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dc.contributor.author Thompson, Gerald L.
dc.date.accessioned 2014-04-03T18:10:09Z
dc.date.available 2014-04-03T18:10:09Z
dc.date.issued 1965
dc.identifier.uri http://hdl.handle.net/1993/23389
dc.description Courtesy of the U.S. Geological Survey. Online document located at http://pubs.usgs.gov/wsp/1809k/report.pdf en_US
dc.description.abstract Melt-water channel deposits are among the most important aquifers in south-western Minnesota, but permeable zones within the deposits are difficult to locate, interpretation of the depositional history of proglacial channel deposits from aerial photographs and test-hole samples indicates the position of the permeable zones. Generally, the coarse-grained deposits are in headwater areas, near the confluence of two channels, in bends, or at the junction of sluiceways. Locally, these deposits yield as much as 1,000 gallons per minute to wells. en_US
dc.language.iso en en_US
dc.publisher United States Government Printing Office, Washington en_US
dc.relation.ispartofseries Geological Survey Water-Supply Paper;1809-K
dc.subject hydrology en_US
dc.subject Melt-water en_US
dc.subject Southwestern Minnesota en_US
dc.subject Lake Winnipeg Basin en_US
dc.title Hydrology of Melt-Water Channels in Southwestern Minnesota en_US
dc.type Technical Report en_US


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