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GEOLOGY INDEX
STUDY QUESTIONS
WEATHERING

When rocks, especially igneous and metamorphic rocks are exposed at the surface, either during eruptions or as a result of erosion, the combinations of minerals which were stable under higher temperatures and pressures are no longer in their original environment of formation. As they are exposed to the highly reactive chemicals of the atmosphere and the surface environment, they begin to change both physically and chemically into new combinations, which are now stable in this new, low temperature, low pressure, surface environment. 

The sum total of these   surface changes at the surface, including changes in size and chemistry, is referred to as weathering. Those processes which result in only a change in size are called physical or mechanical weathering, and those which result in new chemical combinations or minerals are called chemical weathering. 

Physical (Mechanical) weathering

Frost wedged rock at Kitt Peak AZ (jk97)
Physical weathering simply reduces the size of rocks. This takes place in two ways: either inorganically or by the action of living things. Virtually all rocks in the world have been cracked, either by forces which acted upon them when the rocks were still buried, or because of unloading, when the weight of overlying rocks has been removed by erosion and the rocks then expand and crack. Water which seeps into the ground fills these cracks. During cold spells, the water freezes and expands, placing great stress on the rocks, and they break. This process, called frost wedging, is most active in cold climates, at high altitudes or latitudes. Less commonly, growth of crystals in cracks can also cause rocks to break up. 
Living things also cause considerable damage. Plants put out extensive networks of roots which penetrate cracks. As plant roots grow, they exerts pressure on the surrounding materials and split them. Clams and other marine organisms, drill holes into rocks. Finally, a visit to a strip mine, or a journey along an interstate cut into the mountains should be enough to convince anyone of the profound effects of human activity. 

The net effect of physical weathering is the reduction in size of the materials at the surface of the earth. Physical weathering has little effect on the makeup of the materials themselves. However, physical weathering promotes chemical weathering by increasing the surface area exposed to the action of various chemicals.