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Barnett - Hydrology

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karst topography   areas where landscapes have been shaped by the dissolving power of groundwater; area has sinkholes and caves  
limestone   a sedimentary rock that can be dissolved by groundwater to create caves  
carbonic acid   found in most natural water; this chemical dissolves limestone to form caverns  
cavern   naturally formed underground chamber  
stalactite   icicle-like stone pendants that hang from the ceiling of a cavern  
stalagmites   formations that develop on the floor of a cavern  
sinkhole   depression formed when limestone below the soil is dissolved  
artesian well   well in which the water naturally rises above the level of the water table  
aquifer   rock or soil through which groundwater moves easily  
zone of saturation   depth below earth's surface where groundwater completely fills all pore space  
zone of aeration   area below earth's surface where the soil is moist, but the pores are filled mostly with air  
water table   boundary between the zone of aeration and zone of saturation  
subsidence   when groundwater is pumped from a well faster than it is recharged, causing the water table to lower and land to sink  
spring   natural discharge of water where an aquifer and aquiclude meet  
aquiclude   impermeable layer under earth's surface  
permeable   ability to let water pass through  
geyser   explosive hot spring where water erupts from earth due to heating from igneous activity  
watershed   land area in which all water drains into a single river  
estuary   area where the mouth of a river opens into an ocean; mix of freshwater and salt water  
river delta   Triangular deposit of sediment where water empties into an ocean or lake  
alluvial fan   River water emptied from mountain valley onto an open ; deposits (drops) sediment in a fan shape  


   


 

 

 

 

 

 
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