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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 |
L_0264 | petroleum power | T_1546 | FIGURE 1.3 | image | textbook_images/petroleum_power_21023.png |
L_0264 | petroleum power | T_1546 | FIGURE 1.4 | image | textbook_images/petroleum_power_21024.png |
L_0265 | planet orbits in the solar system | T_1547 | FIGURE 1.1 | image | textbook_images/planet_orbits_in_the_solar_system_21026.png |
L_0268 | ponds and lakes | T_1553 | FIGURE 1.1 | image | textbook_images/ponds_and_lakes_21029.png |
L_0268 | ponds and lakes | T_1553 | FIGURE 1.2 | image | textbook_images/ponds_and_lakes_21030.png |
L_0268 | ponds and lakes | T_1553 | FIGURE 1.3 The Badwater Basin in Death Valley con- tains water in wet years. The lake basin is a remnant from when the region was much wetter just after the Ice Ages. | image | textbook_images/ponds_and_lakes_21031.png |
L_0269 | population size | T_1556 | FIGURE 1.1 In a desert such as this, what is the limiting factor on plant populations? What would make the population increase? What would make the population de- crease? | image | textbook_images/population_size_21032.png |
L_0269 | population size | T_1556 | FIGURE 1.2 | image | textbook_images/population_size_21033.png |
L_0270 | precambrian continents | T_1558 | FIGURE 1.1 | image | textbook_images/precambrian_continents_21034.png |
L_0270 | precambrian continents | T_1559 | FIGURE 1.2 | image | textbook_images/precambrian_continents_21035.png |
L_0270 | precambrian continents | T_1560 | FIGURE 1.3 The Precambrian craton is exposed in the Grand Canyon where the Colorado River has cut through the younger sedimentary rocks. | image | textbook_images/precambrian_continents_21036.png |
L_0271 | precambrian plate tectonics | T_1562 | FIGURE 1.1 Rodinia as it came together about 1.1 billion years ago. | image | textbook_images/precambrian_plate_tectonics_21037.png |
L_0277 | preventing hazardous waste problems | T_1581 | FIGURE 1.1 Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186861 | image | textbook_images/preventing_hazardous_waste_problems_21048.png |
L_0278 | principle of horizontality | T_1583 | FIGURE 1.1 | image | textbook_images/principle_of_horizontality_21049.png |
L_0279 | principle of uniformitarianism | T_1585 | FIGURE 1.1 | image | textbook_images/principle_of_uniformitarianism_21050.png |
L_0279 | principle of uniformitarianism | T_1586 | FIGURE 1.2 The Mesquite sand dune in Death Valley National Park, California. This doesnt look exactly like the outcrop of Navajo sandstone, but if you could cut a cross-section into the face of the dune it would look very similar. | image | textbook_images/principle_of_uniformitarianism_21051.png |
L_0280 | principles of relative dating | T_1588 | FIGURE 1.1 | image | textbook_images/principles_of_relative_dating_21052.png |
L_0280 | principles of relative dating | T_1589 | FIGURE 1.2 | image | textbook_images/principles_of_relative_dating_21053.png |
L_0281 | processes of the water cycle | T_1593 | FIGURE 1.1 Because it is a cycle, the water cycle has no beginning and no end. | image | textbook_images/processes_of_the_water_cycle_21055.png |
L_0281 | processes of the water cycle | T_1596 | FIGURE 1.2 | image | textbook_images/processes_of_the_water_cycle_21056.png |
L_0281 | processes of the water cycle | T_1599 | FIGURE 1.3 | image | textbook_images/processes_of_the_water_cycle_21057.png |
L_0281 | processes of the water cycle | T_1599 | FIGURE 1.4 | image | textbook_images/processes_of_the_water_cycle_21058.png |
L_0282 | protecting water from pollution | T_1601 | FIGURE 1.1 | image | textbook_images/protecting_water_from_pollution_21059.png |
L_0283 | radioactive decay as a measure of age | T_1605 | FIGURE 1.1 A parent emits an alpha particle to create a daughter. | image | textbook_images/radioactive_decay_as_a_measure_of_age_21060.png |
L_0283 | radioactive decay as a measure of age | T_1606 | FIGURE 1.2 | image | textbook_images/radioactive_decay_as_a_measure_of_age_21061.png |
L_0284 | radiometric dating | T_1608 | FIGURE 1.1 | image | textbook_images/radiometric_dating_21062.png |
L_0284 | radiometric dating | T_1610 | FIGURE 1.2 Zircon crystal. | image | textbook_images/radiometric_dating_21063.png |
L_0285 | reducing air pollution | T_1614 | FIGURE 1.1 | image | textbook_images/reducing_air_pollution_21064.png |
L_0285 | reducing air pollution | T_1615 | FIGURE 1.2 | image | textbook_images/reducing_air_pollution_21065.png |
L_0285 | reducing air pollution | T_1615 | FIGURE 1.3 | image | textbook_images/reducing_air_pollution_21066.png |
