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Contours of Corcoran Clay Depth in feet from Page (1986) for the Central Valley Hydrologic Model (CVHM)
Summary
- Type of release
- ongoing release of a series of related datasets
- Data Licence
- Not Applicable
- Content Licence
- Creative Commons CCZero
- Verification
- automatically awarded
- Release Date
- 15 March 2013
- Modified Date
- 17 November 2014
- Update Frequency
- notPlanned
- Publishers
- U.S. Geological Survey, Department of the Interior
- Identifier
- contours-of-corcoran-clay-depth-in-feet-from-page-1986-for-the-central-valley-hydrologic-model-
- Landing Page
- http://catalog.data.gov/dataset/contours-of-corcoran-clay-depth-in-feet-from-page-1986-for-the-central-valley-hydrologic-model-
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Description
This digital dataset defines the depth of the Corcoran Clay Member of the Tulare Formation. The complex hydrologic system of the Central Valley is simulated using the USGS numerical modeling code MODFLOW-FMP (Schmid and others, 2006b). This simulation is referred to here as the Central Valley Hydrologic Model (CVHM) (Faunt, 2009). Utilizing MODFLOW-FMP, the CVHM simulates groundwater and surface-water flow, irrigated agriculture, land subsidence, and other key processes in the Central Valley on a monthly basis from 1961-2003. Numerous lenses of fine-grained sediments are distributed throughout the southern Central Valley (San Joaquin Valley) and generally constitute more than 50 percent of the total thickness of the valley fill. Generally, these lenses are discontinuous and not vertically extensive or laterally continuous. However, the Corcoran Clay is a low-permeability, areally extensive, lacustrine deposit (Johnson and others, 1968) as much as 200-ft thick (Davis and others, 1959; Page, 1986). This continuous clay divides the groundwater-flow system of the western San Joaquin Valley into an upper semi-confined zone and a lower confined zone (Williamson and others, 1989; Belitz and Heimes, 1990; Burow and others, 2004). The extent and distribution of the Corcoran Clay was defined for use in the CVHM because the unit is one of the few deposits in the Valley that can be regionally mapped. The CVHM is the most recent regional-scale model of the Central Valley developed by the U.S. Geological Survey (USGS). The CVHM was developed as part of the USGS Groundwater Resources Program (see "Foreword", Chapter A, page iii, for details).
General Information
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This data is described at
http://catalog.data.gov/dataset/contours-of-corcoran-clay-depth-in-feet-from-page-1986-for-the-central-valley-hydrologic-model- Do you think this data is incorrect? Let us know
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This data is published by
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Legal Information
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The rights statement is at
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Outside the US, this data is available under
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There are
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The content is available under
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This data contains
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The data appears in this collection
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This data changes
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