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Chapter 10 vocab

TermDefinition
infiltration precipitation that has fallen on land trickles into the ground and becomes groundwater
zone of saturation groundwater completely fills all the pores of a material
water table upper boundary of the zone of saturation
zone of aeration above the water table, materials are moist, but they are not saturated with water, air occupies much of the pores
permeability tendency of a material to let water pass through
aquifer groundwater flows through permeable sediment and rock
spring natural discharge of groundwater
hot spring have a temperature higher than that of human body
geyser explosive hot springs
cave natural underground opening with a connection to Earth's surface
sinkhole depression in the ground caused by the collapse of a cave
karst topography regions that have sinkholes and disappearing streams
stalactite hang from the caves ceiling
stalagmite come up from the ground
well holes dug or drilled into the ground to reach an aquifer
drawdown difference between the original water table level and the water level in the pumped well
recharge water from precipitation replenishes the water content of an aquifer
artesian well aquifer can spurt above the land surface in the form of a fountian
aquicludes impermeable layers, barriers to groundwater
Created by: JakeMcGarity
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