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 | |
73 other sections not shown
Common terms and phrases
active America anomalies atoms basalt becomes beds beneath block boundary break building California called caused chapter chemical composition continental continental crust continents cooling core crystal currents deep deposited depth described determine direction earth's magnetic field earth's surface earthquakes erosion eruptions evidence example explain fault field figure flow folds forces geologic geologists granite gravity heat horizontal igneous increase indicate island kilometers land lava layers less lines lithosphere lower magma magnetic mantle margin mass material melting metamorphic meters mid-oceanic ridge million minerals motion mountain belt move movement normal North occur oceanic crust original Photo plains plate tectonics poles position present pressure processes quake quartz range regions relatively ridge rise sea floor sediment sedimentary rock seismic seismic refraction shown slope soil South stress structure subduction surface temperature theory thick Trench United usually volcanoes waves weathering zone