Glacial Lake Lind, Wisconsin and Minnesota
Geological Society of America Bulletin
By: M.D. Johnson, K.L. Addis, L.R. Ferber, C.B. Hemstad, G. N. Meyer, and L.T. Komai
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Abstract
Glacial Lake Lind developed in the pre–late Wisconsinan St. Croix River valley, Minnesota and Wisconsin, and lasted more than 1000 yr during the retreat of the Superior lobe at the end of the Wisconsinan glaciation. Lake Lind sediment consists primarily of red varved silt and clay, but also includes mud-flow deposits, nearshore silt (penecontemporaneously deformed in places), nearshore rippled sand, and deltaic sand.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Glacial Lake Lind, Wisconsin and Minnesota |
| Series title | Geological Society of America Bulletin |
| DOI | 10.1130/0016-7606(1999)111<1371:GLLWAM>2.3.CO;2 |
| Volume | 111 |
| Issue | 9 |
| Year Published | 1999 |
| Language | English |
| Publisher | Geological Society of America |
| Description | 16 p. |
| First page | 1371 |
| Last page | 1386 |
| Country | United States |
| State | Minnesota, Wisconsin |
| Other Geospatial | Glacial Lake Lind |
| Google Analytic Metrics | Metrics page |