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L_1054 | transverse wave | T_4938 | FIGURE 1.2 | image | textbook_images/transverse_wave_23130.png |
L_1054 | transverse wave | T_4939 | FIGURE 1.3 | image | textbook_images/transverse_wave_23131.png |
L_1055 | types of friction | T_4941 | FIGURE 1.1 | image | textbook_images/types_of_friction_23132.png |
L_1055 | types of friction | T_4943 | FIGURE 1.2 | image | textbook_images/types_of_friction_23133.png |
L_1055 | types of friction | T_4944 | FIGURE 1.3 | image | textbook_images/types_of_friction_23134.png |
L_1056 | ultrasound | T_4947 | FIGURE 1.1 | image | textbook_images/ultrasound_23136.png |
L_1056 | ultrasound | T_4947 | FIGURE 1.2 Distance = 1437 m/s 1 s = 1437 m | image | textbook_images/ultrasound_23137.png |
L_1056 | ultrasound | T_4948 | FIGURE 1.3 | image | textbook_images/ultrasound_23138.png |
L_1057 | unsaturated hydrocarbons | T_4950 | FIGURE 1.1 | image | textbook_images/unsaturated_hydrocarbons_23139.png |
L_1057 | unsaturated hydrocarbons | T_4951 | FIGURE 1.2 Q: How many bonds does each carbon atom in benzene form? | image | textbook_images/unsaturated_hydrocarbons_23140.png |
L_1057 | unsaturated hydrocarbons | T_4952 | FIGURE 1.3 | image | textbook_images/unsaturated_hydrocarbons_23141.png |
L_1057 | unsaturated hydrocarbons | T_4952 | FIGURE 1.4 | image | textbook_images/unsaturated_hydrocarbons_23142.png |
L_1058 | using earths magnetic field | T_4954 | FIGURE 1.1 | image | textbook_images/using_earths_magnetic_field_23143.png |
L_1058 | using earths magnetic field | T_4955 | FIGURE 1.2 | image | textbook_images/using_earths_magnetic_field_23144.png |
L_1059 | valence electrons | T_4959 | FIGURE 1.1 | image | textbook_images/valence_electrons_23145.png |
L_1059 | valence electrons | T_4959 | FIGURE 1.2 | image | textbook_images/valence_electrons_23146.png |
L_1059 | valence electrons | T_4959 | FIGURE 1.3 | image | textbook_images/valence_electrons_23147.png |
L_1059 | valence electrons | T_4959 | FIGURE 1.4 | image | textbook_images/valence_electrons_23148.png |
L_1059 | valence electrons | T_4960 | FIGURE 1.5 | image | textbook_images/valence_electrons_23149.png |
L_1060 | velocity | T_4962 | FIGURE 1.1 | image | textbook_images/velocity_23150.png |
L_1061 | velocity time graphs | T_4966 | FIGURE 1.1 | image | textbook_images/velocity_time_graphs_23151.png |
L_1062 | visible light and matter | T_4967 | FIGURE 1.1 | image | textbook_images/visible_light_and_matter_23152.png |
L_1062 | visible light and matter | T_4968 | FIGURE 1.2 | image | textbook_images/visible_light_and_matter_23153.png |
L_1062 | visible light and matter | T_4968 | FIGURE 1.3 | image | textbook_images/visible_light_and_matter_23154.png |
L_1062 | visible light and matter | T_4970 | FIGURE 1.4 | image | textbook_images/visible_light_and_matter_23155.png |
L_1062 | visible light and matter | T_4970 | FIGURE 1.5 | image | textbook_images/visible_light_and_matter_23156.png |
L_1063 | vision and the eye | T_4971 | FIGURE 1.1 | image | textbook_images/vision_and_the_eye_23157.png |
L_1063 | vision and the eye | T_4972 | FIGURE 1.2 | image | textbook_images/vision_and_the_eye_23158.png |
L_1063 | vision and the eye | DD_0272 | The ability to see is called vision. The eyes sense light and form images which The brain then interprets. the images are formed by the eyes and the brain tells us what we are looking at. All creatures have different types of eyes, some are great at seeing vast distances such as the eagle or owl and some are able to pick up light in dark settings in order to see better at night, such as cats. Many people have issues with their vision but we have been able to correct this with lenses which come in the form of glasses or contact lenses. The eyes are made up of several parts the pupil, cornea, iris, lens, retina and the optic nerve which carries the images the eyes sees and takes the images to brain for it to interpret. | image | teaching_images/human_system_eye_2857.png |
L_1063 | vision and the eye | DD_0273 | Below is a diagram of the structure of the eyeball. As you can see below, the eyeball is made up of various parts. One of the major parts is the cornea. The cornea of the eyeball is a clear covering that protects the eyeball. The light first comes through the cornea then goes through the pupil. The pupil is the opening in the center of the eyeball. The pupil is the dark part in the center of the iris, which is the colored part of the eye. The light then goes through the lens and reaches the retina. The retina is the part where the image first occurs. Then the optic nerves carries the impulses to the brain. | image | teaching_images/human_system_eye_6138.png |
L_1063 | vision and the eye | DD_0274 | This picture shows the parts of the eye. The light enters the eye through the pupil. The cornea covers the eye and protects it from damage. The iris controls the size of the pupil. The size of the pupil changes based on the amount of light that enters the eye. The lens projects the image onto retina. The retina has nerve cells which transmit color and other information to the brain. The space between the lens and Retina is filled by a transparent liquid called Viterous gel. Fovea has the highest concentration of cone cells. Cone cells are responsible for seeing color and function best in bright light. | image | teaching_images/human_system_eye_2876.png |
L_1064 | vision problems and corrective lenses | T_4974 | FIGURE 1.1 | image | textbook_images/vision_problems_and_corrective_lenses_23159.png |
L_1064 | vision problems and corrective lenses | T_4975 | FIGURE 1.2 | image | textbook_images/vision_problems_and_corrective_lenses_23160.png |
L_1065 | wave amplitude | T_4977 | FIGURE 1.1 | image | textbook_images/wave_amplitude_23161.png |
L_1066 | wave frequency | T_4979 | FIGURE 1.1 A: Waves with a higher frequency have crests that are closer together, so higher frequency waves have shorter wavelengths. | image | textbook_images/wave_frequency_23164.png |
L_1066 | wave frequency | T_4980 | FIGURE 1.2 | image | textbook_images/wave_frequency_23165.png |
L_1067 | wave interactions | T_4984 | FIGURE 1.1 | image | textbook_images/wave_interactions_23166.png |
L_1067 | wave interactions | T_4987 | FIGURE 1.2 | image | textbook_images/wave_interactions_23167.png |
L_1068 | wave interference | T_4991 | FIGURE 1.1 | image | textbook_images/wave_interference_23168.png |
L_1068 | wave interference | T_4993 | FIGURE 1.2 | image | textbook_images/wave_interference_23169.png |
L_1068 | wave interference | DD_0275 | This diagram shows the result of constructive wave interference. The highest point of a waveâs amplitude is called a crest. The lowest point in amplitude is called a trough. Constructive interference occurs when two waves meet and overlap so that their crests and troughs align. In this image, the crests and troughs of Wave 1 and Wave 2 synchronize. This causes an increase in amplitude. The result is the wave on the right, which has a greater amplitude than Wave 1 and Wave 2. | image | teaching_images/waves_interactions_interference_7681.png |
L_1068 | wave interference | DD_0276 | This diagram shows the results of constructive interference and destructive interference in sound waves. Wave interference is when two waves meet while traveling in opposite directions. The highest point of a waveâs amplitude is called a crest. The lowest point in amplitude is called a trough. In the example of constructive interference, the crests and troughs of the two waves align. This causes increased wave amplitude when the two waves overlap. In the example of destructive interference, the highest point of amplitude of one wave occurs at the lowest point of the other and cancel each other out. This causes decreased wave amplitude when the two waves overlap. | image | teaching_images/waves_interactions_interference_9298.png |
L_1069 | wave particle theory | T_4996 | FIGURE 1.1 | image | textbook_images/wave_particle_theory_23170.png |
L_1071 | wavelength | T_5005 | FIGURE 1.1 | image | textbook_images/wavelength_23172.png |
L_1071 | wavelength | T_5005 | FIGURE 1.2 | image | textbook_images/wavelength_23173.png |
L_1071 | wavelength | T_5005 | FIGURE 1.3 Q: Of all the colors of visible light, red light has the longest wavelength and violet light has the shortest wavelength. Which color of light has the greatest energy? | image | textbook_images/wavelength_23174.png |
L_1072 | wedge | T_5007 | FIGURE 1.1 | image | textbook_images/wedge_23175.png |
L_1072 | wedge | T_5007 | FIGURE 1.2 | image | textbook_images/wedge_23176.png |
L_1073 | wheel and axle | T_5008 | FIGURE 1.1 Q: Where is the force applied in a Ferris wheel and a doorknob? Is it applied to the wheel or to the axle? | image | textbook_images/wheel_and_axle_23178.png |
L_1074 | why earth is a magnet | T_5011 | FIGURE 1.1 | image | textbook_images/why_earth_is_a_magnet_23179.png |
L_1076 | work | T_5014 | FIGURE 1.1 | image | textbook_images/work_23180.png |
L_1076 | work | T_5015 | FIGURE 1.2 | image | textbook_images/work_23181.png |
L_0007 | erosion and deposition by gravity | T_0059 | FIGURE 10.30 This 2001 landslide in El Salvador (Central America) was started by an earthquake. Soil and rocks flowed down a hillside and swallowed up houses in the city below. | image | textbook_images/erosion_and_deposition_by_gravity_20047.png |
L_0007 | erosion and deposition by gravity | T_0060 | FIGURE 10.31 Mudslide. A mudslide engulfs whatever is in its path. | image | textbook_images/erosion_and_deposition_by_gravity_20048.png |
L_0007 | erosion and deposition by gravity | T_0062 | FIGURE 10.32 Slump takes place suddenly, like a land- slide. How does slump differ from a land- slide? | image | textbook_images/erosion_and_deposition_by_gravity_20049.png |
L_0007 | erosion and deposition by gravity | T_0063 | FIGURE 10.33 Creep is seen on a hillside. What evi- dence shows creep has occurred? | image | textbook_images/erosion_and_deposition_by_gravity_20050.png |
L_0021 | the atmosphere | T_0196 | FIGURE 15.1 The atmosphere shields Earth from harmful solar rays. | image | textbook_images/the_atmosphere_20133.png |
L_0021 | the atmosphere | T_0198 | FIGURE 15.2 The atmosphere is a big part of the water cycle. What do you think would happen to Earths water without it? | image | textbook_images/the_atmosphere_20134.png |
L_0021 | the atmosphere | T_0205 | FIGURE 15.3 This graph identifies the most common gases in air. | image | textbook_images/the_atmosphere_20135.png |
L_0021 | the atmosphere | T_0207 | FIGURE 15.4 This drawing represents a column of air. The column rises from sea level to the top of the atmosphere. Where does air have the greatest density? | image | textbook_images/the_atmosphere_20136.png |
L_0021 | the atmosphere | T_0209 | FIGURE 15.5 At sea level, pressure was greater outside than inside the bottle. The greater outside pressure crushed the bottle. | image | textbook_images/the_atmosphere_20137.png |
L_0025 | weather and water in the atmosphere | T_0254 | FIGURE 16.1 How much water vapor can the air hold when its temperature is 40 C? | image | textbook_images/weather_and_water_in_the_atmosphere_20156.png |
L_0025 | weather and water in the atmosphere | T_0254 | FIGURE 16.2 How hot does it feel when the air tempera- ture is 90F? It depends on the humidity. | image | textbook_images/weather_and_water_in_the_atmosphere_20157.png |
L_0025 | weather and water in the atmosphere | T_0257 | FIGURE 16.3 Find the cirrus, cirrostratus, and cirrocu- mulus clouds in the figure. What do they have in common? They all form high in the troposphere. Clouds that form in the mid troposphere have the prefix alto-, as in altocumulus. Where do stratocumulus clouds form? | image | textbook_images/weather_and_water_in_the_atmosphere_20158.png |