L_0286 | reducing ozone destruction | T_1619 | FIGURE 1.1 | image | textbook_images/reducing_ozone_destruction_21067.png |
L_0287 | revolutions of earth | T_1621 | FIGURE 1.1 According to Ptolemy, a planet moves on a small circle (epicycle) that in turn moves on a larger circle (deferent) around Earth. | image | textbook_images/revolutions_of_earth_21068.png |
L_0287 | revolutions of earth | T_1622 | FIGURE 1.2 | image | textbook_images/revolutions_of_earth_21069.png |
L_0287 | revolutions of earth | T_1622 | FIGURE 1.3 | image | textbook_images/revolutions_of_earth_21070.png |
L_0287 | revolutions of earth | T_1623 | FIGURE 1.4 | image | textbook_images/revolutions_of_earth_21071.png |
L_0288 | rocks | T_1624 | FIGURE 1.1 | image | textbook_images/rocks_21072.png |
L_0288 | rocks | T_1624 | FIGURE 1.2 | image | textbook_images/rocks_21073.png |
L_0288 | rocks | T_1624 | FIGURE 1.3 Rock samples. Sample Sample 1 Minerals plagioclase, quartz, hornblende, pyrox- ene plagioclase, hornblende, pyroxene Texture Crystals, visible to naked eye Formation Magma cooled slowly Rock type Diorite | image | textbook_images/rocks_21074.png |
L_0289 | rocks and processes of the rock cycle | T_1626 | FIGURE 1.1 | image | textbook_images/rocks_and_processes_of_the_rock_cycle_21075.png |
L_0291 | rotation of earth | T_1635 | FIGURE 1.1 Foucaults Pendulum is at the Pantheon in Paris, France. | image | textbook_images/rotation_of_earth_21079.png |
L_0292 | safety of water | T_1640 | FIGURE 1.1 Dracunculiasis, commonly known as Guinea Worm, is contracted when a per- son drinks the guinea worm larvae. | image | textbook_images/safety_of_water_21080.png |
L_0293 | satellites shuttles and space stations | T_1641 | FIGURE 1.1 The space shuttle Atlantis being launched into orbit by a rocket on Cape Canaveral, Florida. | image | textbook_images/satellites_shuttles_and_space_stations_21081.png |
L_0293 | satellites shuttles and space stations | T_1644 | FIGURE 1.2 | image | textbook_images/satellites_shuttles_and_space_stations_21082.png |
L_0293 | satellites shuttles and space stations | T_1644 | FIGURE 1.3 | image | textbook_images/satellites_shuttles_and_space_stations_21083.png |
L_0293 | satellites shuttles and space stations | T_1644 | FIGURE 1.4 | image | textbook_images/satellites_shuttles_and_space_stations_21084.png |
L_0293 | satellites shuttles and space stations | T_1644 | FIGURE 1.5 The space shuttle orbiter Atlantis touches down at the Kennedy Space Center in Florida. | image | textbook_images/satellites_shuttles_and_space_stations_21085.png |
L_0294 | saturn | T_1645 | FIGURE 1.1 | image | textbook_images/saturn_21086.png |
L_0294 | saturn | T_1647 | FIGURE 1.2 | image | textbook_images/saturn_21087.png |
L_0294 | saturn | T_1647 | FIGURE 1.3 primitive life may exist on Titan, the extreme cold and lack of carbon dioxide make it unlikely (Figure 1.4). | image | textbook_images/saturn_21088.png |
L_0294 | saturn | T_1647 | FIGURE 1.4 | image | textbook_images/saturn_21089.png |
L_0300 | seafloor spreading hypothesis | T_1667 | FIGURE 1.1 Magma at the mid-ocean ridge creates new seafloor. Since new oceanic crust is created at the mid-ocean ridges, either Earth is getting bigger (which it is not) or oceanic crust must be destroyed somewhere. Since the oldest oceanic crust was found at the edges of the trenches, Hess hypothesized that the seafloor subducts into Earths interior at the trenches to be recycled in the mantle. | image | textbook_images/seafloor_spreading_hypothesis_21094.png |
L_0301 | seasons | T_1670 | FIGURE 1.1 The Earths tilt on its axis leads to one hemisphere facing the Sun more than the other hemisphere and gives rise to sea- sons. | image | textbook_images/seasons_21095.png |
L_0301 | seasons | T_1673 | FIGURE 1.2 | image | textbook_images/seasons_21096.png |
L_0302 | seawater chemistry | T_1675 | FIGURE 1.1 | image | textbook_images/seawater_chemistry_21099.png |
L_0302 | seawater chemistry | T_1675 | FIGURE 1.2 | image | textbook_images/seawater_chemistry_21100.png |
L_0303 | sedimentary rock classification | T_1677 | FIGURE 1.1 | image | textbook_images/sedimentary_rock_classification_21101.png |
L_0303 | sedimentary rock classification | T_1677 | FIGURE 1.2 Fossils in a biochemical rock, limestone, in the Carmel Formation in Utah. Picture Rock Name Conglomerate Type of Sedimentary Rock Clastic (fragments of non-organic sediments) Picture Rock Name Rock Gypsum Type of Sedimentary Rock Chemical precipitate | image | textbook_images/sedimentary_rock_classification_21102.png |
L_0304 | sedimentary rocks | T_1678 | FIGURE 1.1 | image | textbook_images/sedimentary_rocks_21103.png |
