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ES 09 JRW

TermDefinition
Porosity Amount of pore spaces
Water Table Upper boundary
Zone of Aeration Air in pores above
Permeability Ability of material to let water pass
Aquifers Permeable sediments with large pores.
Aquaicludes Barriers to groundwater flow
Geyser Explosive hot spring
Acidic water dissolves ___ in limestone Calcite
Stalactites/stalagmites form by Calcite precipitation
Ordinary Well Reaches below water table
Hot Springs naturally hot water, typically heated by subterranean volcanic activity.
Groundwater slightly acidic is caused by ______ Carbonic Acid
Overpumping Forms _____ Cone of depression
Precipitation must ______ level Recharge
Artesian Well Drilled into aquifer under pressure, it also spurts water like a fountain
Hard Water has high amounts of______. It can also clog pipes. Ca, Mg, Fe
Spring Natural discharge of groundwater; occurs where aquifer intersects surface; Temperature usually regional average.
Groundwater movement Flows downhill along slope of water table.
Zone of Saturation Groundwater completely fills pores.
Accumulation of Groundwater Water cycle leads to precipitation, precipitation infiltrates through soil pore spaces.
Created by: jwork
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