Structure associated with rock creep in the Black Hills, South Dakota
Geological Society of America Bulletin
By: J.J. Norton and J. A. Redden
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Abstract
Many areas of schist in the southern Black Hills, South Dakota, have a thin zone of disintegrated rock that is 4-10 feet below the ground surface and parallel to it. Fresh, undeformed schist overlying this zone has moved downhill in a mass-wasting process since the present surface was formed.
Suggested Citation
Norton, J., Redden, J.A., 1960, Structure associated with rock creep in the Black Hills, South Dakota: Geological Society of America Bulletin, v. 71, no. 7, p. 1109-1112, https://doi.org/10.1130/0016-7606(1960)71[1109:SAWRCI]2.0.CO;2.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Structure associated with rock creep in the Black Hills, South Dakota |
| Series title | Geological Society of America Bulletin |
| DOI | 10.1130/0016-7606(1960)71[1109:SAWRCI]2.0.CO;2 |
| Volume | 71 |
| Issue | 7 |
| Year Published | 1960 |
| Language | English |
| Publisher | Geological Society of America |
| Description | 4 p. |
| First page | 1109 |
| Last page | 1112 |
| Country | United States |
| State | South Dakota |
| Other Geospatial | Black Hills |