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Chapter 10 - Ground Water

AB
infiltrationprecipitation that falls on the land and enters the ground, thus becoming groundwater
porositythe percentage of pore space in any material
zone of saturationthe surface at which groudwater completly fills all the pores of a material
water tablethe upper boundry of the zone of saturation
permeabilitythe ability to allow water to pass through a material
aquifergroundwater flow that takes place through permeable layers
cavea natural underground opening with a connection to Earth's surface
karst topographythis shows some of the characteristic surface features produced by dissolution of limestone
sinkholea depression in the ground that has been caused by the collapse of a cave or by the direct dissolution of bedrock by acid rain or moist soil
stalactitecone-shaped or cylindrical forms, made-up from natural deposits that form and hang from a cave's ceiling like icicles
stalagmitemound shaped dripstone deposits that are a result from minerals dripping from stalactites
travertinedripsotne formations that are composed of a certain type of limestone
atresian wellfountain of water that spurts above the land surface when a well taps a deep, confined aquifer containing water under pressure
drawdownthe difference between the original water-table level and the water level in a pumped well
geyserexplosive hot springs that erupt at regular intervals
hot springa spring that discharges warm/hot water
rechargea process in which water from precipitation and run-off is added back to the zone of saturation
springnatrual discharges of groundwater
wella hole dug or drilled deep into the ground to reach a reservoir of groundwater


Mrs. Bolin

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