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L_0163 | explosive eruptions | T_1165 | FIGURE 1.4 | image | textbook_images/explosive_eruptions_20761.png |
L_0163 | explosive eruptions | T_1166 | FIGURE 1.5 | image | textbook_images/explosive_eruptions_20762.png |
L_0166 | finding and mining ores | T_1175 | FIGURE 1.1 | image | textbook_images/finding_and_mining_ores_20769.png |
L_0166 | finding and mining ores | T_1176 | FIGURE 1.2 gold traveled down rivers and then settled in gravel deposits. Currently, California has active mines for gold and silver and for non-metal minerals such as sand and gravel, which are used for construction. | image | textbook_images/finding_and_mining_ores_20770.png |
L_0166 | finding and mining ores | T_1177 | FIGURE 1.3 Underground mine. | image | textbook_images/finding_and_mining_ores_20771.png |
L_0209 | intraplate activity | T_1334 | FIGURE 1.1 | image | textbook_images/intraplate_activity_20866.png |
L_0209 | intraplate activity | T_1334 | FIGURE 1.2 The Hawaiian-Emperor chain can be traced from Hawaii in the central Pacific north of the Equator into the Aleutian trench, where the oldest of the volcanoes is being subducted. It looks like a skewed "L". | image | textbook_images/intraplate_activity_20867.png |
L_0209 | intraplate activity | T_1335 | FIGURE 1.3 | image | textbook_images/intraplate_activity_20868.png |
L_0214 | landforms from erosion and deposition by gravity | T_1351 | FIGURE 1.1 | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20881.png |
L_0214 | landforms from erosion and deposition by gravity | T_1353 | FIGURE 1.2 | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20882.png |
L_0214 | landforms from erosion and deposition by gravity | T_1353 | FIGURE 1.3 | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20883.png |
L_0214 | landforms from erosion and deposition by gravity | T_1353 | FIGURE 1.4 Creep is the extremely gradual movement of soil downhill. Curves in tree trunks indicate creep because the base of the tree is moving downslope while the top is trying to grow straight up (Figure 1.5). Tilted telephone or power company poles are also signs of creep. | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20884.png |
L_0214 | landforms from erosion and deposition by gravity | T_1353 | FIGURE 1.5 | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20885.png |
L_0214 | landforms from erosion and deposition by gravity | T_1357 | FIGURE 1.6 A rock wall stabilizes a slope that has been cut away to make a road. | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20886.png |
L_0220 | locating earthquake epicenters | T_1380 | FIGURE 1.1 | image | textbook_images/locating_earthquake_epicenters_20906.png |
L_0234 | mesozoic plate tectonics | T_1426 | FIGURE 1.1 | image | textbook_images/mesozoic_plate_tectonics_20937.png |
L_0234 | mesozoic plate tectonics | T_1426 | FIGURE 1.2 | image | textbook_images/mesozoic_plate_tectonics_20938.png |
L_0241 | mineral formation | T_1442 | FIGURE 1.1 | image | textbook_images/mineral_formation_20946.png |
L_0241 | mineral formation | T_1444 | FIGURE 1.2 | image | textbook_images/mineral_formation_20947.png |
L_0241 | mineral formation | T_1444 | FIGURE 1.3 | image | textbook_images/mineral_formation_20948.png |
L_0241 | mineral formation | T_1445 | FIGURE 1.4 | image | textbook_images/mineral_formation_20949.png |
L_0241 | mineral formation | T_1445 | FIGURE 1.5 | image | textbook_images/mineral_formation_20950.png |
L_0241 | mineral formation | T_1446 | FIGURE 1.6 | image | textbook_images/mineral_formation_20951.png |
L_0242 | mineral groups | T_1448 | FIGURE 1.1 | image | textbook_images/mineral_groups_20952.png |
L_0242 | mineral groups | T_1448 | FIGURE 1.2 | image | textbook_images/mineral_groups_20953.png |
