Seaside Water Trail
Ground Water Committee
At times, it may feel like our ground water resource is infinite but it is not. What we do can harm or help our resource. We are dependent on clean and abundant water.

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We have opportunities to affect our ground water in a positive or negative way. Wise use and management of our water will provide for our needs but overuse and unwise use of our water can lead to very negative consequences for our water system.

General Threats to Our Ground Water

  • Saltwater Intrusion
  • Lowered Ground Water Level
  • Contamination

Saltwater Intrusion
Intrusion of saltwater into fresh ground water aquifers can be caused by:

1) wells that tap water too close to saltwater
2) wells too close to the shore
3) wells that pump at an excessive rate
4) or some combination of the above

Due to the characteristics of the Yorktown-Eastover Aquifer system, saltwater intrusion is more of a concern in these aquifers than the Columbia Aquifer.

Lowered Ground Water Level
All wells cause some loss of ground water level around them. This area is called the cone of depression. If pumping rates are too high or wells are too close together, ground water level can drop so low that the water that comes from the well is reduced. In extreme cases, the water level can fall so low that the material around the well can be dewatered. Without water to hold the pores in this material apart, pores will compact and a permanent loss of water results. This will in turn affect the well and how much water it can yield.

The major source of fresh water on the Eastern Shore is the Yorktown-Eastover Aquifers and since more industrial, municipal and private systems use this water these aquifers have more potential to be damaged by lowered ground water levels.

Preliminary Results of the Eastern Shore of Virginia Ground Water Model showing change in water levels in the Upper Yorktown-Eastover Aquifer over the last 80 years.

Contamination
The Columbia Aquifer is the most at risk for contamination. The Columbia is the water table aquifer and is generally found within 20 feet of the surface in the middle of the Shore and less than 6 feet near the edges of the Shore. Much of the earth in this aquifer is sand which allows water and contaminants to rapidly soak into the ground. Some private residences use this aquifer for drinking water but this aquifer is highly vulnerable to contamination. Major potential sources of ground water contamination on the Eastern Shore include fertilizer, pesticides, petroleum (gasoline, diesel, and oil), and wastewater from improperly constructed or maintained septic systems.

Hot Links:

Eastern Shore of Virginia Groundwater Committee
Accomack-Northampton Planning District Commission
Phone 757-787-2936 or toll-free 866-787-3001
Fax 757-787-4221
email anpdc@a-npdc.org
23372 Front Street, PO Box 417, Accomac, VA, 23301