L_0025 | weather and water in the atmosphere | T_0261 | FIGURE 16.4 Frozen precipitation may fall as snow, sleet, or freezing rain. type of frozen precipitation. Hail forms in thunderstorms when strong updrafts carry rain high into the troposphere. The rain freezes into balls of ice called hailstones. This may happen over and over again until the hailstones are as big as baseballs. Hail forms only in cumulonimbus clouds. | image | textbook_images/weather_and_water_in_the_atmosphere_20159.png |
L_0035 | loss of soil | T_0355 | FIGURE 19.1 Runoff carried away the bare soil in this field. Why do you think the soil bare to begin with? | image | textbook_images/loss_of_soil_20230.png |
L_0035 | loss of soil | T_0355 | FIGURE 19.2 Farming leaves some soil exposed to ero- sion. | image | textbook_images/loss_of_soil_20231.png |
L_0035 | loss of soil | T_0356 | FIGURE 19.3 Sheep and goats can damage plants and leave the soil bare. | image | textbook_images/loss_of_soil_20232.png |
L_0035 | loss of soil | T_0360 | FIGURE 19.4 Logging, mining, construction, and paving surfaces are some of the ways that soil erosion increases. | image | textbook_images/loss_of_soil_20233.png |
L_0035 | loss of soil | T_0360 | FIGURE 19.5 Whats fun for people may be bad for soil. Off-road vehicles can destroy plants and leave the ground bare. This sets up the soil for erosion. | image | textbook_images/loss_of_soil_20234.png |
L_0035 | loss of soil | T_0361 | FIGURE 19.6 There are many farming methods that help prevent soil erosion. | image | textbook_images/loss_of_soil_20235.png |
L_0046 | century tsunami | T_0449 | FIGURE 1.1 | image | textbook_images/century_tsunami_20315.png |
L_0046 | century tsunami | T_0450 | FIGURE 1.2 This map shows the peak tsunami wave heights. | image | textbook_images/century_tsunami_20316.png |
L_0046 | century tsunami | T_0450 | FIGURE 1.3 An aerial view shows the damage to Sendai, Japan caused by the earthquake and tsunami. The black smoke is coming from an oil refinery, which was set on fire by the earthquake. The tsunami pre- vented efforts to extinguish the fire until several days after the earthquake. | image | textbook_images/century_tsunami_20317.png |
L_0046 | century tsunami | T_0451 | FIGURE 1.4 A sign in Thailand shows an evacuation route. | image | textbook_images/century_tsunami_20318.png |
L_0063 | the universe | T_0633 | FIGURE 26.15 This is a simplified diagram of the ex- pansion of the universe. The distance between galaxies gets bigger, but the size of each galaxy stays about the same. | image | textbook_images/the_universe_20440.png |
L_0063 | the universe | T_0635 | FIGURE 26.16 HUDF09 is 13.2 billion light years away from us. This is only 480 million years after the Big Bang. The smaller box shows where the galaxy is and the larger box contains a larger image of the galaxy. This is part of the Hubble Ultra Deep Field. | image | textbook_images/the_universe_20441.png |
L_0064 | minerals | T_0638 | FIGURE 3.1 Silver is used to make sterling silver jew- elry. Table salt is the mineral halite. Glass is produced from the mineral quartz. | image | textbook_images/minerals_20442.png |
L_0064 | minerals | T_0640 | FIGURE 3.2 A water molecule has two hydrogen atoms (shown in gray) bonded to one oxygen molecule (shown in red). | image | textbook_images/minerals_20443.png |
L_0064 | minerals | T_0645 | FIGURE 3.3 Sodium ions (purple balls) bond with chloride ions (green balls) to form halite crystals. | image | textbook_images/minerals_20444.png |
L_0064 | minerals | T_0645 | FIGURE 3.4 Diamonds (A) and graphite (B) are both made of only carbon, but theyre not much alike. | image | textbook_images/minerals_20445.png |
L_0064 | minerals | T_0646 | FIGURE 3.5 Under a microscope, salt crystals are cubes. | image | textbook_images/minerals_20446.png |
L_0064 | minerals | T_0648 | FIGURE 3.6 One silicon atom bonds to four oxygen atoms to form a pyramid | image | textbook_images/minerals_20447.png |
L_0064 | minerals | T_0648 | FIGURE 3.7 Beryl (a) and biotite (b) are both silicate minerals. | image | textbook_images/minerals_20448.png |
