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Published byFerdinand Lane Modified over 8 years ago
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a) San Andreas b) San Jacinto c) Garlock d) Imperial
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a) CO2 b) Nitrogen c) Oxygen d) Water vapor
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a) Air pressure b) Temperature c) Nitrogen and oxygen concentration d) Ozone concentration
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a) Ozone b) Pressure c) Clouds d) gravity
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a) Temperature conversion b) Temperature inversion c) Thermal conversion d) Thermal convection
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a) Bacteria in the roots of legumes b) Respiration c) Decomposition of proteins in the soil d) photosynthesis
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a) Coal, oil, and natural gas b) Dissolved carbon dioxide, bicarbonate, carbonate ions c) Organic molecules and fossil fuels d) Simple sugars, carbon dioxide, and methane gas
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a) Cementing of sediments underground b) Compression of rock in mountain building c) Cooling of magma underground d) Cooling of lava above ground
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a) Cementing sediments underground b) Compression of rock in mountain building c) Cooling o magma underground d) Cooling of lave above ground
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a) Intrusive and extrusive b) Erosion and compaction c) Cementation and compaction d) Clastic and chemical
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a) Characteristics of living organisms on the seafloor b) Patterns of magnetic fields on the seafloor c) The relatively young age of the seafloor d) Topographical features on the seafloor
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a) Convergent boundary b) Transform boundary c) Divergent boundary d) Major plate
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a) Flexible rebound hypothesis b) Regressing recoil hypothesis c) Recovering rock hypothesis d) Elastic rebound hypothesis
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a) Epicenter b) Fault c) Fracture d) Focus
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a) The lowering of aquifer levels b) The interaction of tides with the coast c) Mining activity in the nineteenth century d) Plates moving past each other along active faults
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a) Lava type and height b) Lava type and shape c) Eruption frequency and height d) Eruption frequency and shape
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a) Northern and western b) Northern and eastern c) Central and western d) Eastern and southern
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a) Sea floor spreading b) Underwater volcanoes c) Erosion of ocean ridges d) Deep sea thermal venting
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