Geological Survey research 1968: Chapter C
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Abstract
Refractory flint clay and semiflint clay layers, totaling as much as 7% feet in thickness, occur in the lower part of the Allegheny Formation of Pennsylvanian age in north-central Randolph County, W.Va. The deposit seems to be a lens in a widespread bed of plastic clay and may underlie an area of 1-2 square miles. Refractory tests of three samples indicate a pyrometric cone equivalent of cone 30-31 which is comparable with tests of the most highly refractory clay previously reported from West Virginia.
Publication type | Report |
---|---|
Publication Subtype | USGS Numbered Series |
Title | Geological Survey research 1968: Chapter C |
Series title | Professional Paper |
Series number | 600 |
Chapter | C |
DOI | 10.3133/pp600C |
Year Published | 1968 |
Language | English |
Publisher | U.S. Geological Survey |
Contributing office(s) | North Dakota Water Science Center, Wisconsin Water Science Center, Dakota Water Science Center |
Description | 225 p. |
Larger Work Type | Report |
Larger Work Subtype | USGS Numbered Series |
Larger Work Title | Scientific notes and summaries of investigations in geology, hydrology, and related fields (Professional Paper 600) |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |