17 Recharge and Flow 4

17 Recharge and Flow 4 - Much of the Recharge Occurs at...

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Maintenance of hydrologic connection with the underlying limestone is primary source of recharge to the Floridan Lakes and Aquifer Recharge
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Elevation, Recharge, and Groundwater Movement Subsidence lakes and sinks are a primary source of recharge to the Floridan Aquifer
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Elevation (m) Recharge Areas
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Unformatted text preview: Much of the Recharge Occurs at Higher Elevations Groundwater flows from topographic highs toward lower elevations Recharge Generalized Groundwater Movement and Artesian Conditions confining confining Artesian Aquifer Water under pressure Central part Of state...
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This note was uploaded on 02/17/2011 for the course SWS 2007 taught by Professor bonczek during the Fall '09 term at University of Florida.

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17 Recharge and Flow 4 - Much of the Recharge Occurs at...

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