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<br /> <br /> <br />12 <br /> <br />Erosion/ <br /> <br /> <br />ition <br /> <br />EROS ION I s the remova I and s I mu I taneous transportat I on of <br />earth materials from one location to another by water, wind, <br />waves. or moving Ice. DEPOSITION Is the placing of the <br />eroded material In a new location. All material which. is <br />eroded Is later deposited in another location. <br /> <br />Characteristics <br /> <br />Erosion and deposition are occurring continually at varying <br />rates over the earth's surface. Swiftly moving flood waters <br />cause rapid local erosion as the water carries away earth <br />materials. Deposition occurs where flood waters slow down, <br />pool or lose energy in other ways and the materials settle <br />out. Simi larly, wind erosion can occur from exposed areas <br />such as fields, tailings and desert areas when the wind is <br />strong and the materials are deposited when the wind <br />diminishes. Another factor which controls the amount of <br />erosion is the ease with which material can be dislodged. <br />Hard granites erode very slowly while soft slits and sands <br />erode very quickly. Vegetation which holds soils In place <br />can decrease significantly the rates of erosion from water <br />and wind. <br /> <br />Consequences <br /> <br />Erosion can result in minor inconveniences or total <br />destruction. Severe erosion removes the earth from beneath <br />bridges, roads, and foundations of structures adjacent to <br />streams. By undercutting It can lead to Increased rockfal I <br />and landsl Ide hazard. The deposition of material can block <br />culverts, aggravate flooding, destroy crops and lawns by <br />burying them, and reduce the capacity of water reservoirs as <br />the deposited materials displace water. <br /> <br />Severe erosion from man-made alterations of the <br />dra i nage systems resu I ted in a large gu I I Y I n Doug I as <br />Note man standing In the center of the picture. <br /> <br />natural <br />County. <br />