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. |
From inside the book
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Page 26
... geologists know about the earth's interior ? How do they obtain information about the parts of the earth beneath the surface ? Is there even a slight chance that geologists are wrong , that the earth really is hollow ? Geologists , in ...
... geologists know about the earth's interior ? How do they obtain information about the parts of the earth beneath the surface ? Is there even a slight chance that geologists are wrong , that the earth really is hollow ? Geologists , in ...
Page 58
... geologists were able to get a first- hand view of part of the submerged ridge and rift valley . A series of more than forty dives by submersibles , including ALVIN , car- ried French and American marine geologists directly into the rift ...
... geologists were able to get a first- hand view of part of the submerged ridge and rift valley . A series of more than forty dives by submersibles , including ALVIN , car- ried French and American marine geologists directly into the rift ...
Page 113
... geologists accepted the idea that a geosyncline was a necessary predecessor of a mountain belt . Geosynclines were thought to border continents along one edge of the subsiding trough and be bounded by a line of volcanic islands at the ...
... geologists accepted the idea that a geosyncline was a necessary predecessor of a mountain belt . Geosynclines were thought to border continents along one edge of the subsiding trough and be bounded by a line of volcanic islands at the ...
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