...FINAL EXAM STUDENT’S MANE: LORENZO NICOLAS MBA OBAMA PROFFESOR’S NAME: NINA WALKER SCI110 STRAYER UNIVERISTY March 19, 2014 1. There are two types of weathering. The first is mechanical weathering, the gradual breakdown of rock to sand, and then to silt, or powdered rock, and finally to clay through physical means. Mechanical weathering occurs in a variety of ways. For example, Heat and cold may cause minerals within a rock to expand and shrink at different rates, creating cracks. Water may seep into those cracks and freeze, expanding and splitting the rock. A raging river or ocean waves can smash rocks against each other, wearing the outsides smooth and turning rocks into sand. Or sand carried by the wind can act like sandpaper, slowly wearing rock away. A Glacier can rub debris against the rock beneath it, also acting like sandpaper. Even plants can force rocks to split as roots creep into cracks and grow. The second type of weathering is chemical Weathering, the breakup of rock caused by a change in its chemical makeup. Rain is the most common producer of chemicals that can weather rock. For example, Rain absorbs carbon dioxide and sulfur dioxide from the atmosphere, forming carbonic acid and sulfuric acid, two liquids capable of dissolving other materials. The levels of carbonic and sulfuric acids in rain, while generally weak, can over time dissolve rock such as limestone, freeing other types of rock. Over very long periods, rain can even dissolve enough limestone...
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