L_0242 | mineral groups | T_1449 | FIGURE 1.3 A gold nugget. | image | textbook_images/mineral_groups_20954.png |
L_0242 | mineral groups | T_1450 | FIGURE 1.4 | image | textbook_images/mineral_groups_20955.png |
L_0242 | mineral groups | T_1451 | FIGURE 1.5 | image | textbook_images/mineral_groups_20956.png |
L_0242 | mineral groups | T_1451 | FIGURE 1.6 | image | textbook_images/mineral_groups_20957.png |
L_0242 | mineral groups | T_1452 | FIGURE 1.7 | image | textbook_images/mineral_groups_20958.png |
L_0242 | mineral groups | T_1453 | FIGURE 1.8 Apatite. | image | textbook_images/mineral_groups_20959.png |
L_0242 | mineral groups | T_1454 | FIGURE 1.9 | image | textbook_images/mineral_groups_20960.png |
L_0242 | mineral groups | T_1455 | FIGURE 1.10 This mineral has shiny, gold, cubic crys- tals with striations, so it is pyrite. | image | textbook_images/mineral_groups_20961.png |
L_0243 | mineral identification | T_1458 | FIGURE 1.1 Purple quartz, known as amethyst, and clear quartz are the same mineral despite the different colors. | image | textbook_images/mineral_identification_20962.png |
L_0243 | mineral identification | T_1460 | FIGURE 1.2 | image | textbook_images/mineral_identification_20963.png |
L_0243 | mineral identification | T_1463 | FIGURE 1.3 Halite has cubic cleavage. | image | textbook_images/mineral_identification_20964.png |
L_0243 | mineral identification | T_1463 | FIGURE 1.4 | image | textbook_images/mineral_identification_20965.png |
L_0243 | mineral identification | T_1463 | FIGURE 1.5 Fluorite has octahedral cleavage. | image | textbook_images/mineral_identification_20966.png |
L_0243 | mineral identification | T_1464 | FIGURE 1.6 | image | textbook_images/mineral_identification_20967.png |
L_0244 | minerals | T_1466 | FIGURE 1.1 | image | textbook_images/minerals_20968.png |
L_0244 | minerals | T_1469 | FIGURE 1.2 | image | textbook_images/minerals_20969.png |
L_0247 | mountain building | T_1477 | FIGURE 1.1 | image | textbook_images/mountain_building_20977.png |
L_0247 | mountain building | T_1478 | FIGURE 1.2 | image | textbook_images/mountain_building_20978.png |
L_0247 | mountain building | T_1479 | FIGURE 1.3 | image | textbook_images/mountain_building_20979.png |
L_0267 | plate tectonics through earth history | T_1551 | FIGURE 1.1 The Appalachian Mountains in New Hampshire. | image | textbook_images/plate_tectonics_through_earth_history_21027.png |
L_0267 | plate tectonics through earth history | T_1551 | FIGURE 1.2 | image | textbook_images/plate_tectonics_through_earth_history_21028.png |
L_0272 | precipitation | T_1565 | FIGURE 1.1 | image | textbook_images/precipitation_21038.png |
L_0272 | precipitation | T_1565 | FIGURE 1.2 | image | textbook_images/precipitation_21039.png |
L_0272 | precipitation | T_1565 | FIGURE 1.3 | image | textbook_images/precipitation_21040.png |
L_0273 | predicting earthquakes | T_1567 | FIGURE 1.1 | image | textbook_images/predicting_earthquakes_21041.png |
L_0273 | predicting earthquakes | T_1568 | FIGURE 1.2 | image | textbook_images/predicting_earthquakes_21042.png |
L_0274 | predicting volcanic eruptions | T_1574 | FIGURE 1.1 | image | textbook_images/predicting_volcanic_eruptions_21043.png |
L_0274 | predicting volcanic eruptions | T_1575 | FIGURE 1.2 An earth observation satellite. | image | textbook_images/predicting_volcanic_eruptions_21044.png |
L_0307 | soil characteristics | T_1689 | FIGURE 1.1 Peat is so rich in organic material, it can be burned for energy. | image | textbook_images/soil_characteristics_21112.png |
L_0307 | soil characteristics | T_1689 | FIGURE 1.2 | image | textbook_images/soil_characteristics_21113.png |
