Groundwater And Groundwater Law in Massachusetts

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collapsed, or eroded glacio fluvial deposits, most well-stratified sand and gravelwithsomesilt.
Till— boulders, gravel, sand.
silt, clay, nonsorted to poorly sorted Water-land contact . ^ Stream {geology modified from mapping by G. W. Holmes.
Open-File ReportU.S. Geological Survey) Location of high ground-water yielding deposits of stratifed drift in the Lenox-Lee area 51 2) HousatonJc Valley between Lenox and Lee(Motts, 1972, p. 39) An extensive groundwater aquifer has been identified in an ar
...ea which is underconsiderationasa landfill site.
A broad band of sand and gravel of ice-contact origin extends along the Housatonic Valley between Lenox and Lee. The deposits (Fig. 4-5, 6) are generally highly permeable and contain very large amounts of excellent quality water. The extreme northern partof the deposits by itself has a potential of about 6 mgd, more than enough water to satisfy all local communities and industry well beyond the year 2000.
Because of their proximity to Lenoxand Lee, and because much of the surrounding area is underlain by bedrock and till, the sand and gravel ice-contact deposits have been chosen as landfill sites by Lenox, Lee and local industries.


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