L_0304 | sedimentary rocks | T_1678 | FIGURE 1.2 A river dumps sediments along its bed and on its banks. | image | textbook_images/sedimentary_rocks_21104.png |
L_0305 | seismic waves | T_1679 | FIGURE 1.1 The crest, trough, and amplitude are illus- trated in this diagram. | image | textbook_images/seismic_waves_21105.png |
L_0305 | seismic waves | T_1681 | FIGURE 1.2 unsqueezing Earth materials as they travel. This produces a change in volume for the material. P-waves bend slightly when they travel from one layer into another. Seismic waves move faster through denser or more rigid material. As P-waves encounter the liquid outer core, which is less rigid than the mantle, they slow down. This makes the P-waves arrive later and further away than would be expected. The result is a P-wave shadow zone. No P-waves are picked up at seismographs 104o to 140o from the earthquakes focus. | image | textbook_images/seismic_waves_21106.png |
L_0305 | seismic waves | T_1681 | FIGURE 1.3 How P-waves travel through Earths interior. | image | textbook_images/seismic_waves_21107.png |
L_0306 | short term climate change | T_1686 | FIGURE 1.1 Under normal conditions, low pressure and warm water (shown in red) build up in the western Pacific Ocean. Notice that continents are shown in brown in the image. North and South America are on the right in this image. | image | textbook_images/short_term_climate_change_21109.png |
L_0306 | short term climate change | T_1686 | FIGURE 1.2 In El Nio conditions, the trade winds weaken or reverse directions. Warm wa- ter moves eastward across the Pacific Ocean and piles up against South Amer- ica. | image | textbook_images/short_term_climate_change_21110.png |
L_0306 | short term climate change | T_1687 | FIGURE 1.3 A La Nia year is like a normal year but the circulation patterns are more extreme. | image | textbook_images/short_term_climate_change_21111.png |
L_0311 | solar energy on earth | T_1710 | FIGURE 1.1 | image | textbook_images/solar_energy_on_earth_21126.png |
L_0311 | solar energy on earth | T_1710 | FIGURE 1.2 | image | textbook_images/solar_energy_on_earth_21127.png |
L_0312 | solar power | T_1712 | FIGURE 1.1 | image | textbook_images/solar_power_21128.png |
L_0312 | solar power | T_1712 | FIGURE 1.2 | image | textbook_images/solar_power_21129.png |
L_0312 | solar power | T_1713 | FIGURE 1.3 | image | textbook_images/solar_power_21130.png |
L_0313 | star classification | T_1714 | FIGURE 1.1 A Hertzsprung-Russell diagram shows the brightness and color of main se- quence stars. The brightness is indicated by luminosity and is higher up the y- axis. The temperature is given in degrees Kelvin and is higher on the left side of the x-axis. How does our Sun fare in terms of brightness and color compared with other stars? | image | textbook_images/star_classification_21131.png |
L_0314 | star constellations | T_1717 | FIGURE 1.1 In this image the Big Dipper is outlined and shown next to the Aurora borealis near Fairbanks, Alaska. | image | textbook_images/star_constellations_21132.png |
L_0315 | star power | T_1721 | FIGURE 1.1 A thermonuclear bomb is an uncon- trolled fusion reaction in which enormous amounts of energy are released. | image | textbook_images/star_power_21133.png |
L_0315 | star power | T_1722 | FIGURE 1.2 | image | textbook_images/star_power_21134.png |
L_0315 | star power | T_1722 | FIGURE 1.3 | image | textbook_images/star_power_21135.png |
L_0316 | states of water | T_1724 | FIGURE 1.1 A water molecule. The hydrogen atoms have a slightly positive charge, and the oxygen atom has a slightly negative charge. | image | textbook_images/states_of_water_21136.png |
L_0316 | states of water | T_1724 | FIGURE 1.2 | image | textbook_images/states_of_water_21137.png |
L_0319 | streams and rivers | T_1733 | FIGURE 1.1 | image | textbook_images/streams_and_rivers_21138.png |
L_0319 | streams and rivers | T_1733 | FIGURE 1.2 | image | textbook_images/streams_and_rivers_21139.png |
L_0319 | streams and rivers | T_1734 | FIGURE 1.3 | image | textbook_images/streams_and_rivers_21140.png |
L_0319 | streams and rivers | T_1734 | FIGURE 1.4 The East River meanders through Crested Butte, Colorado. | image | textbook_images/streams_and_rivers_21141.png |
L_0319 | streams and rivers | T_1735 | FIGURE 1.5 | image | textbook_images/streams_and_rivers_21142.png |
L_0319 | streams and rivers | T_1735 | FIGURE 1.6 | image | textbook_images/streams_and_rivers_21143.png |
L_0320 | supervolcanoes | T_1737 | FIGURE 1.1 | image | textbook_images/supervolcanoes_21144.png |
L_0320 | supervolcanoes | T_1738 | FIGURE 1.2 | image | textbook_images/supervolcanoes_21145.png |
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