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Barnett Hydrology Hangman

 
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Question Answer
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