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Groundwater

AB
infiltrationthe process by which precipitation that falls on land enters the ground
porositythe percentage of pore space in a material
zone of saturationthe depth below Earth's surface at which groundwater completly fills all the pores of a material
water tablethe upper boundary of the zone of saturation
permeabilitythe ability of a material to let water pass through it
aquiferwhere most groundwater flows through permeable layers
cavea natural underground opening with a connenction to Earth's surface
sinkholea depression in the ground caused by the collapse of a cave or by the direct dissolution of bedrock by acidic rain or moist soil
karst topographylimestone regions that have sinkholes, sinks, and sinking streams
stalactitecone-shaped or cylindrical structures that hang from a cave's ceilings like isicles
stalagmitemound-shaped dripstone deposits underneath the stalactites
travertineanother type of dripstone formation that are composed of another type of limestone
springnatural discharge of groundwater
hot springa spring that discharges water that is much warmer than the average annual temperature
geyserexplosive hot springs that erupt at regular intervals
wellholes that are dug or drilled deep into the ground to reach a reservoir of groundwater
drawdownteh difference between the original water-table level and the water level in the pumped well
rechargethe water from precipitation and runoff that is added back to the zone of precipitation
artesian wella spring that discharges pressurized water


G. Gier

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