Back to results

Virginia Polytechnic Institute

Geology of the Millers Cove area, Roanoke, Craig and Montgomery counties, Virginia

Abstract

dc:description.abstract

The Millers Cove area is underlain by rock ranging in age from Middle Cambrian Elbrook Dolomite to Early Mississippian Price Sandstone. Carbonate deposition was dominant into the Ordovician with elastic sedimentation dominant throuhout the rest of the Paleozoic. Cove Mountain is formed by the overturned northeast plunging Cove Mountain anticline and Dragons Tooth syncline. To the southwest the anticline passes beneath the Pulaski fault. The extension of the anticline to the northeast is unknown but it may be continuous with the Broad Run anticline. The Dragons Tooth syncline is continuous to the northeast with the North Mountain syncline but to the southwest passes beneath the Pulaski fault. The southwest plunging Brush Mountain-Little Mountain syncline may be continuous with the northeast plunging Broad Run Mountain syncline. The Miller fault has 10,000 feet of stratigraphic displacement where it passes under the Pulaski fault but it loses displacement and apparently terminates to the northeast. Thus, the Miller fault block is paraautochthonous. The Pulaski fault which separates the Miller fault block from the Catawba syncline is an overthrust of 10 mile horizontal displacement and 10,000 foot stratigraphic displacement. The first of two different deforming forces produced folds whose axes trend N. 35° E. The second was associated with thrust faulting and caused refolding along trends of N. 60° E. Accompanying faulting was the rotation of the southwestern end of the Miller fault block, the depression of the Brush Mountain-Little Mountain syncline beneath the weight of the Pulaski and Miller fault blocks, and the bowing of the Catawba syncline and Sinking Creek anticline under the buttressing action of Cove Mountain.

Degree

thesis:*
Name thesis:degree_name
Master of Science
Level thesis:degree_level
masters
Discipline thesis:degree_discipline
Geology
Department dc:contributor.department
Geology
Grantor dc:publisher
Virginia Polytechnic Institute
Year dc:date.issued
1966

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Bauerlein, Henry Jack

Rights

dc:rights
Statement dc:rights
  • In Copyright
Language dc:language.iso
en

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/10919/82706
OAI identifier oai:identifier
oai:vtechworks.lib.vt.edu:10919/82706

Chain of custody

source
Harvested from
Virginia Tech
Base URL
vtechworks.lib.vt.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
related terms
citation

Bauerlein, Henry Jack. Geology of the Millers Cove area, Roanoke, Craig and Montgomery counties, Virginia. masters thesis, Virginia Polytechnic Institute, 1966. http://hdl.handle.net/10919/82706