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
... mountain ranges in the Andes mountain belt . A parallel but much lower range is visible at the extreme right skyline of the picture . 160 40 ° 140 ° 20 ° DO 60 °. Figure 5.1 Photo by C. C. Plummer . A mountain , as you know , is a large ...
... mountain ranges in the Andes mountain belt . A parallel but much lower range is visible at the extreme right skyline of the picture . 160 40 ° 140 ° 20 ° DO 60 °. Figure 5.1 Photo by C. C. Plummer . A mountain , as you know , is a large ...
Page 105
... mountain belts . Caledonides Urals Alps Himalaya New Zealand Alps mountain range . For instance , a geologist may study the varia- tions in metamorphic rocks in a mountainous area with the in- tent of gaining more insight to metamorphic ...
... mountain belts . Caledonides Urals Alps Himalaya New Zealand Alps mountain range . For instance , a geologist may study the varia- tions in metamorphic rocks in a mountainous area with the in- tent of gaining more insight to metamorphic ...
Page 116
... mountain belt move vertically up- ward . Erosion may keep pace with uplift and the area remain low . Alternatively , uplift may temporarily outpace erosion , re- sulting in plateaus or mountain ranges . The present Appalachian Mountains ...
... mountain belt move vertically up- ward . Erosion may keep pace with uplift and the area remain low . Alternatively , uplift may temporarily outpace erosion , re- sulting in plateaus or mountain ranges . The present Appalachian Mountains ...
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