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Earth Science-- Water Moving Underground

AB
HYDROSPHEREwater of Earth's surface
UNDERGROUNDwhere most useable fresh water is located
EVAPORATIONwater vapor going into the atmosphere, usually by the sun's heat
CONDENSATIONwater gas changing into water liquid
PRECIPITATIONgravity pulling water from clouds
TRANSPIRATIONprocess by which green plants lose water
CAPILLARY WATERfringe water between pore space in Earth Materials
WATER BUDGETthe balance sheet for rain and water usage
SURPLUSmore water than you need
USAGEless water than you need, but storage not empty
DEFICITprecipitation less than needed, storage IS empty
RECHARGErain is greater than needed, storage is not full
GREATEST PORE SPACEparticles round and same size
LEAST PORE SPACEwhen particles are angular and assorted size
POROSITYindicates volume of open space
PERMEABILITYthe ability of the rock to transmit water
SATURATIONall pore spaces are filled with water
CAPILLARY ACTIONmovement of water up due to closeness of particles
ARTESIAN WELLwater under pressure comes from an aquifer under an impermeable layer; no pumping needed
AQUIFERpermeable layer which is saturated with water
FISSUREcracks in rocks that allow water to reach the surface; oasis
PAINT POTmud volcanoes; hot water moves through clay
GEYSERSgushes of hot water & steam that erupt through water tube with constrictions
FUMEROLESholes in ground from which hot gas escapes
HARD WATERwater containing minerals Ca, Mg, and/ or Fe
KARST TOPOGRAPHYunusual topography; lost rivers, sink holes, underground rivers
STALACTITEScalcite deposits on ceilings, formed from dripping
STALAGMITESbelow stalactites, round mass on ground
COLUMN (PILLAR)when stalactites & stalagmites meet

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