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NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_3617 | image | textbook_images/pressure_of_fluids_22294.png | FIGURE 15.4 The pressure of ocean water increases rapidly as the water gets deeper. | 0.336412 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | DQ_003164 | image | question_images/ocean_currents_7112.png | ocean_currents_7112.png | 0.333026 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_4686 | image | textbook_images/oceanic_pressure_22994.png | FIGURE 1.1 | 0.32784 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | DQ_000254 | image | question_images/ocean_zones_8126.png | ocean_zones_8126.png | 0.320823 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_0180 | image | textbook_images/ocean_movements_20120.png | FIGURE 14.17 Deep currents flow because of differences in density of ocean water. | 0.320672 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | DD_0015 | image | teaching_images/ocean_waves_7117.png | This diagram illustrates the components and behavior of a wave propagating through water. The highest point in a wave is called the Crest, whereas the lowest point is called the Trough. Waves are periodic, meaning they maintain the same pattern as they propagate. The distance from one crest to another is called the Wavelength. The wavelength can also be measured from any point in the wave to the next point at the same elevation. Beneath the wave crests, water molecules tend to move in an orbital path. Two important properties of a wave are its Frequency and Period. The frequency of a wave is related to how fast the wave is moving. Frequency is defined as the number of times a particular point in a wave, say a crest, passes by a given point each second. Period is defined as the time it takes for a wave to move through one wavelength or cycle. | 0.317222 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | DQ_000216 | image | abc_question_images/ocean_zones_18126.png | ocean_zones_18126.png | 0.316252 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | DQ_000234 | image | question_images/ocean_zones_7138.png | ocean_zones_7138.png | 0.31623 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_0207 | image | textbook_images/the_atmosphere_20136.png | 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? | 0.308887 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | DQ_000239 | image | question_images/ocean_zones_7139.png | ocean_zones_7139.png | 0.307723 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_0250 | text | null | The water cycle plays an important role in weather. When liquid water evaporates, it causes humidity. When water vapor condenses, it forms clouds and precipitation. Humidity, clouds, and precipitation are all important weather factors. | 0.732868 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_1319 | text | null | The oceans are an essential part of Earths water cycle. Since they cover so much of the planet, most evaporation comes from oceans and most precipitation falls on oceans. | 0.725992 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_1578 | text | null | The atmosphere has different properties at different elevations above sea level, or altitudes. | 0.724528 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_0102 | text | null | Earths atmosphere slowly cooled. Once it was cooler, water vapor could condense. It changed back to its liquid form. Liquid water could fall to Earths surface as rain. Over millions of years water collected to form the oceans. Water began to cycle on Earth as water evaporated from the oceans and returned again as rainfall. | 0.723649 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_1753 | text | null | The atmosphere is layered, corresponding with how the atmospheres temperature changes with altitude. By under- standing the way temperature changes with altitude, we can learn a lot about how the atmosphere works. | 0.723196 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_1593 | text | null | Most of Earths water is stored in the oceans, where it can remain for hundreds or thousands of years. | 0.721191 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_0229 | text | null | Air temperature in the stratosphere layer increases with altitude. Why? The stratosphere gets most of its heat from the Sun. Therefore, its warmer closer to the Sun. The air at the bottom of the stratosphere is cold. The cold air is dense, so it doesnt rise. As a result, there is little mixing of air in this layer. | 0.719969 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_1235 | text | null | The high and low pressure areas created by the six atmospheric circulation cells also determine in a general way the amount of precipitation a region receives. Rain is common in low pressure regions due to rising air. Air sinking in high pressure areas causes evaporation; these regions are usually dry. These features have a great deal of influence on climate. | 0.716916 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_0147 | text | null | Freshwater below Earths surface is called groundwater. The water infiltrates, or seeps down into, the ground from the surface. How does this happen? And where does the water go? | 0.715111 |
NDQ_017923 | the depth of water where oceanic pressure is double atmospheric pressure at the surface is | null | a. 30 meters., b. 300 meters., c. 400 meters., d. 11000 meters. | a | T_0160 | text | null | Oceans cover more than 70 percent of Earths surface and hold 97 percent of its surface water. Its no surprise that the oceans have a big influence on the planet. The oceans affect the atmosphere, climate, and living things. | 0.711402 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | DQ_000234 | image | question_images/ocean_zones_7138.png | ocean_zones_7138.png | 0.344947 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0185 | image | textbook_images/the_ocean_floor_20125.png | FIGURE 14.22 The features of the ocean floor. This dia- gram has a lot of vertical exaggeration. | 0.319339 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_3617 | image | textbook_images/pressure_of_fluids_22294.png | FIGURE 15.4 The pressure of ocean water increases rapidly as the water gets deeper. | 0.314157 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | DQ_000403 | image | question_images/parts_ocean_floor_7239.png | parts_ocean_floor_7239.png | 0.313788 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0170 | image | textbook_images/ocean_movements_20112.png | FIGURE 14.9 A wave travels through the water. How would you describe the movement of wa- ter molecules as a wave passes through? | 0.30868 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0181 | image | textbook_images/ocean_movements_20121.png | FIGURE 14.18 An upwelling occurs when deep ocean water rises to the surface. | 0.308398 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_4130 | image | textbook_images/archimedes_law_22664.png | FIGURE 1.1 | 0.308262 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_1046 | image | textbook_images/deep_ocean_currents_20688.png | FIGURE 1.2 | 0.307505 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_3626 | image | textbook_images/buoyancy_of_fluids_22303.png | FIGURE 15.13 Whether an object sinks or floats depends on its weight and the strength of the buoyant force acting on it. | 0.306137 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_4686 | image | textbook_images/oceanic_pressure_22994.png | FIGURE 1.1 | 0.303754 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0298 | text | null | When a place is near an ocean, the water can have a big effect on the climate. | 0.683755 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0160 | text | null | Oceans cover more than 70 percent of Earths surface and hold 97 percent of its surface water. Its no surprise that the oceans have a big influence on the planet. The oceans affect the atmosphere, climate, and living things. | 0.674902 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0038 | text | null | Eventually, the sediment in ocean water is deposited. Deposition occurs where waves and other ocean motions slow. The smallest particles, such as silt and clay, are deposited away from shore. This is where water is calmer. Larger particles are deposited on the beach. This is where waves and other motions are strongest. | 0.673849 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0187 | text | null | The ocean floor is home to many species of living things. Some from shallow water are used by people for food. Clams and some fish are among the many foods we get from the ocean floor. Some living things on the ocean floor are sources of human medicines. For example, certain bacteria on the ocean floor produce chemicals that fight cancer. | 0.666557 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_2434 | text | null | The ocean is huge but even this body of water is becoming seriously polluted. Climate change also affects the quality of ocean water for living things. | 0.666345 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_1319 | text | null | The oceans are an essential part of Earths water cycle. Since they cover so much of the planet, most evaporation comes from oceans and most precipitation falls on oceans. | 0.665829 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_1593 | text | null | Most of Earths water is stored in the oceans, where it can remain for hundreds or thousands of years. | 0.661971 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0186 | text | null | The ocean floor is rich in resources. The resources include both living and nonliving things. | 0.661691 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_1443 | text | null | Water on Earth, such as the water in the oceans, contains chemical elements mixed into a solution. Various processes can cause these elements to combine to form solid mineral deposits. | 0.657793 |
NDQ_017924 | without special equipment, humans cannot withstand the pressure of ocean water below | null | a. 50 meters., b. 100 meters., c. 200 meters., d. 500 meters. | d | T_0164 | text | null | You know that ocean water is salty. But do you know why? How salty is it? | 0.654331 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | DQ_011173 | image | question_images/optics_refraction_9193.png | optics_refraction_9193.png | 0.316139 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | DQ_011175 | image | question_images/optics_refraction_9194.png | optics_refraction_9194.png | 0.316083 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_3747 | image | textbook_images/science_skills_22397.png | FIGURE 2.6 This cylinder contains about 66 mL of liquid. What would the measure- ment be if you read the top of the meniscus by mistake? MEDIA Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/5036 | 0.312197 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_3617 | image | textbook_images/pressure_of_fluids_22294.png | FIGURE 15.4 The pressure of ocean water increases rapidly as the water gets deeper. | 0.309782 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | DQ_000216 | image | abc_question_images/ocean_zones_18126.png | ocean_zones_18126.png | 0.306449 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_4686 | image | textbook_images/oceanic_pressure_22994.png | FIGURE 1.1 | 0.306434 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_1411 | image | textbook_images/mechanical_weathering_20927.png | FIGURE 1.1 Ice wedging. | 0.304666 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | DQ_012206 | image | question_images/optics_reflection_9185.png | optics_reflection_9185.png | 0.304166 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | DQ_012198 | image | question_images/optics_reflection_9181.png | optics_reflection_9181.png | 0.304166 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_3800 | image | textbook_images/properties_of_electromagnetic_waves_22425.png | FIGURE 21.4 Light slows down when it enters water from the air. This causes the wave to refract, or bend. | 0.304085 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_0147 | text | null | Freshwater below Earths surface is called groundwater. The water infiltrates, or seeps down into, the ground from the surface. How does this happen? And where does the water go? | 0.604817 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_0669 | text | null | Most water on Earth, like the water in the oceans, contains elements. The elements are mixed evenly through the water. Water plus other substances makes a solution. The particles are so small that they will not come out when you filter the water. But the elements in water can form solid mineral deposits. | 0.602302 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_0024 | text | null | Flowing water slows down when it reaches flatter land or flows into a body of still water. What do you think happens then? The water starts dropping the particles it was carrying. As the water slows, it drops the largest particles first. The smallest particles settle out last. | 0.594961 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_1593 | text | null | Most of Earths water is stored in the oceans, where it can remain for hundreds or thousands of years. | 0.571545 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_4893 | text | null | A given kind of matter has the same chemical makeup and the same chemical properties regardless of its state. Thats because state of matter is a physical property. As a result, when matter changes state, it doesnt become a different kind of substance. For example, water is still water whether it exists as ice, liquid water, or water vapor. | 0.571175 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_1277 | text | null | Water sometimes comes into contact with hot rock. The water may emerge at the surface as either a hot spring or a geyser. | 0.565694 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_0164 | text | null | You know that ocean water is salty. But do you know why? How salty is it? | 0.56128 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_4018 | text | null | Water (H2 O) is an example of a chemical compound. Water molecules always consist of two atoms of hydrogen and one atom of oxygen. Like water, all other chemical compounds consist of a fixed ratio of elements. It doesnt matter how much or how little of a compound there is. It always has the same composition. | 0.560416 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_0032 | text | null | Some water soaks into the ground. It travels down through tiny holes in soil. It seeps through cracks in rock. The water moves slowly, pulled deeper and deeper by gravity. Underground water can also erode and deposit material. | 0.560402 |
NDQ_017926 | the depth of the water at the place described in question 6 is | null | a. 500 meters., b. 700 meters., c. 900 meters., d. 11000 meters. | d | T_1597 | text | null | Water may seep through dirt and rock below the soil and then through pores infiltrating the ground to go into Earths groundwater system. Groundwater enters aquifers that may store fresh water for centuries. Alternatively, the water may come to the surface through springs or find its way back to the oceans. | 0.559078 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_4114 | image | textbook_images/air_pressure_and_altitude_22656.png | FIGURE 1.1 | 0.325895 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_3617 | image | textbook_images/pressure_of_fluids_22294.png | FIGURE 15.4 The pressure of ocean water increases rapidly as the water gets deeper. | 0.322421 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_3618 | image | textbook_images/pressure_of_fluids_22296.png | FIGURE 15.6 This graph shows how air pressure de- creases with increasing altitude. the air pressure on the surface of the drink. Because fluid flows from an area of high to low pressure, the drink moves up the straw and into your mouth. When you breathe, a muscle called the diaphragm causes the rib cage and lungs to expand or contract. When they expand, the air in the lungs is under less pressure than the air outside the body, so air flows into the lungs. When the ribs and lungs contract, air in the lungs is under greater pressure than air outside the body, so air flows out of the lungs. | 0.321858 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_4686 | image | textbook_images/oceanic_pressure_22994.png | FIGURE 1.1 | 0.316075 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | DQ_000254 | image | question_images/ocean_zones_8126.png | ocean_zones_8126.png | 0.310416 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | DQ_000216 | image | abc_question_images/ocean_zones_18126.png | ocean_zones_18126.png | 0.3101 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | DQ_000239 | image | question_images/ocean_zones_7139.png | ocean_zones_7139.png | 0.302889 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_1516 | image | textbook_images/ocean_zones_21006.png | FIGURE 1.1 Vertical and horizontal ocean zones. | 0.290448 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_4051 | image | textbook_images/types_of_chemical_reactions_22613.png | FIGURE 8.8 As carbon dioxide increases in the atmo- sphere, more carbon dioxide dissolves in ocean water. | 0.29034 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | DQ_000318 | image | question_images/ocean_waves_7126.png | ocean_waves_7126.png | 0.290083 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_1593 | text | null | Most of Earths water is stored in the oceans, where it can remain for hundreds or thousands of years. | 0.671268 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_1578 | text | null | The atmosphere has different properties at different elevations above sea level, or altitudes. | 0.661178 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_1319 | text | null | The oceans are an essential part of Earths water cycle. Since they cover so much of the planet, most evaporation comes from oceans and most precipitation falls on oceans. | 0.64643 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_1515 | text | null | Oceanographers divide the ocean into zones both vertically and horizontally. | 0.644217 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_0298 | text | null | When a place is near an ocean, the water can have a big effect on the climate. | 0.643419 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_0186 | text | null | The ocean floor is rich in resources. The resources include both living and nonliving things. | 0.641103 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_0160 | text | null | Oceans cover more than 70 percent of Earths surface and hold 97 percent of its surface water. Its no surprise that the oceans have a big influence on the planet. The oceans affect the atmosphere, climate, and living things. | 0.638412 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_1753 | text | null | The atmosphere is layered, corresponding with how the atmospheres temperature changes with altitude. By under- standing the way temperature changes with altitude, we can learn a lot about how the atmosphere works. | 0.63333 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_1235 | text | null | The high and low pressure areas created by the six atmospheric circulation cells also determine in a general way the amount of precipitation a region receives. Rain is common in low pressure regions due to rising air. Air sinking in high pressure areas causes evaporation; these regions are usually dry. These features have a great deal of influence on climate. | 0.627902 |
