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L_0211 | introduction to groundwater | T_1341 | FIGURE 1.1 | image | textbook_images/introduction_to_groundwater_20870.png |
L_0212 | intrusive and extrusive igneous rocks | T_1343 | FIGURE 1.1 | image | textbook_images/intrusive_and_extrusive_igneous_rocks_20871.png |
L_0212 | intrusive and extrusive igneous rocks | T_1343 | FIGURE 1.2 | image | textbook_images/intrusive_and_extrusive_igneous_rocks_20872.png |
L_0212 | intrusive and extrusive igneous rocks | T_1344 | FIGURE 1.3 | image | textbook_images/intrusive_and_extrusive_igneous_rocks_20873.png |
L_0212 | intrusive and extrusive igneous rocks | T_1344 | FIGURE 1.4 case, the magma cooled enough to form some crystals before erupting. Once erupted, the rest of the lava cooled rapidly. This is called porphyritic texture. | image | textbook_images/intrusive_and_extrusive_igneous_rocks_20874.png |
L_0212 | intrusive and extrusive igneous rocks | T_1344 | FIGURE 1.5 | image | textbook_images/intrusive_and_extrusive_igneous_rocks_20875.png |
L_0213 | jupiter | T_1346 | FIGURE 1.1 | image | textbook_images/jupiter_20876.png |
L_0213 | jupiter | T_1346 | FIGURE 1.2 Jupiters structure. | image | textbook_images/jupiter_20877.png |
L_0213 | jupiter | T_1347 | FIGURE 1.3 | image | textbook_images/jupiter_20878.png |
L_0213 | jupiter | T_1348 | FIGURE 1.4 | image | textbook_images/jupiter_20879.png |
L_0215 | landforms from glacial erosion and deposition | T_1360 | FIGURE 1.1 | image | textbook_images/landforms_from_glacial_erosion_and_deposition_20887.png |
L_0215 | landforms from glacial erosion and deposition | T_1360 | FIGURE 1.2 | image | textbook_images/landforms_from_glacial_erosion_and_deposition_20888.png |
L_0215 | landforms from glacial erosion and deposition | T_1360 | FIGURE 1.3 | image | textbook_images/landforms_from_glacial_erosion_and_deposition_20889.png |
L_0215 | landforms from glacial erosion and deposition | T_1360 | FIGURE 1.4 | image | textbook_images/landforms_from_glacial_erosion_and_deposition_20890.png |
L_0215 | landforms from glacial erosion and deposition | T_1360 | FIGURE 1.5 | image | textbook_images/landforms_from_glacial_erosion_and_deposition_20891.png |
L_0215 | landforms from glacial erosion and deposition | T_1362 | FIGURE 1.6 A large boulder dropped by a glacier is a glacial erratic. | image | textbook_images/landforms_from_glacial_erosion_and_deposition_20892.png |
L_0215 | landforms from glacial erosion and deposition | T_1363 | FIGURE 1.7 The long, dark lines on a glacier in Alaska are medial and lateral moraines. | image | textbook_images/landforms_from_glacial_erosion_and_deposition_20893.png |
L_0215 | landforms from glacial erosion and deposition | T_1364 | FIGURE 1.8 | image | textbook_images/landforms_from_glacial_erosion_and_deposition_20894.png |
L_0216 | landforms from groundwater erosion and deposition | T_1367 | FIGURE 1.1 When water sinks into the ground, it be- comes groundwater. | image | textbook_images/landforms_from_groundwater_erosion_and_deposition_20895.png |
L_0216 | landforms from groundwater erosion and deposition | T_1367 | FIGURE 1.2 | image | textbook_images/landforms_from_groundwater_erosion_and_deposition_20896.png |
L_0216 | landforms from groundwater erosion and deposition | T_1368 | FIGURE 1.3 | image | textbook_images/landforms_from_groundwater_erosion_and_deposition_20897.png |
L_0216 | landforms from groundwater erosion and deposition | T_1368 | FIGURE 1.4 | image | textbook_images/landforms_from_groundwater_erosion_and_deposition_20898.png |
L_0217 | lithification of sedimentary rocks | T_1369 | FIGURE 1.1 | image | textbook_images/lithification_of_sedimentary_rocks_20899.png |
L_0221 | location and direction | T_1381 | FIGURE 1.1 | image | textbook_images/location_and_direction_20907.png |
L_0221 | location and direction | T_1386 | FIGURE 1.2 | image | textbook_images/location_and_direction_20908.png |
L_0222 | long term climate change | T_1388 | FIGURE 1.1 | image | textbook_images/long_term_climate_change_20909.png |
L_0222 | long term climate change | T_1390 | FIGURE 1.2 | image | textbook_images/long_term_climate_change_20910.png |
L_0222 | long term climate change | T_1391 | FIGURE 1.3 | image | textbook_images/long_term_climate_change_20911.png |
L_0224 | magnetic evidence for seafloor spreading | T_1393 | FIGURE 1.1 Magnetic polarity is normal at the ridge crest but reversed in symmetrical patterns away from the ridge center. This normal and reversed pattern continues across the seafloor. | image | textbook_images/magnetic_evidence_for_seafloor_spreading_20912.png |
L_0224 | magnetic evidence for seafloor spreading | T_1394 | FIGURE 1.2 | image | textbook_images/magnetic_evidence_for_seafloor_spreading_20913.png |
L_0225 | magnetic polarity evidence for continental drift | T_1395 | FIGURE 1.1 Magnetite crystals. | image | textbook_images/magnetic_polarity_evidence_for_continental_drift_20914.png |
L_0225 | magnetic polarity evidence for continental drift | T_1396 | FIGURE 1.2 Earths current north magnetic pole is in northern Canada. | image | textbook_images/magnetic_polarity_evidence_for_continental_drift_20915.png |
L_0225 | magnetic polarity evidence for continental drift | T_1396 | FIGURE 1.3 | image | textbook_images/magnetic_polarity_evidence_for_continental_drift_20916.png |
L_0225 | magnetic polarity evidence for continental drift | T_1398 | FIGURE 1.4 Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186134 | image | textbook_images/magnetic_polarity_evidence_for_continental_drift_20917.png |
L_0226 | maps | T_1399 | FIGURE 1.1 | image | textbook_images/maps_20918.png |
L_0226 | maps | T_1400 | FIGURE 1.2 | image | textbook_images/maps_20919.png |
L_0226 | maps | T_1400 | FIGURE 1.3 | image | textbook_images/maps_20920.png |
L_0227 | mars | T_1402 | FIGURE 1.1 | image | textbook_images/mars_20921.png |
L_0227 | mars | T_1405 | FIGURE 1.2 | image | textbook_images/mars_20922.png |
L_0227 | mars | T_1405 | FIGURE 1.3 | image | textbook_images/mars_20923.png |
L_0227 | mars | T_1405 | FIGURE 1.4 The north polar ice cap on Mars. | image | textbook_images/mars_20924.png |
L_0227 | mars | T_1406 | FIGURE 1.5 The Mars Science Laboratory was launched on November 26, 2011 and will search for any evidence that the Red Planet was once capable of supporting life. Curiosity is a car-sized rover that will scour the red planet for clues after it lands in August 2012. | image | textbook_images/mars_20925.png |
L_0229 | measuring earthquake magnitude | T_1409 | FIGURE 1.1 | image | textbook_images/measuring_earthquake_magnitude_20926.png |
L_0230 | mechanical weathering | T_1411 | FIGURE 1.1 Ice wedging. | image | textbook_images/mechanical_weathering_20927.png |
L_0230 | mechanical weathering | T_1412 | FIGURE 1.2 Rocks on a beach are worn down by abrasion as passing waves cause them to strike each other. | image | textbook_images/mechanical_weathering_20928.png |
L_0230 | mechanical weathering | T_1414 | FIGURE 1.3 | image | textbook_images/mechanical_weathering_20929.png |
L_0231 | mercury | T_1415 | FIGURE 1.1 | image | textbook_images/mercury_20930.png |
L_0231 | mercury | T_1417 | FIGURE 1.2 | image | textbook_images/mercury_20931.png |
L_0231 | mercury | T_1418 | FIGURE 1.3 Mercury contains a thin crust, a mantle, and a large, liquid core that is rich in iron. Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186936 | image | textbook_images/mercury_20932.png |
L_0232 | mercury pollution | T_1420 | FIGURE 1.1 | image | textbook_images/mercury_pollution_20933.png |