L_0064 | minerals | T_0650 | FIGURE 3.8 The deep blue mineral is azurite and the green is malachite. Both of these carbon- ate minerals are used for jewelry. | image | textbook_images/minerals_20449.png |
L_0064 | minerals | T_0654 | FIGURE 3.9 Gypsum is the white mineral that is common around hot springs. This is Mammoth Hot Springs in Yellowstone National Park. | image | textbook_images/minerals_20450.png |
L_0065 | identification of minerals | T_0656 | FIGURE 3.10 You can use properties of a mineral to identify it. The color and rose-like struc- ture of this mineral mean that it is gyp- sum. | image | textbook_images/identification_of_minerals_20451.png |
L_0065 | identification of minerals | T_0659 | FIGURE 3.11 Quartz comes in many different colors including: (A) transparent quartz, (B) blue agate, (C) rose quartz, and (D) purple amethyst. | image | textbook_images/identification_of_minerals_20452.png |
L_0065 | identification of minerals | T_0659 | FIGURE 3.12 Rub a mineral across an unglazed porce- lain plate to see its streak. The hematite shown here has a red streak. | image | textbook_images/identification_of_minerals_20453.png |
L_0065 | identification of minerals | T_0663 | FIGURE 3.13 (A) Diamonds have an adamantine luster. These minerals are transparent and highly reflective. (B) Kaolinite is a clay with a dull or earthy luster. (C) Opals luster is greasy. (D) Chalcopyrite, like its cousin pyrite, has metallic luster. (E) Stilbite (orange) has a resinous luster. (F) The white ulexite has silky luster. (G) Sphalerite has a submetallic luster. (H) This Mayan artifact is carved from jade. Jade is a mineral with a waxy luster. Hardness 2 3 4 5 6 7 8 9 10 Mineral Gypsum Calcite Fluorite Apatite Orthoclase feldspar Quartz Topaz Corundum Diamond | image | textbook_images/identification_of_minerals_20454.png |
L_0065 | identification of minerals | T_0665 | FIGURE 3.14 Minerals with different crystal structures have a tendency to break along certain planes. | image | textbook_images/identification_of_minerals_20455.png |
L_0065 | identification of minerals | T_0665 | FIGURE 3.15 Cubes have six sides that are all the same size square. All of the angles in a cube are equal to 90. Rhombohedra also have six sides, but the sides are diamond-shaped. Octahedra have eight sides that are all shaped like triangles. | image | textbook_images/identification_of_minerals_20456.png |
L_0065 | identification of minerals | T_0667 | FIGURE 3.16 This mineral formed a smooth, curved surface when it fractured. | image | textbook_images/identification_of_minerals_20457.png |
L_0066 | formation of minerals | T_0669 | FIGURE 3.17 Lava is melted rock that erupts onto Earths surface. | image | textbook_images/formation_of_minerals_20458.png |
L_0066 | formation of minerals | T_0670 | FIGURE 3.18 When the water in glass A evaporates, the dissolved mineral particles are left behind. calcite tufa towers form. When the lake level drops, the tufa towers are revealed. | image | textbook_images/formation_of_minerals_20459.png |
L_0066 | formation of minerals | T_0670 | FIGURE 3.19 Tufa towers are found in interesting forma- tions at Mono Lake, California. | image | textbook_images/formation_of_minerals_20460.png |
L_0066 | formation of minerals | T_0671 | FIGURE 3.20 (A) A quartz vein formed in this rock. (B) Geodes form when minerals evaporate out in open spaces inside a rock. | image | textbook_images/formation_of_minerals_20461.png |
L_0067 | mining and using minerals | T_0673 | FIGURE 3.21 Aluminum is made from the minerals in rocks known as bauxite. | image | textbook_images/mining_and_using_minerals_20462.png |
L_0067 | mining and using minerals | T_0675 | FIGURE 3.22 This diamond mine is more than 500 m deep. | image | textbook_images/mining_and_using_minerals_20463.png |
L_0067 | mining and using minerals | T_0678 | FIGURE 3.23 The dome of the capital building in Hart- ford, Connecticut is coated with gold leaf. | image | textbook_images/mining_and_using_minerals_20464.png |
Subsets and Splits