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
Results 1-3 of 28
Page 277
... acid for rock weather- ing at the earth's surface is dissolved carbon dioxide ( CO2 ) in water . Water and carbon dioxide form carbonic acid ( H2CO3 ) , a weak acid that dissociates into the hydrogen ion and the bicar- bonate ion ( see ...
... acid for rock weather- ing at the earth's surface is dissolved carbon dioxide ( CO2 ) in water . Water and carbon dioxide form carbonic acid ( H2CO3 ) , a weak acid that dissociates into the hydrogen ion and the bicar- bonate ion ( see ...
Page 278
... acid and sulfuric acid in rain . These two acids are much stronger than carbonic acid . The strength of an acidic solution is measured on the pH scale from 0 to 14 ( box figure 2 ) . A solution of pH 7 is chem- ically neutral , neither ...
... acid and sulfuric acid in rain . These two acids are much stronger than carbonic acid . The strength of an acidic solution is measured on the pH scale from 0 to 14 ( box figure 2 ) . A solution of pH 7 is chem- ically neutral , neither ...
Page 286
... acid in solution . Which one is most important for chemical weathering ? What is the difference between a residual ... acid H2CO3 ( b ) water H2O ( c ) carbon dioxide CO2 ( d ) hydrochloric acid HCl 16. The most common end product of the ...
... acid in solution . Which one is most important for chemical weathering ? What is the difference between a residual ... acid H2CO3 ( b ) water H2O ( c ) carbon dioxide CO2 ( d ) hydrochloric acid HCl 16. The most common end product of 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