L_0232 | mercury pollution | T_1421 | FIGURE 1.2 Methyl mercury bioaccumulates up the food chain. | image | textbook_images/mercury_pollution_20934.png |
L_0233 | mesosphere | T_1423 | FIGURE 1.1 Although the mesosphere has extremely low pressure, it occasionally has clouds. The clouds in the photo are mesopheric clouds called noctilucent clouds. | image | textbook_images/mesosphere_20936.png |
L_0237 | metamorphic rocks | T_1432 | FIGURE 1.1 | image | textbook_images/metamorphic_rocks_20939.png |
L_0238 | meteors | T_1435 | FIGURE 1.1 A meteor streaks across the sky. | image | textbook_images/meteors_20940.png |
L_0238 | meteors | T_1435 | FIGURE 1.2 A lunar meteorite originates on the Moon and strikes Earth. Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186958 | image | textbook_images/meteors_20941.png |
L_0240 | milky way | T_1439 | FIGURE 1.1 | image | textbook_images/milky_way_20944.png |
L_0240 | milky way | T_1439 | FIGURE 1.2 | image | textbook_images/milky_way_20945.png |
L_0246 | moon | T_1473 | FIGURE 1.1 | image | textbook_images/moon_20973.png |
L_0246 | moon | T_1474 | FIGURE 1.2 | image | textbook_images/moon_20974.png |
L_0246 | moon | T_1475 | FIGURE 1.3 | image | textbook_images/moon_20975.png |
L_0246 | moon | T_1475 | FIGURE 1.4 The Moons internal structure shows a small metallic core (yellow), a primi- tive mantle (orange), a depleted mantle (blue), and a crust (gray). The crust is composed of igneous rock rich in the elements oxygen, silicon, magnesium, and aluminum. The crust is about 60 km thick on the near side of the Moon and about 100 km thick on the far side. | image | textbook_images/moon_20976.png |
L_0248 | natural gas power | T_1481 | FIGURE 1.1 | image | textbook_images/natural_gas_power_20980.png |
L_0248 | natural gas power | T_1483 | FIGURE 1.2 A natural gas drill rig in Texas. | image | textbook_images/natural_gas_power_20981.png |
L_0249 | natural resource conservation | T_1484 | FIGURE 1.1 Recycling can help conserve natural re- sources. | image | textbook_images/natural_resource_conservation_20982.png |
L_0250 | neptune | T_1485 | FIGURE 1.1 | image | textbook_images/neptune_20983.png |
L_0250 | neptune | T_1486 | FIGURE 1.2 | image | textbook_images/neptune_20984.png |
L_0250 | neptune | T_1487 | FIGURE 1.3 Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186951 | image | textbook_images/neptune_20985.png |
L_0251 | nitrogen cycle in ecosystems | T_1489 | FIGURE 1.1 | image | textbook_images/nitrogen_cycle_in_ecosystems_20986.png |
L_0251 | nitrogen cycle in ecosystems | T_1489 | FIGURE 1.2 The nitrogen cycle. Nitrogen-fixing bacteria either live free or in a symbiotic relationship with leguminous plants (peas, beans, peanuts). The symbiotic bacteria use carbohydrates from the plant to produce ammonia that is useful to the plant. Plants use this fixed nitrogen to build amino acids, nucleic acids (DNA, RNA), and chlorophyll. When these legumes die, the fixed nitrogen they contain fertilizes the soil. | image | textbook_images/nitrogen_cycle_in_ecosystems_20987.png |
L_0252 | non renewable energy resources | T_1492 | FIGURE 1.1 | image | textbook_images/non_renewable_energy_resources_20988.png |
L_0252 | non renewable energy resources | T_1495 | FIGURE 1.2 | image | textbook_images/non_renewable_energy_resources_20989.png |
L_0253 | nuclear power | T_1497 | FIGURE 1.1 When struck by a tiny particle, Uranium-235 breaks apart and releases energy. | image | textbook_images/nuclear_power_20990.png |
L_0253 | nuclear power | T_1497 | FIGURE 1.2 Nuclear power plants like this one provide France with almost 80% of its electricity. | image | textbook_images/nuclear_power_20991.png |
