Relation of the Wissahickon mica gneiss to the Shenandoah limestone and Octoraro schist of the Doe Run and Avondale region, Chester County, Pennsylvania
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- Document: Report
- Larger Work: This publication is Chapter B of Shorter contributions to general geology, 1916
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Abstract
The region discussed in this paper lies in Chester County, Pa., and is included in the eastern half of the Coatesville quadrangle. (See fig. 3.) It is within the belt of crystal-line schists and gneisses of the Piedmont Plateau. The northern half of the area, which will be called the Doe Run region, from the village of that name (see Fig. 4, p. 15), has been surveyed by Eleanora F. Bliss in connection with the problem of the relation of the Wissahickon mica gneiss to the Octoraro schist.
Study Area
Publication type | Report |
---|---|
Publication Subtype | USGS Numbered Series |
Title | Relation of the Wissahickon mica gneiss to the Shenandoah limestone and Octoraro schist of the Doe Run and Avondale region, Chester County, Pennsylvania |
Series title | Professional Paper |
Series number | 98 |
Chapter | B |
DOI | 10.3133/pp98B |
Year Published | 1917 |
Language | English |
Publisher | U.S. Geological Survey |
Description | 29 p. |
Larger Work Type | Report |
Larger Work Subtype | USGS Numbered Series |
Larger Work Title | Shorter contributions to general geology, 1916 (Bulletin 98) |
First page | 9 |
Last page | 34 |
Country | United States |
State | Pennsylvania |
Other Geospatial | Doe Run And Avondale Region |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |