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Access
a legend for the map below
Source
of Map: Water Resources Inventory of CT, Part 6, Upper Housatonic
River Basin, by the
U. S. Geological Survey and the CT Department of Environmental
Protection, 1972.
THIS IS AN EARLY (1972) GENERALIZED MAP OF ESTIMATED AQUIFER
BOUNDARIES
ONLY (YELLOW TAN COLOR IS DISCOLORATION ONLY. SHORT WOODS
BROOK
AQUIFER IS LARGEST OF THREE SEGMENTS, TO RIGHT )
COMPARE
IT TO LATER DATE USGS SURFICIAL MATERIALS MAP

EXCERPT
ON SHORT WOODS BROOK
AQUIFER FROM 1980 HVCEO STUDY
The largest of three small aquifers in New Fairfield, this
narrow and shallow site of 0.4 square miles lies along a brook
valley just north of the Town center. Except for a retail
business center and a small number of homes in the center,
the direct recharge area is entirely undeveloped, and mostly
wetland (zoned for two-acre residential).
Composition of this aquifer is favorable - coarse-grained;
although very close in location to the north end of Margerie
Reservoir, USGS maps do not show a hydraulic connection.

View
of Short Woods Brook Aquifer near
Shaws. Photo courtesy of Rick Gottschalk.
Basic
protection measures should focus on wetland preservation and
strict controls on sewage disposal. The nearby Town road salt
stockpile should also be relocated or controlled to prevent
groundwater contamination. By virtue of location, this small
aquifer could potentially provide a small central area water
supply source for the Town.
UPDATE
ON SHORT WOODS
BROOK AQUIFER AS OF 2004
The New Fairfield Municipal Water System
became operational in 2004 with three bedrock wells. The minimum
safe yield is about 14,000 gallons per day (gpd), but local
officials lowered it to 12,000 gpd. Current use for Town properties
and Shaw’s market is 3,000 - 4,000 gpd. Additional properties
along the water main may be allowed to tap into this system
in the future as conditions permit.
Maximum
theoretical yield with all 3 wells pumping continuously would
be about 115,000 gpd, although at that level the wells might
begin interfering with one another and the sanitary radii
would have to be increased.
While
there are known groundwater contamination problems in New
Fairfield Center that contribute to the need for new potable
supplies, local officials do not plan to take water from the
nearby Short Woods Brook stratified drift aquifer.
A key
reason is that this aquifer provides a hydraulic head that
pushes water into the bedrock fractures, and there is concern
that pumping large volumes of water from the stratified drift
aquifer might begin to pull pollutants northward from the
contaminated areas to the south.
The municipality
has given names to the two other nearby small aquifers to
the west. The first section is known as the Bigelow Aquifer
which runs south to north under a swampy area between Bigelow
Road and Route 37. Then the second segment, known as the Warwick
Aquifer, is configured west to east along Route 37 from Warwick
Road to Bigelow Road.
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