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use regulations should be enacted by Cumberland Township to protect the aquifer recharge<br />

area. (Portions of Cumberland Township are currently served by the Gettysburg Municipal<br />

Authority water supply and additional areas of the township may be served in the future.)<br />

Although the area is underlain by the "Gettysburg" Triassic sediment formation, good well<br />

locations should be found where rock fractures are indicated. In a recent study, five specific<br />

well locations were identified with the potential for supplying up to 0.5 mgd or more.'<br />

These well locations are illustrated in Figure 3.93.<br />

I<br />

1<br />

Other sources of information on water supplies in Adam County may be found in State<br />

p~blications.~~~<br />

Mid-County West and North - Gettysburg Plain: This broad area extends southwest to<br />

northeast across most of the county, including portions of Liberty and Freedom Townships<br />

to the southwest; Highland, Cumberland, and Franklin Townships to the west; and Butler,<br />

Tyrone, and Huntington Townships to the north of Gettysburg. The potential for obtaining<br />

adequate supplies of acceptable quality water throughout this "Gettysburg Plain" area<br />

underlain by the Gettysburg Triassic Formation should be similar to the potential near<br />

Gettysburg itself, as illustrated in Figure 3.9.3. The water yields from current wells range<br />

from 1 to 630 gallons per minute (gpm) with a median for residential wells of 12 gpm and<br />

for commercial wells of 69 gpm. The water is generally hard and may have iron and other<br />

constituents above recommended values<br />

Mid-County South and East - Bonneauville and the Route 15 Comcior area.- This extensive<br />

area LUIS from Mount Joy Township in the south, northeast through portions of Mt.<br />

Pleasant, Strabaa, Hamilton, and Reading Townships east of Gettysburg. Most of this area<br />

is underlain by Triassic sedimentaq rock, but a narrow Diabase formation with poor water<br />

yields runs diagonally across the county from southwest to northeast between Bonneauville<br />

and Gettysburg. The Borough of Bonneauville is served by 6 wells and is at or over its<br />

currently-available water supply capacity of about 0.1 mgd. Future growth in this area will<br />

require the search for fractures in the Triassic formation for additional wells with adequate<br />

yields and acceptable water quality.<br />

Eastern A dm County - Abbottstown, Easr Berlin, and New word area.- Abbottstown and<br />

East Berlin Municipal Water Authorities both appear to have adequate water supply<br />

capacity from their wells for substantial future growth. New Oxford, which obtains most of<br />

its water from the Conewago Creek (an average of about 0.57 mgd), is currently near its<br />

approved capacity, but has obtained a permit from DER to double withdrawals from the<br />

creek, from .65 mgd to 1.3 mgd. The "safe yield from the creek (Le., the amount of water<br />

that flows in the creek even during periods of drought) is 7.45 mgd, so even further<br />

withdrawals of water could be permitted. The growing areas around Cross Keys, Dicks<br />

Dam, and other contiguous or nearby locations in Oxford, Mt. Pleasant, Berwick, and<br />

Hamilton Townships could be served by extensions to the New Oxford Municipal Authority<br />

water supply lines.<br />

3-9-8

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