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 165
... building's height and mass . Nat- ural bodies of rock and sediment vibrate the same way , with periods that vary ... building design can greatly lessen earthquake damage . A B Box 7.1 Figure 1 Mexico City earthquake , 1985. ( A ) This 15 ...
... building's height and mass . Nat- ural bodies of rock and sediment vibrate the same way , with periods that vary ... building design can greatly lessen earthquake damage . A B Box 7.1 Figure 1 Mexico City earthquake , 1985. ( A ) This 15 ...
Page 192
... buildings with a high radon level , the gas seeps in from the underlying soil through the building's founda- tion . If a building's windows are kept open and fresh air cir- culates freely , radon concentrations cannot build up . How ...
... buildings with a high radon level , the gas seeps in from the underlying soil through the building's founda- tion . If a building's windows are kept open and fresh air cir- culates freely , radon concentrations cannot build up . How ...
Page 213
... building . If a building is erected on expansive clay that subse- quently gets wet , a portion of the building will be shoved up- ward . In all likelihood the building will break . Some people think that expansive soils have caused more ...
... building . If a building is erected on expansive clay that subse- quently gets wet , a portion of the building will be shoved up- ward . In all likelihood the building will break . Some people think that expansive soils have caused more ...
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