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Appraisal of the Northern Shenandoah Valley
Carbonate Aquifer System,
Frederick County, Virginia

The carbonate aquifer system of the Northern Shenandoah Valley provides an important water supply to local communities. This is an area with an expanding economy and a growing population, and this aquifer is likely to be further developed to meet future water needs. An improved understanding of this complex aquifer system is required to effectively develop and manage it as a sustainable water supply. Hydrogeologic information provided by a detailed aquifer appraisal will provide useful information to better Location  mapaddress questions about (1) the quantity of water available for use, (2) the effects of increased pumpage on ground-water levels and instream flows, (3) the relation between karst features and the hydrology and geochemistry of the surface- and ground-water flow systems, and (4) the quality of the ground-water supply and its vulnerability to current and potential future sources of contamination. The area being considered in this study encompasses the carbonate formations in Frederick County, Virginia bounded on the east by the Martinsburg Formation, and on the west by Little North Mountain.

OBJECTIVE

The objective of this study is to better characterize the carbonate aquifer system in the Northern Shenandoah Valley and provide relevant hydrogeologic information that can be used to guide the development and management of this important water resource.

APPROACH

This study will be carried out as four major work elements to include (1) Hydrogeologic Framework, (2) Ground-Water Flow System, (3) Water Balance, and (4) Water Quality. The study will be completed in three and one-half years beginning in October 2000.  During Federal FY 2001 field reconnaissance was conducted, and existing geologic, hydrologic, and associated information was collected, organized, and evaluated. Limited field data-collection activities began and will be expanded in FY 2002 and 2003. Data analyses will be completed in 2003, and a final report will be produced in FY 2004. Continued monitoring and further investigation of specific water management issues will likely be carried out thereafter.

Activities proposed for Fiscal Year 2002 are as follows:

Hydrogeologic Framework

  • Establish a subdivision of major formations, with descriptions of folds, faults, and prominent jointing (to be conducted in cooperation with Randall Orndorff of the USGS Geologic Division).

  • Continue to field locate sinkholes and springs with GPS, enter into a geospatial database, and describe their position and relation to geologic and hydrologic features (to be conducted in cooperation with Randall Orndorff of the USGS Geologic Division).

  • Establish a preliminary hydrogeologic framework for the study area (revise and finalize in 2003).

Ground-Water Flow System

  • Continue well inventory and evaluation of completion reports, water-level measurements, and well yield information.

  • Continue operation of water-level monitoring network, conducting water-level measurements during high and low water conditions to provide information for a generalized water-table map (evaluate and revise water-level network in 2002 to produce a more detailed water-table map in 2003).

Water Balance

  • Identify sources of existing information and evaluate appropriate methods for measuring or estimating components of the water balance.

  • Collect and evaluate appropriate data and identify additional data needs.

  • Conduct field reconnaissance to identify locations for spring discharge and stream seepage measurements (to be done in 2002).

Stream Gaging

  • Continue operation of stream gages on Cedar Creek and Opequon Creek. Discharge data will be archived and published in the USGS annual data report.

RELEVANCE AND BENEFITS

Work on this project will contribute to the knowledge of water resources in the carbonate aquifers of Frederick County and the northern Shenandoah Valley of Virginia. The study will set the framework for further investigation of fundamental processes controlling the occurrence and movement of water in the carbonate aquifer system. Over the long term, information from this study will be incorporated with current and past investigations in neighboring states to increase our knowledge of the hydrogeologic controls on ground-water flow in the karst terrain of the Middle Atlantic States.

 

For information contact:
George E. Harlow, Jr.
804-261-2631
geharlow@usgs.gov
David L. Nelms
804-261-2630
dlnelms@usgs.gov

Contact: GS-W-VArmd_webmaster@usgs.gov
U.S. Department of Interior, U.S. Geological Survey
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January 26, 2007 09:45