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ES Chapter 06 Vocabulary Review

Running Water & Groundwater
Prentice Hall Earth Science

AB
aquiferrock or soil through which groundwater moves easily
artesian wella well in which the water naturally rises above the level of the water table
bed loadsediment that is carried by a stream along the bottom of its channel
capacitythe total amount of sediment a stream is able to transport
caverna naturally formed underground chamber or series of chambers most commonly produced by solution activity in limestone
deltaan accumulation of sediment formed where a stream enters a lake or an ocean
dischargethe quantity of water in a stream that passes a given point in a period of time
dividean imaginary line that separates the drainage of two streams; often found along a ridge
drainage basinthe land area that contributes water to a stream
floodoccurs when the discharge of a stream becomes so great that it exceeds the carrying capacity of its channel and overflows its banks
floodplainthe flat, low-lying portion of a stream valley subject to periodic flooding
geysera hot spring or fountain that ejects water at various intervals
gradientthe slope of a stream over a certain distance
groundwaterwater underground in the zone of saturation
infiltrationthe movement of surface water into rock or soil through cracks and pore spaces
karst topographyan area that has a land surface or topography with numerous depressions called sinkholes
meandera looplike bend in the course of a stream
natural leveean elevated landform that parallels a stream and acts to confine its waters, except during floodstage
permeabilitya measure of a material’s ability to transmit fluids
porositythe volume of open spaces in rock or soil
sinkholea depression produced in a region where soluble rock has been removed by groundwater
springa flow of groundwater that emerges naturally at the ground surface
stream channelthe course that the water in a stream follows
travertinea form of limestone that is deposited by hot springs or as a cave deposit
tributarya stream that empties itself into another stream
water cyclethe constant movement of water among the oceans, the atmosphere, geosphere, and the biosphere
water tablethe upper level of the saturated zone of groundwater
wellan opening bored into the zone of saturation
zone of saturationzone where all open spaces in sediment and rock are completely filled with water
rejuvinationa change in the base level of a stream, often caused by regional uplift
stalactitean icicle-like structure that hangs from the ceiling of a cavern
stalagmitea columnlike form that grows upward from the floor of a cavern


Chemistry & Physics
Lumberton High School
Lumberton, NC

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