NDQ_017929 | for each additional meter below the oceans surface, pressure changes by 100 kpa. | null | a. true, b. false | b | T_0777 | text | null | Plates move apart at divergent plate boundaries. This can occur in the oceans or on land. | 0.627484 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_3624 | image | textbook_images/buoyancy_of_fluids_22302.png | FIGURE 15.12 Fluid pressure exerts force on all sides of this object, but the force is greater at the bottom of the object where the fluid is deeper. | 0.381138 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_4183 | image | textbook_images/buoyancy_22689.png | FIGURE 1.1 | 0.377168 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_3947 | image | textbook_images/behavior_of_gases_22545.png | FIGURE 4.12 As the volume of a gas increases, its pressure decreases. | 0.312074 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_0287 | image | textbook_images/weather_forecasting_20178.png | FIGURE 16.23 The greater the air pressure outside the tube, the higher the mercury rises inside the tube. Mercury can rise in the tube because theres no air pressing down on it. | 0.310396 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | DD_0234 | image | teaching_images/states_of_matter_9253.png | There are three states of matter. These three states include solid, liquid, and gas. Solid states of matter are rigid and have a fixed shape and fixed volume. They cannot be squashed. Liquid states of matter are not rigid and have no fixed shape, but have a fixed volume. They too cannot be squashed. Gas states of matter are not rigid and have no fixed shape and no fixed volume. This state of matter can be squashed. | 0.307021 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | DQ_011501 | image | question_images/states_of_matter_7614.png | states_of_matter_7614.png | 0.301011 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | DQ_011650 | image | question_images/state_change_7602.png | state_change_7602.png | 0.298391 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_4740 | image | textbook_images/pressure_in_fluids_23030.png | FIGURE 1.3 | 0.297465 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_3944 | image | textbook_images/solids_liquids_gases_and_plasmas_22541.png | FIGURE 4.8 Kinetic energy is needed to overcome the force of attraction between particles of the same substance. | 0.295881 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_4583 | image | textbook_images/lipid_classification_22927.png | FIGURE 1.3 | 0.294049 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_3801 | text | null | Although all electromagnetic waves travel at the same speed, they may differ in their wavelength and frequency. | 0.700065 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_4715 | text | null | Compare and contrast the basic properties of matter, such as mass and volume. | 0.678192 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_3960 | text | null | Solids that change to gases generally first pass through the liquid state. However, sometimes solids change directly to gases and skip the liquid state. The reverse can also occur. Sometimes gases change directly to solids. | 0.677774 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_0024 | text | null | Flowing water slows down when it reaches flatter land or flows into a body of still water. What do you think happens then? The water starts dropping the particles it was carrying. As the water slows, it drops the largest particles first. The smallest particles settle out last. | 0.672186 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_3860 | text | null | Electric current cannot travel through empty space. It needs a material through which to travel. However, when current travels through a material, the flowing electrons collide with particles of the material, and this creates resistance. | 0.663835 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_3939 | text | null | Water vapor is an example of a gas. A gas is matter that has neither a fixed volume nor a fixed shape. Instead, a gas takes both the volume and the shape of its container. It spreads out to take up all available space. You can see an example in Figure 4.6. | 0.662887 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_3946 | text | null | For a given amount of gas, scientists have discovered that the pressure, volume, and temperature of a gas are related in certain ways. Because these relationships always hold in nature, they are called laws. The laws are named for the scientists that discovered them. | 0.662099 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_4940 | text | null | Friction is the force that opposes motion between any surfaces that are in contact. There are four types of friction: static, sliding, rolling, and fluid friction. Static, sliding, and rolling friction occur between solid surfaces. Fluid friction occurs in liquids and gases. All four types of friction are described below. | 0.661862 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_0251 | text | null | Humidity is the amount of water vapor in the air. High humidity increases the chances of clouds and precipitation. | 0.659128 |
NDQ_017962 | pressure always spreads throughout a fluid. | null | a. true, b. false | a | T_4893 | text | null | A given kind of matter has the same chemical makeup and the same chemical properties regardless of its state. Thats because state of matter is a physical property. As a result, when matter changes state, it doesnt become a different kind of substance. For example, water is still water whether it exists as ice, liquid water, or water vapor. | 0.657882 |
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