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Chap 13 Streams Rivers

AB
base levelriver cannot erode its bed deeper than the largest body of water it enters
bed loadheavier materials mover along he bottom of river
capacitymeasure of the total amount of sediment a stream can carry
competencea measure describing the maximum size of particles a stream can carry
deltafan shaped deposite formed as river opens into a quiet /larger body of water
depositionprocess by which materials fall to the bottom of stream/river
dischargeamount/volume of water passing a certain point in a given amount of time
divideland that separates on drainage basin from another
drainage basinall the land that drains into a river and its tributaries
flash floodsudden water rise due to heavy long rains rapid melt of winter snow
floodriver overflows its banks
flood plainpart of river valley flow hat is covered by flood water
gradientsteepness of the slope of a stream/river
headward erosionprocess by which land is worn away at the head of stream/gully
loaderoded rock and soil material transported down stream
meandersriver in flood plan tpically winds back and forth
natural leveesthick deposites that build u along the sides of a river
oxbow lakecurved body of water formed when deposites isolate a river meander
potholedeep oval/circular basin formed as materials in a whirl pool grind bedrock
river systema river and all its tributaries
stream piracyheadway erosion causes one river to wear through divide to capture another's head waters
suspensionwater has muddy appearance because of particles being carried
tributarystream that runs into another stream or river
watershedall the land that drains into a river and its tributaries


Science Instructor
Scarsdale, NY

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