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Introduction to Groundwater, Karst and the Edwards Aquifer Water color by Kathy Rottier
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Groundwater Zones
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Alternate image of groundwater zones
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Porosity
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Permeability
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Types of groundwater flow
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Aquifer Recharge and Discharge
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Groundwater flow timescales
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Artesian groundwater systems
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Water: the great dissolver and precipitator Dissolves:Precipitates: Limestone, gypsum, salt (makes caves and landscapes these rocks) Cave deposits (stalactites, travertine, etc) Cements that hold sedimentary rocks together (calcareous, siliceous, and ferruginous) Few minerals from sandstones, shales, and igneous and metamorphic rocks (does not make caves in these rocks) Spring and geyser deposits Concretions and geodes
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Limestone Dissolution H 2 O + CO 2 = H 2 CO 3 water + carbon dioxide = carbonic acid H 2 CO3 + CaCO 3 = Ca ++ + 2 HCO 3 - carbonic acid + calcium carbonate (limestone) = calcium ions + bicarbonate ions
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Karst Development: Initial Stage
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Karst Development: Intermediate Stage
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Karst Development: Late Stage
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Karst Terrain Mike Warton
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Geologic History of the Edwards Aquifer
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Uplifting and Earthquakes
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The Edwards Aquifer
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Barton Springs Segment (map view)
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Barton Springs Segment (cross-section view)
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Inner Space Caverns Photos by Marsha Willis
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Longhorn Caverns ’Photos by Larry Jayroe
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Photo Credit: City of Austin <http://www.ci.austin.tx.us/watershed/images/ bartonaerial.jpg>,accessed September 22, 2008
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Barton Springs Pool
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Example Hydrograph
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Discharge at Barton Springs January 1980 – September 2008 Source: USGS,accessed September 19, 2008
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Source: http://media.point2.com/p2a/htmltext/d51f/3a57/e5a5/4d13a91f bcd071034cf8/original.jpg, accessed September 22, 2008 The End
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