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Shenandoah National ParkRed maple in full fall color.
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Shenandoah National Park
Groundwater
Groundwater Model

(UK Groundwater Forum)

Groundwater Model

Two significant publications (DeKay 1972, Plummer et al 2001), fully cited below, provide both general descriptions of groundwater conditions throughout the park as well as specific conditions in the Big Meadows area. Groundwater withdrawal and condition are of particular interest because of relationships between high elevation ridge tops that tend to receive more moisture but that do not accumulate the water, presence of visitor use facilities along the crest of the ridge with associated high demand for potable water and withdrawal problems, and potential exposure to pollutants.

Related Information

Useful references specific to Shenandoah National Park groundwater are:

DeKay, R.H. 1972. Development of ground-water supplies in Shenandoah National Park, Virginia. Mineral Resources Report 10. Virginia Division of Mineral Resources. 158pp.

Plummer, L.N., E. Busenburg, J.K. Bohlke, D.L. Nelms, R.L. Michel, and P. Schlosser. 2001. Ground water residence times in Shenandoah National Park, Blue Ridge Mountain, Virginia, USA, A multi-tracer approach. Chemical Geology, v. 179/1-4, pp. 93-111.

The early post card view of the Marys Rock Tunnel is typical of the iconic use of images of the engineering structure  

Did You Know?
The 600' long Marys Rock Tunnel was completed in 1932 and the public considered it a scenic wonder. It became iconic and tunnel images were used on everything from post cards to jewelry.

Last Updated: July 25, 2006 at 00:31 EST