Physical Geology: Earth RevealedCoverage of plate tectonics is moved to the beginning of the book. The text is also used as the official Annenberg CPB distributed telecourse for physical geology.The beautiful new art program and interactive writing style will grab students' attention and further their interest in the subject. |
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Page 104
... ranges . A mountain range is a group of closely spaced mountains or parallel ridges ( figure 5.1 ) . A mountain range is likely to be composed of tectonically deformed sedi- mentary , volcanic or metamorphic rocks . It may also show a ...
... ranges . A mountain range is a group of closely spaced mountains or parallel ridges ( figure 5.1 ) . A mountain range is likely to be composed of tectonically deformed sedi- mentary , volcanic or metamorphic rocks . It may also show a ...
Page 116
... range . The normal faulting implies horizontal tensional force , therefore , fault - block moun- tain ranges are caused by extension , the regional pulling apart of the crust . Isostatic vertical adjustment of a fault block probably ...
... range . The normal faulting implies horizontal tensional force , therefore , fault - block moun- tain ranges are caused by extension , the regional pulling apart of the crust . Isostatic vertical adjustment of a fault block probably ...
Page 414
Earth Revealed David McGeary, Charles C. Plummer. Faults Mountain range Valley Mountain range Valley Figure 18.10 Fault Two possible origins of the mountains and valleys of the Basin and Range province . Movement along the faults is ...
Earth Revealed David McGeary, Charles C. Plummer. Faults Mountain range Valley Mountain range Valley Figure 18.10 Fault Two possible origins of the mountains and valleys of the Basin and Range province . Movement along the faults is ...
Contents
Chapter | 6 |
Box 8 | 8 |
Delivering Alaskan OilThe Environment vs the Economy | 10 |
Copyright | |
74 other sections not shown
Common terms and phrases
abyssal plains andesite asthenosphere atoms basalt basin beds beneath Benioff zone California Canyon caused chapter chemical weathering composition continental crust continental rise continental slope continents convection converging boundary cooling core craton crystal deep deposited depth dikes diverging boundary drilling earth's crust earth's surface earthquakes erosion eruptions feldspar folds fossils fracture zones gabbro geologists granite gravity heat flow horizontal hot mantle igneous rock isostatic kilometers lava flows lithosphere mafic magma magnetic anomalies mantle rock melting metamorphic rocks meteorites meters mid-oceanic ridge million mountain belt mountain ranges move normal faults occur oceanic crust oceanic trenches Photo plate boundaries plate motion plate tectonics plutonic pressure quake quartz reef regions ridge crest rift valley San Andreas fault sandstone sea floor sea level sediment sedimentary rock seismic waves shale shown in figure silicate soil solidified stress structure subducting plate temperature terrane thick turbidity currents U.S. Geological Survey uplift volcanoes