L_0307 | soil characteristics | T_1690 | FIGURE 1.3 | image | textbook_images/soil_characteristics_21114.png |
L_0307 | soil characteristics | T_1691 | FIGURE 1.4 Earthworms and insects are important residents of soils. Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186344 | image | textbook_images/soil_characteristics_21115.png |
L_0308 | soil erosion | T_1693 | FIGURE 1.1 | image | textbook_images/soil_erosion_21116.png |
L_0308 | soil erosion | T_1694 | FIGURE 1.2 | image | textbook_images/soil_erosion_21117.png |
L_0308 | soil erosion | T_1695 | FIGURE 1.3 | image | textbook_images/soil_erosion_21118.png |
L_0308 | soil erosion | T_1697 | FIGURE 1.4 | image | textbook_images/soil_erosion_21119.png |
L_0308 | soil erosion | T_1697 | FIGURE 1.5 | image | textbook_images/soil_erosion_21120.png |
L_0308 | soil erosion | T_1697 | FIGURE 1.6 Urban areas and parking lots result in less water entering the ground. Water runs off the parking lot onto nearby lands and speeds up erosion in those areas. | image | textbook_images/soil_erosion_21121.png |
L_0308 | soil erosion | T_1697 | FIGURE 1.7 | image | textbook_images/soil_erosion_21122.png |
L_0309 | soil formation | T_1699 | FIGURE 1.1 | image | textbook_images/soil_formation_21123.png |
L_0310 | soil horizons and profiles | T_1704 | FIGURE 1.1 | image | textbook_images/soil_horizons_and_profiles_21124.png |
L_0310 | soil horizons and profiles | T_1706 | FIGURE 1.2 | image | textbook_images/soil_horizons_and_profiles_21125.png |
L_0322 | surface ocean currents | T_1748 | FIGURE 1.1 | image | textbook_images/surface_ocean_currents_21149.png |
L_0322 | surface ocean currents | T_1748 | FIGURE 1.2 The ocean gyres. Why do the Northern Hemisphere gyres rotate clockwise and the Southern Hemisphere gyres rotate counterclockwise? | image | textbook_images/surface_ocean_currents_21150.png |
L_0322 | surface ocean currents | T_1749 | FIGURE 1.3 | image | textbook_images/surface_ocean_currents_21151.png |
L_0322 | surface ocean currents | DD_0095 | The diagram below shows the types of Ocean current. An ocean current is a continuous, directed movement of seawater generated by forces acting upon this mean flow, such as breaking waves, wind, the Coriolis effect, cabbeling, temperature and salinity differences, while tides are caused by the gravitational pull of the Sun and Moon. Depth contours, shoreline configurations, and interactions with other currents influence a current's direction and strength. Ocean currents flow for great distances, and together, create the global conveyor belt which plays a dominant role in determining the climate of many of the EarthÕs regions. More specifically, ocean currents influence the temperature of the regions through which they travel. For example, warm currents traveling along more temperate coasts increase the temperature of the area by warming the sea breezes that blow over them. Perhaps the most striking example is the Gulf Stream, which makes northwest Europe much more temperate than any other region at the same latitude. Another example is Lima, Peru where the climate is cooler (sub-tropical) than the tropical latitudes in which the area is located, due to the effect of the Humboldt Current. | image | teaching_images/ocean_currents_7109.png |
L_0322 | surface ocean currents | DD_0096 | This diagram shows the way ocean and waves move. Most ocean waves are caused by winds. A wave is the transfer of energy through matter. A wave that travels across miles of ocean is traveling energy, not water. Ocean waves transfer energy from wind through water. The energy of a wave may travel for thousands of miles. The water itself moves very little. Ocean water also moves from the deep sea to the ocean surface. Places where this happens are called areas of upwelling. The marine life and the climate can be affected as the cold water makes its way up from the deep. | image | teaching_images/ocean_currents_7107.png |
