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E. S. Surface Water G, ch 4

AB
runoffwater that doesn't soak into the ground
rill erosionwater erosion due to runoff; create small channels
gully erosionwhen a rill channel becomes broader
sheet erosionrainwater flows over a gentle slope, maoves sediments from entire surface
drainage basinland area drained by a river syster
meandera curve in a mature stream
flood plainbroad valley floor carved by a meandering stream
alluvial fantriangular deposit of sediment that forms when water loses its energy
deltaa triangular deposit of sediment formed when a river slows and empties into an ocean
ground waterwater that soaks into the ground and collects in pores
permeablewater can pass through
impermeablewater can not pass through
aquiferlayer of permeable rock that transmits water freely
zone of saturationthe area where all of the pores in the rock are filled with water
water tableupper surface of the zone of saturation
artesian wella well in which water under pressure rises to the surface
springwater flows out of the water table and reaches the surface
hot springheated ground water comes to the surface
geysera hot spring that erupts periodically and shoots water and steam into the air
caveunderground opening formed by dissolved limestone rock
Young Streamflows swiftly through a steep valley, rapids and waterfalls
Mature Streamflows less swiftly, rocks eroded, meanders
Old Streamflows slowly through a flood plain that it made by erosion
River Systemcontains streams in all stages of development, like a tree
Longshore currenta source of shoreline erosion
beachdeposits of sediment that run parallel to the shore
barrier islandsand deposits that run parallel to the shore but are separated from the mainland
channela groove made by water running down the same path

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