Structure associated with rock creep in the Black Hills, South Dakota
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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.
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 |
Google Analytic Metrics | Metrics page |