Geology of Clover Hollow and surrounding area, Giles and Craig Counties, Virginia
Structures in the study area, from southeast to northwest, are the Blacksburg synclinorium, Poplar Hill anticline, Saltville fault, Spruce Run syncline, Clover Hollow anticline, and Johns Creek syncline. The folds are believed to have had their inception by early Middle Ordovician time. The Knox-Mid...
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| Format: | Others |
| Language: | en |
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Virginia Polytechnic Institute and State University
2015
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| Online Access: | http://hdl.handle.net/10919/52227 |