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Layer: Elevation of the Base of the Combined Chase, Council Grove, and Admire Groups (ft) (2)

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Description: The structure-contour map of the altitude of the base of the combined Chase, Council Grove, and Admire Groups was created from the correlation of geologic logs across the study area. The Chase, Council Grove, and Admire Groups are composed of cross-bedded, fine-grained sandstone, shale, and thin limestone. The three groups are stratigraphically below the Wellington Formation. The thickness of these groups range from 570 to 940 feet with a median of 745 feet.

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Copyright Text: Modified by the OWRB from the 2013 USGS publication Hydrogeology and simulation of groundwater flow in the Central Oklahoma (Garber-Wellington) aquifer, Oklahoma, 1987 to 2009, and simulation of available water in storage, 2010-2059. Scientific Investigation Report 2013 - 5219. Authors: Shana L. Mashburn, Derek Ryter, Christopher R. Neel, S. Jerrod Smith, and Jessica S. Magers

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Layer: Elevation of the Base of the Wellington Formation (ft) (3)

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Description: The structure-contour map of the altitude in feet of the base of the Wellignton Formation was created from the correlation of geologic logs across the study area. The Wellington Formation consists of cross-bedded, fine-grained sandstone with interbedded shale or mudstone. Datum is National Geodetic Vertical Datum of 1929.

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Copyright Text: Modified by the OWRB from the 2013 USGS publication Hydrogeology and simulation of groundwater flow in the Central Oklahoma (Garber-Wellington) aquifer, Oklahoma, 1987 to 2009, and simulation of available water in storage, 2010-2059. Scientific Investigation Report 2013 - 5219. Authors: Shana L. Mashburn, Derek Ryter, Christopher R. Neel, S. Jerrod Smith, and Jessica S. Magers

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Layer: Elevation of the Base of the Hennessey Formation (ft) (4)

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Description: The structure-contour map of the altitude of the base of the Hennessey Group was created from the correlation of geologic logs across the study area and was originally published in Christenson and others (1992). The Permian-age Hennessey Group overlies the western part of the Central Oklahoma aquifer and consists of interbedded red shale, clay, and some siltstone or fine-grained sandstone. The Hennessey Group is composed of the Bison Formation, Salt Plain Formation, Kingman Formation, and the Fairmont Shale. Although not considered part of the Central Oklahoma aquifer, the Hennessey Group outcrops in the western one-third of teh aquifer area and acts as a confining layer. Total Thickness of the Hennessey Group ranges from 600 to 650 feet.

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Copyright Text: Modified by the OWRB from the 2013 USGS publication Hydrogeology and simulation of groundwater flow in the Central Oklahoma (Garber-Wellington) aquifer, Oklahoma, 1987 to 2009, and simulation of available water in storage, 2010-2059. Scientific Investigation Report 2013 - 5219. Authors: Shana L. Mashburn, Derek Ryter, Christopher R. Neel, S. Jerrod Smith, and Jessica S. Magers

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Layer: Elevation of the Base of Fresh Groundwater (ft) (5)

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Description: The structure-contour map of the altitude of the base of fresh groundwater constructed by Christenson and others (1992) using geophysical logs. The base of freshwater-elevation contours were used to determine the base of the aquifer and was defined at 5,000 mg/L dissolved solids.

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Copyright Text: Modified by the OWRB from the 2013 USGS publication Hydrogeology and simulation of groundwater flow in the Central Oklahoma (Garber-Wellington) aquifer, Oklahoma, 1987 to 2009, and simulation of available water in storage, 2010-2059. Scientific Investigation Report 2013 - 5219. Authors: Shana L. Mashburn, Derek Ryter, Christopher R. Neel, S. Jerrod Smith, and Jessica S. Magers

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Layer: Potentiometric Surface Contours (ft), 1986-1987 (6)

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Description: The 1986-1987 potentiometric surface map was compiled in Christenson and others (1992) and Parkhurst and others (1996). Water levels were measured in more than 300 wells between December 22, 1986 and April 24, 1987.

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Copyright Text: Modified by the OWRB from the 2013 USGS publication Hydrogeology and simulation of groundwater flow in the Central Oklahoma (Garber-Wellington) aquifer, Oklahoma, 1987 to 2009, and simulation of available water in storage, 2010-2059. Scientific Investigation Report 2013 - 5219. Authors: Shana L. Mashburn, Derek Ryter, Christopher R. Neel, S. Jerrod Smith, and Jessica S. Magers

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Layer: Potentiometric Surface Contours (ft), 2009 (7)

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Description: Water levels were measured in 280 wells between February 17, 2009 and March 13, 2009 by the United States Geological Survey as part of their investigation of the Central Oklahoma (Garber-Wellington) aquifer and was originally published in Mashburn and Magers (2011).

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Copyright Text: Modified by the OWRB from the 2013 USGS publication Hydrogeology and simulation of groundwater flow in the Central Oklahoma (Garber-Wellington) aquifer, Oklahoma, 1987 to 2009, and simulation of available water in storage, 2010-2059. Scientific Investigation Report 2013 - 5219. Authors: Shana L. Mashburn, Derek Ryter, Christopher R. Neel, S. Jerrod Smith, and Jessica S. Magers

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Layer: Saturated Thickness (ft), 2009 (8)

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Description: This map was created as part of the USGS hydrogeologic investigation of the Central Oklahoma (Garber-Wellington) aquifer. The saturated thickness ranges from 200-330 feet in the eastern region of the aquifer near Lincoln and Pottawatomie Counties to about 920 feet near 35 degrees, 25 minutes latitude and 97 degrees, 25 minutes longitude, near Tinker Air Force Base.

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Copyright Text: Modified by the OWRB from the 2013 USGS publication Hydrogeology and simulation of groundwater flow in the Central Oklahoma (Garber-Wellington) Aquifer, Oklahoma, 1987 to 2009, and simulation of available water in storage, 2010-2059. Scientific Investigation Report 2013 - 5219. Authors: Shana L. Mashburn, Derek Ryter, Christopher R. Neel, S. Jerrod Smith, and Jessica S. Magers

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Layer: Mean Recharge, Inches per Day, 1887-2009 (9)

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Description: The map was created as part of the USGS hydrogeologic investigation of the Central Oklahoma (Garber-Wellington) aquifer using climate, soil, and land-use data. The spatially distributed recharge estimates were calculated using the SWB code developed by Westenbroek and others (2010).

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Copyright Text: Modified by the OWRB from the 2013 USGS publication Hydrogeology and simulation of groundwater flow in the Central Oklahoma (Garber-Wellington) aquifer, Oklahoma, 1987 to 2009, and simulation of available water in storage, 2010-2059. Scientific Investigation Report 2013 - 5219. Authors: Shana L. Mashburn, Derek Ryter, Christopher R. Neel, S. Jerrod Smith, and Jessica S. Magers

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XMax: -65125.224630162265
YMax: 1442433.2817574143
Spatial Reference: 102039  (102039)



Drawing Info:
N/A
Advanced Query Capabilities:
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Supports OrderBy: false
Supports Distinct: false
Supports Pagination: false
Supports TrueCurve: false
Supports Returning Query Extent: true
Supports Query With Distance: true
Supports Sql Expression: false
Supports Query With ResultType: false
Supports Returning Geometry Centroid: false


HasZ: false

HasM: false

Has Attachments: false

HTML Popup Type: esriServerHTMLPopupTypeNone

Type ID Field: null

Fields: None