| Abstract: | The Winegar Phase of the Wisconsin Glaciation produced a band of hummocky glacial topography in northern Wisconsin. Some hummocks are composed of flow till and somewhat sorted till-like debris-flow sediment. These hummocks formed when ice melted beneath a cover of debris that flowed to its present position. Other hummocks contain interlayered lodgement and meltout till, flow till, debris-flow and slopewash sediment, lake, and meltwater-stream sediment. These hummocks formed where sediment was stacked near the ice margin. In other hummocks till and supraglacial debris-flow and slopewash sediment deposited during the Winegar Phase form a thin veneer over older meltwater-stream sediment. These hummocks formed when ice buried in pre-Winegar Phase stream sediment melted, and the overlying sediment collapsed. ?? 1993. |
| Genre: | Article |
| ProdID: | 70017351 |
| Citation Author: | Attig, J. W.; Clayton, L. |
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| Citation End Page: | 67 |
| Citation Issue: | C |
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| Citation Language: | English |
| Citation Larger Work Title: | Quaternary International |
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| Citation Number Of Pages: | 7 |
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| Citation Publisher: | Elsevier |
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| Citation Search Results Text: | Stratigraphy and origin of an area of hummocky glacial topography, northern Wisconsin, U.S.A.; 1993; Article; Journal; Quaternary International; Attig, J. W.; Clayton, L. |
| Citation Start Page: | 61 |
| Citation Volume: | 18 |
| Citation Year: | 1993 |
| Type: | citation/reference |
| Text: | Stratigraphy and origin of an area of hummocky glacial topography, northern Wisconsin, U.S.A.; 1993; Article; Journal; Quaternary International; Attig, J. W.; Clayton, L. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1016/1040-6182(93)90054-J |
| Date Other: | Fri, 1 Jan 1993 00:00 -0600 |
| Publisher: | Elsevier |
