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Layer: Karst Flow - KGS (1)

Name: Karst Flow - KGS

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Layer: KGS Karst Basins (2)

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Description: The information used to compile this GIS data was obtained by numerous investigators over the last 25 years. Major springs and the relative size of their catchment areas can be evaluated for potential as water supplies.

Service Item Id: 1f4c70a2881b4ab0adfe0cb29f83d1d1

Copyright Text: Kentucky Geological Survey, James C Currens and Randall L. Paylor, Water Section

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Layer: Royal Spring Aquifer - KGS August 2023 (3)

Name: Royal Spring Aquifer - KGS August 2023

Display Field: Name

Type: Feature Layer

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Description: http://kgs.uky.edu/kgsweb/download/rivers/karstdye.ZIPRoyal Spring Aquifer extracted and projected from KY Single Zone to KY North Zone.Created at a scale of 1:100,000. Should only be used for general guidance at larger scales.

Copyright Text: Kentucky Geological Survey Jim Currens, hydrogeologist 228 Mining and Mineral Resources Building Kentucky Geological Survey University of Kentucky Lexington KY 40506-0107 859-257-5500 currens@uky.edu Kentucky Geological Survey Doug Curl Head, Geoscience Information Manager 228 MMRB, University of Kentucky Lexington KY 40506-0107 859-323-0519 859-257-1147 doug@uky.edu

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Layer: Royal Spring Aquifer - KDOW 2010 (4)

Name: Royal Spring Aquifer - KDOW 2010

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Description: Field investigations and various modeling programs have been used to determine the wellhead protection areas throughout Kentucky. Systems using wells will have a WHPA-1, which represents a 400' minimum radius around the well or a 6-month time of travel for groundwater to the source. WHPA-2 generally represents a 10-year time of travel or the hydrologic boundary if there was not sufficient information to model the protection area. WHPA-3 will generally be the hydrologic boundary. Water suppliers using abandoned underground mine works will have the entire mined out area delineated as a WHPA-1. Systems that are using a spring or a well in karst areas will have the entire basin delineated as WHPA-1. This is due to the highly sensitive nature of the entire recharge area for these types of aquifers. Systems that use wells may have delineations that change if new wells are added or old wells are abandoned. Different modeling programs have been used to establish wellhead protection areas. These areas may change if a system decides to change the way they have modeled the aquifer being used.

Copyright Text: Kentucky Division of Water

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