L_0330 | thunderstorms | T_1772 | FIGURE 1.1 | image | textbook_images/thunderstorms_21157.png |
L_0330 | thunderstorms | T_1773 | FIGURE 1.2 giant. Eventually, the drops become large enough to fall to the ground. At this time, the thunderstorm is mature, and it produces gusty winds, lightning, heavy precipitation, and hail (Figure 1.2). | image | textbook_images/thunderstorms_21158.png |
L_0330 | thunderstorms | T_1776 | FIGURE 1.3 | image | textbook_images/thunderstorms_21159.png |
L_0330 | thunderstorms | T_1777 | FIGURE 1.4 | image | textbook_images/thunderstorms_21160.png |
L_0330 | thunderstorms | T_1778 | FIGURE 1.5 | image | textbook_images/thunderstorms_21161.png |
L_0333 | transform plate boundaries | T_1788 | FIGURE 1.1 Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186149 | image | textbook_images/transform_plate_boundaries_21171.png |
L_0340 | types of soils | T_1814 | FIGURE 1.1 | image | textbook_images/types_of_soils_21189.png |
L_0340 | types of soils | T_1815 | FIGURE 1.2 | image | textbook_images/types_of_soils_21190.png |
L_0340 | types of soils | T_1816 | FIGURE 1.3 | image | textbook_images/types_of_soils_21191.png |
L_0340 | types of soils | T_1817 | FIGURE 1.4 Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186352 | image | textbook_images/types_of_soils_21192.png |
L_0341 | types of volcanoes | T_1820 | FIGURE 1.1 | image | textbook_images/types_of_volcanoes_21193.png |
L_0341 | types of volcanoes | T_1820 | FIGURE 1.2 | image | textbook_images/types_of_volcanoes_21194.png |
L_0341 | types of volcanoes | T_1821 | FIGURE 1.3 | image | textbook_images/types_of_volcanoes_21195.png |
L_0341 | types of volcanoes | T_1821 | FIGURE 1.4 | image | textbook_images/types_of_volcanoes_21196.png |
L_0341 | types of volcanoes | T_1823 | FIGURE 1.5 | image | textbook_images/types_of_volcanoes_21197.png |
L_0346 | volcanic landforms | T_1849 | FIGURE 1.1 | image | textbook_images/volcanic_landforms_21210.png |
L_0346 | volcanic landforms | T_1849 | FIGURE 1.2 | image | textbook_images/volcanic_landforms_21211.png |
L_0346 | volcanic landforms | T_1849 | FIGURE 1.3 | image | textbook_images/volcanic_landforms_21212.png |
L_0346 | volcanic landforms | T_1850 | FIGURE 1.4 | image | textbook_images/volcanic_landforms_21213.png |
L_0346 | volcanic landforms | T_1851 | FIGURE 1.5 | image | textbook_images/volcanic_landforms_21214.png |
L_0346 | volcanic landforms | T_1851 | FIGURE 1.6 | image | textbook_images/volcanic_landforms_21215.png |
L_0346 | volcanic landforms | T_1852 | FIGURE 1.7 Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186309 | image | textbook_images/volcanic_landforms_21216.png |
L_0347 | volcano characteristics | T_1854 | FIGURE 1.1 | image | textbook_images/volcano_characteristics_21217.png |
L_0347 | volcano characteristics | T_1856 | FIGURE 1.2 Volcanoes can be active, dormant, or extinct. | image | textbook_images/volcano_characteristics_21218.png |
L_0348 | volcanoes at hotspots | T_1858 | FIGURE 1.1 | image | textbook_images/volcanoes_at_hotspots_21219.png |
L_0348 | volcanoes at hotspots | T_1858 | FIGURE 1.2 The Society Islands are the exposed peaks of a great chain of volcanoes that lie on the Pacific Plate. The youngest island sits directly above the Society hotspot (Figure 1.2). | image | textbook_images/volcanoes_at_hotspots_21220.png |
L_0349 | volcanoes at plate boundaries | T_1866 | FIGURE 1.1 | image | textbook_images/volcanoes_at_plate_boundaries_21221.png |
L_0369 | sponges and cnidarians | T_1983 | FIGURE 12.1 Sponge | image | textbook_images/sponges_and_cnidarians_21305.png |
Subsets and Splits