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The constant circulation of water amoug the se, the atmospherem and the land
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water that flows back to the oceans in surface streams
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water contained in soil and bedrock. all surface water
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direct evaporation from the leaf surfaces of plants
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a moving body of water confined in a channel and flowing downslope
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any stream that contributes water to another stream
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the verticle drop of a stream over a specific distance
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the volume of water flowing downstream per unit time. It is measured in unitit of cubic meters per second (m3/ sec)
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channel characteristics refer to the shape and roughness of a stream channel
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the floor of a stream channel
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the rising slope bordering the side of a stream channel
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a measure of the largest particles that a stream can transport
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the maximum quantity of sediment that a stream can carry
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the portion of a stream's sediment load that is carried in solution
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the portion of a stream's load that is carried for a considerable time in suspension, free from contact with the streambed
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the portion of a stream's load that is transported on or immediately above the streambed
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downward erosion by a stream
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the deepest level to which a sream can erode its bed. the ultimate base level is usually sea level, but this is seldom attained
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a stream with a smooth, concave profile. A graded stream is in equilibrium with its sediment supply; it transports all the sediment supplied to it with neither erosion nor deposition in the streambed
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the action of a stream as it cuts into and erodes its banks.
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one of a series of sinuous curves or loops in the course of a stream
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a stream deposit located on the inside of a growing meander
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a cresent-shaped lake formed whre a meander is cut off from a stream and the ends of the cut-off meander become plugged with sediment
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a stream that divides into a network of branching and reuniting shallow channels separated by midchannel bars
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the region that is ultimately drained by a single river
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a fan-like accumulation of sediment created where a steep streamslows down rapidly as it reaches a relatively flat valley floor
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the nearly flat, alluvial, fan-shaped tract of land at the mouth of a steam
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a channel that flows outward from the main stream channel, such as is commonly found in deltas
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