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 | |
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