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Aquifer Geology and Geography. Permeable materials such as sandstone, limestone and layers of sand and gravel. Recharge Zone. Ground surface where water enters an aquifer Dependent on permeability. Springs and Wells. Movement determined by the slope of the water table
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Aquifer Geology and Geography Permeable materials such as sandstone, limestone and layers of sand and gravel
Recharge Zone • Ground surface where water enters an aquifer • Dependent on permeability
Springs and Wells • Movement determined by the slope of the water table • If the water table reaches the Earth’s surface water will flow out of the ground (Spring) • Water table higher than the Earth’s surface lakes will form.
Artesian Well • Water flows from a crack in the cap rock of an aquifer. http://www.bartleby.com/images/A4images/A4artwel.jpg
Hot Springs • one form of an artesian well http://www.personal.engin.umich.edu/~yeq/images/YellowStone%201/Mammoth%20Hot%20Springs%201.jpg
Wells • A human made hole that is deeper than the level of the water table http://mainegov-images.informe.org/doc/nrimc/mgs/sites-1999/oct99-1.gif
Cave Formations • The underground erosion of limestone • Caused by carbonic acid
Deposition • Deposits of calcium carbonate
Stalactites • Stalactites-form from the ceiling http://www.goodearthgraphics.com/virtcave/staltite/stal1.jpg
Stalagmites • Stalagmites-form from dripping water http://www.dudleycc.pwp.blueyonder.co.uk/stalagmites.jpg
Dripstone Column http://science.nature.nps.gov/im/images/cavecol1.jpg
Sinkholes • When the water table is lower than the level of a cave • Results in the roof collapsing