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Groundwater is defined as water that is found beneath the water table under Earth’s surface.
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Groundwater Freshwater storehouse
98 percent of all the usable fresh water on the planet 60 times as plentiful as fresh water found in lakes and streams valuable resource
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travels through pores in soil and rock, in fractures, and through weathered areas of bedrock.
Movement
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Vocabulary Porosity: amount of pore space present in rock and soil
Permeability: ability of fluids to travel through the rock or soil . A “high” permeability and porosity value means that the water can travel very quickly
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Aquifer Body of water-saturated sediment or rock in which water can move readily unconfined aquifer is exposed to the surface of the land confined aquifer is an aquifer that has a confining layer that separates it from the land surface.
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If the water is pressurized at a high enough value, when a well is drilled into the confining aquifer, water rises above the land surface. This is known as a flowing artesian water well.
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Sinkhole
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Recharge and Drawdown Porosity and permeability affects the recharge rate of the groundwater. Drawdown: lowering of the aquifer near a pumping well. creates voids in the bedrock Sinkholes (cannot hold the weight of the material above and collapses)
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Sources http://education.nationalgeographic.org/encyclopedia/aquifer/
Birchall, Gary and John McCutcheon. Planet Earth: A Physical Geography. Ontario: John Wiley and Sons Print
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