on the ground that they are fit to be applied to God: let him be anathema." Since the term Dyophysitism is used for describing the Chalcedonian positions, it has a distinctive opposite meaning to the terms Monophysite (the notion that Christ has only one, divine nature) and Miaphysite (the notion that Christ is both divine and human, but in one nature).

Dyophisitism has also been used to describe some aspects of Nestorianism, the doctrines ascribed to Nestorius of Constantinople. It is now generally agreed that some of his ideas were not far from those that eventually emerged as orthodox, but the orthodoxy of his formulation of the doctrine of Christ is still controversial among churches.

The belief in Jesus Christ being true Man and true God was embedded in the Chalcedonian Creed.

Spread
Development of dyophysite Christology was gradual; Dyophysite tradition and its complex terminology were finally formulated as a result of long Christological debates that were constant during the 4th and 5th centuries. The importance of dyophysitism was often emphasized by prominent representatives of the Antiochene School. After many debates and several councils, Dyophysitism gained its official ecclesiastical form at the Fourth Ecumenical Council, held in Chalcedon in 451.

The Chalcedonian Definition became the basis for the Christological doctrine of the two natures of Jesus Christ, which is held up to the present day by a majority of Christian churches, including the Eastern Orthodox Church, the Roman Catholic Church, Eastern Catholic Churches, the Anglican Church, and the Old Catholic Church, as well as Reformed, Lutheran, and various other Christian denominations. This definition states that Christ is One Person and One Hypostasis in Two Natures. Apart from that, the ancient Church of the East has preserved dyophysite Christology and other traditions of the Antiochene School.

See also
First Council of Ephesus
Miaphysitism
Monophysitism
Nestorianism
Oriental Orthodoxy
Second Council of Constantinople

References

Citations

Sources

Christian terminology
Christology
Eastern Orthodox theology
Schisms in Christianity
Nature of Jesus Christ

Dyophysitism


Sy Landy (7 May 1931 – 28 November 2007) was an American Trotskyist politician.

Born in Brooklyn, Landy studied at Brooklyn College, where he joined the third camp Trotskyist Independent Socialist League (ISL), led by Max Shachtman. The ISL moved away from revolutionary politics and merged with Norman Thomas' Socialist Party in 1958. Schachtman and many of the "Schachtmanites" moved rapidly to the right. Landy was a prominent supporter of Hal Draper's left opposition to Shachtman's support for the Bay of Pigs invasion, joined Draper in splitting from the Socialist Party in the early 1960s.  During this period, he also became a member of the board of New Politics.

Draper founded the Independent Socialist Club (with the old "third camp" socialist politics), and Landy established the group in New York, initially one of its three main centres.  In 1969, it became the International Socialists (IS), and Landy retained a leadership role, but he became increasingly interested in the ideas of black power and the ideals of the French uprising of May 1968.  Within the IS, he became a leader of the opposition "Revolutionary Tendency".  This split in 1973 to form the Revolutionary Socialist League.  Although he was elected to the Central Committee of the new organisation, in 1975 he opened a debate over what he believed was an increasing stagist tendency, and the organisation's refusal to call for a global general strike under then current circumstances. He was soon expelled from the organisation alongside Walter Daum, and the two's supporters, who had formed the "Revolutionary Party Tendency", soon joined them in founding the League for the Revolutionary Party (LRP).

Sy Landy remained the National Secretary of the LRP until his death, occasionally working as a teacher in Jersey City.  In 1992, he worked with two other organisations to found the international Communist Organization for the Fourth International.

References

1931 births
2007 deaths
American Trotskyists
Politicians from Brooklyn
Brooklyn College alumni
Activists from New York City
Members of the International Socialists (United States)

Sy Landy


John Pounds (17 June 1766 – 1 January 1839) was a teacher and altruist born in Portsmouth, and the man most responsible for the creation of the concept of Ragged schools. After Pounds' death, Thomas Guthrie (often credited with the creation of Ragged Schools) wrote his Plea for Ragged Schools and proclaimed John Pounds as the originator of this idea.

Pounds was severely crippled in his mid-teens, from falling into a dry dock at Portsmouth Dockyard, where he was apprenticed as a shipwright. He could no longer work at the dockyard, and from then onward made his living as a shoemaker.

He would scour the streets of Portsmouth looking for children who were poor and homeless, taking them into his small workshop and teaching them basic reading, writing, and arithmetic skills. This small workshop was often host to as many as 40 children at any one time. John carried with him simple food items like baked potatoes to attract children.

Many years after his death, John Pounds has become a local hero in his birthplace of Portsmouth, winning a "Man of the Millennium" award in 1999 from a local newspaper, ahead of nationally more famous local heroes including Admiral Lord Nelson and Charles Dickens.

A unitarian chapel named in his memory stands in Old Portsmouth and his life was celebrated in a sacred cantata Greatheart: The Story of John Pounds, by the Rev. Carey Bonner. In 2005, the John Pounds Centre was opened in Queen Street, Portsmouth to encourage "a happier and healthier lifestyle, should that be through learning, physical or social activities." Until 1975 there was a girl's secondary modern in Portsea named after him: it is now a community centre.

Notes

Further reading
Henry Hawkes, Recollections of John Pounds, 1884, books.google.com
J. F. Fyfe, John Pounds, in: The Progressive English Reading Books: books.google.com
Roland Everett Jayne, The Story of John Pounds: Founder of Ragged Schools, Epworth Press, 1925.

External links

18th-century English educators
People from Portsmouth
1766 births
1839 deaths
19th-century English educators

John Pounds