L_0253 | nuclear power | T_1498 | FIGURE 1.3 Uranium mine in Kakadu National Park, Australia. | image | textbook_images/nuclear_power_20992.png |
L_0253 | nuclear power | T_1498 | FIGURE 1.4 | image | textbook_images/nuclear_power_20993.png |
L_0255 | obtaining energy resources | T_1503 | FIGURE 1.1 | image | textbook_images/obtaining_energy_resources_20996.png |
L_0255 | obtaining energy resources | T_1504 | FIGURE 1.2 Less energy is being wasted. Non-renewable resources will last longer. The cost is kept lower. | image | textbook_images/obtaining_energy_resources_20997.png |
L_0256 | ocean ecosystems | T_1505 | FIGURE 1.1 | image | textbook_images/ocean_ecosystems_20998.png |
L_0256 | ocean ecosystems | T_1507 | FIGURE 1.2 | image | textbook_images/ocean_ecosystems_20999.png |
L_0256 | ocean ecosystems | T_1507 | FIGURE 1.3 | image | textbook_images/ocean_ecosystems_21000.png |
L_0256 | ocean ecosystems | T_1507 | FIGURE 1.4 | image | textbook_images/ocean_ecosystems_21001.png |
L_0256 | ocean ecosystems | T_1508 | FIGURE 1.5 | image | textbook_images/ocean_ecosystems_21002.png |
L_0257 | ocean garbage patch | T_1510 | FIGURE 1.1 Trash has washed up on this beach. | image | textbook_images/ocean_garbage_patch_21003.png |
L_0257 | ocean garbage patch | T_1513 | FIGURE 1.2 | image | textbook_images/ocean_garbage_patch_21004.png |
L_0257 | ocean garbage patch | T_1513 | FIGURE 1.3 Plastic bags in the ocean can be mis- taken for food by an unsuspecting marine predator. | image | textbook_images/ocean_garbage_patch_21005.png |
L_0258 | ocean zones | T_1516 | FIGURE 1.1 Vertical and horizontal ocean zones. | image | textbook_images/ocean_zones_21006.png |
L_0259 | oil spills | T_1520 | FIGURE 1.1 | image | textbook_images/oil_spills_21007.png |
L_0259 | oil spills | T_1522 | FIGURE 1.2 | image | textbook_images/oil_spills_21008.png |
L_0259 | oil spills | T_1522 | FIGURE 1.3 Burning the oil can reduce the amount in the water. | image | textbook_images/oil_spills_21009.png |
L_0259 | oil spills | T_1522 | FIGURE 1.4 A containment boom holds back oil, but it is only effective in calm water. | image | textbook_images/oil_spills_21010.png |
L_0259 | oil spills | T_1524 | FIGURE 1.5 The toll on wildlife is felt throughout the Gulf. Plankton, which form the base of the food chain, are killed by the oil, leaving other organisms without food. Islands and marshlands around the Gulf have many species that are already at risk, including four endangered species of sea turtles. With such low numbers, rebuilding their populations after the spill will be difficult. | image | textbook_images/oil_spills_21011.png |
L_0260 | overpopulation and over consumption | T_1528 | FIGURE 1.1 Pesticides are hazardous in large quanti- ties and some are toxic in small quantities. | image | textbook_images/overpopulation_and_over_consumption_21012.png |
L_0260 | overpopulation and over consumption | T_1530 | FIGURE 1.2 | image | textbook_images/overpopulation_and_over_consumption_21013.png |
L_0261 | ozone depletion | T_1532 | FIGURE 1.1 | image | textbook_images/ozone_depletion_21015.png |
L_0261 | ozone depletion | T_1532 | FIGURE 1.2 | image | textbook_images/ozone_depletion_21016.png |
L_0261 | ozone depletion | T_1533 | FIGURE 1.3 | image | textbook_images/ozone_depletion_21017.png |
L_0262 | paleozoic and mesozoic seas | T_1536 | FIGURE 1.1 | image | textbook_images/paleozoic_and_mesozoic_seas_21018.png |
L_0263 | paleozoic plate tectonics | T_1540 | FIGURE 1.1 | image | textbook_images/paleozoic_plate_tectonics_21019.png |
L_0264 | petroleum power | T_1544 | FIGURE 1.1 | image | textbook_images/petroleum_power_21021.png |
L_0264 | petroleum power | T_1545 | FIGURE 1.2 | image | textbook_images/petroleum_power_21022.png |
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