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- Q5569326 subject Q8720716.
- Q5569326 abstract "The Glenshaw Formation is a mapped sedimentary bedrock unit in Pennsylvania, Maryland, West Virginia, and Ohio, of Pennsylvanian age. It is the lower of two formations in the Conemaugh Group, the upper being the Casselman Formation. The boundary between these two units is the top of the marine Ames Limestone. The Conemaugh Group overlies the Upper Freeport coal bed of the Allegheny Formation and underlies the Pittsburgh coal seam of the Monongahela Group.The Conemaugh Group consists of cyclic sequences of shale, siltstone, sandstone, red beds, thin impure limestone, and thin nonpersistent coal. Red beds are associated with landslides.The thickness of the Conemaugh Group averages about 400 feet in Ohio, and it ranges from 450 feet on the Ohio River in West Virginia to 520 feet in Washington County, Pennsylvania, and then to 890 feet in Somerset County, Pennsylvania.The Glenshaw formation was originally mapped in Pennsylvania by Flint, but was extended into West Virginia by Cardwell et al. in 1968. It is also recognized in eastern Ohio.".
- Q5569326 wikiPageWikiLink Q1371.
- Q5569326 wikiPageWikiLink Q1391.
- Q5569326 wikiPageWikiLink Q1397.
- Q5569326 wikiPageWikiLink Q1400.
- Q5569326 wikiPageWikiLink Q17510861.
- Q5569326 wikiPageWikiLink Q18157762.
- Q5569326 wikiPageWikiLink Q3694119.
- Q5569326 wikiPageWikiLink Q373772.
- Q5569326 wikiPageWikiLink Q4731301.
- Q5569326 wikiPageWikiLink Q5049298.
- Q5569326 wikiPageWikiLink Q620627.
- Q5569326 wikiPageWikiLink Q7199428.
- Q5569326 wikiPageWikiLink Q736917.
- Q5569326 wikiPageWikiLink Q82480.
- Q5569326 wikiPageWikiLink Q8720716.
- Q5569326 comment "The Glenshaw Formation is a mapped sedimentary bedrock unit in Pennsylvania, Maryland, West Virginia, and Ohio, of Pennsylvanian age. It is the lower of two formations in the Conemaugh Group, the upper being the Casselman Formation. The boundary between these two units is the top of the marine Ames Limestone.".
- Q5569326 label "Glenshaw Formation".