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Groundwater
West Virginia regulates
ground water in its Groundwater Protection Act [W.
Va. Code ch. 12, art. 12]. Groundwater is water located
beneath the earth's surface in the deeper saturated zone
where only water surrounds soil particles and fills cracks.
The more shallow zone underneath the surface is known as
the unsaturated zone and contains both air and water in
spaces between soil particles. Groundwater accumulates
in aquifers and the shallowest aquifer is the water table.
Standards are promulgated
by the Environmental Quality Board and the DEP is "designated
to be the lead agency for groundwater." The DEP Director
oversees and coordinates implementation of the act by each
regulatory agency through a certification program. Applications
for certifications are required of governmental bodies whose
actions (permits, activities, etc.) "may affect groundwater
quality." Civil and criminal penalties are contained
in the act.
Hole-ly ground. An
intriguing aspect of groundwater is its ability to make
caves and caverns.
West Virginia has over 400 known underground caverns, mostly
located in the eastern counties. Many caverns occur
in broad bands of Mississippian limestone near the surface
starting in Tucker County and extending southwestwardly
to Greenbrier and Monroe Counties.
Caverns form along cracks
in soluble rock, such as limestone, as groundwater containing
carbonic acid, picked up from decaying vegetation, slowly
enlarges the cracks. Since cracks crosscross each
other, passageways are formed. In time a natural fairyland
is created and dripping water creates stalactites and stalagmites.
As caverns enlarge, groundwater moves more freely and faster
through openings and the water table drops. Underground
streams are common in caverns and may hide from view by
us surface dwellers to emerge at another location.
Lost River in Hardy County is an example. Where caverns
are close to the surface of land, depressions, called sinks,
may form.
VOCs. In December 1999 the
U. S. Geological Survey released a study showing the presence
of harmful volatile organic compounds in groundwater nationally,
in both rural and urban areas. The most detected VOC
was chloroform and the second VOC was MTBE, a gasoline additive.
Last updated on Tuesday, July 25, 2000
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