Distribution and Significance of Some Ice-Disintegration Features in West-Central Indiana

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dc.contributor.authorBleuer, Ned K.
dc.date.accessioned2022-09-06T15:21:13Z
dc.date.available2022-09-06T15:21:13Z
dc.date.issued1974
dc.description.abstract"Ice-disintegration features are well known from the northern Great Plains of the United States and Canada; but they have not been extensively documented in the Midwest, although, historically, parts of this very west-central Indiana area served in T.C. Chamberlin's ""Nature of the Englacial Drift of the Mississippi Basin"" (1893) as the foremost examples of englacial and superglacial drift deposition (Bleuer, 1973). The form, distribution, and significance of such features in west-central Indiana, which include linear disintegration ridges and trenches, ice-walled channels and lakes, circular disintegration ridges(doughnuts), and prairie mounds, are described in this report."en
dc.identifier.citationBleuer, N. K., 1974, Distribution and significance of some ice-disintegration features in west-central Indiana: Indiana Geological Survey Occasional Paper 8, 11 p., 5 figs.en
dc.identifier.urihttps://hdl.handle.net/2022/28133
dc.language.isoenen
dc.publisherIndiana Geological & Water Surveyen
dc.relation.ispartofseriesOccasional Papers;08
dc.rightsThis work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 4.0 License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/4.0/ or send a letter to Creative Commons, 543 Howard Street, 5th Floor, San Francisco, California, 94105, USA.en
dc.rights.urihttps://creativecommons.org/licenses/by-sa/4.0/en
dc.subjectGeologic landscapeen
dc.subjectGlacial Geologyen
dc.subjectCentral-West Indianaen
dc.subjectIce Ageen
dc.titleDistribution and Significance of Some Ice-Disintegration Features in West-Central Indianaen
dc.typeTechnical Reporten

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