1966
DOI: 10.3133/ofr6693
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Records of selected wells, springs, test holes, materials tests, and chemical analyses of water in the Houstatonic River basin, Massachusetts

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Cited by 6 publications
(6 citation statements)
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“…1). Surficial sediments are glacially derived sand and gravel deposits (Norvitch and Lamb, 1966), and overlie Cambrian-Ordivician-age Berkshire schist (Dale, 1923). Ridge's (2003Ridge's ( , 2004 deglaciation sequences show western Massachusetts ice-free by 17,200 yr ago, and deglaciation at Davis Pond may have been at least as early as 19.0-18.5 cal ka BP.…”
Section: Site Descriptionmentioning
confidence: 99%
“…1). Surficial sediments are glacially derived sand and gravel deposits (Norvitch and Lamb, 1966), and overlie Cambrian-Ordivician-age Berkshire schist (Dale, 1923). Ridge's (2003Ridge's ( , 2004 deglaciation sequences show western Massachusetts ice-free by 17,200 yr ago, and deglaciation at Davis Pond may have been at least as early as 19.0-18.5 cal ka BP.…”
Section: Site Descriptionmentioning
confidence: 99%
“…Locally, fractures in these rocks have been enlarged by solution, which has considerably increased aquifer permeability. As a result, well yields that exceed 1,000 gal/ min have been reported (Norvitch and Lamb, 1966). Wells completed in this aquifer provide industrial and rural domestic supplies but no public supplies.…”
Section: Carbonate Rock Aquifermentioning
confidence: 93%
“…Streamflow in the Housatonic River is affected by regulation on the East Branch Housatonic River and by the five large dams that use water for hydroelectric power and paper-mill processes. Additional detailed information on surfaceand ground-water characteristics in the Housatonic River Basin can be found in Norvitch (1966), Norvitch and Lamb (1966), Norvitch and others (1968), Wandle and Lippert (1984), and Bent (1999).…”
Section: Hydrologymentioning
confidence: 99%