Pottsville Formation

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Blackwater Falls in West Virginia. The major ledge is Connoquenessing sandstone of the Middle Pottsville Formation.
Blackwater Falls in West Virginia. The major ledge is Connoquenessing sandstone of the Middle Pottsville Formation.

The Pennsylvanian Pottsville Formation (φp) is a mapped bedrock unit in eastern Pennsylvania, western Maryland and West Virginia. It is a major ridge-former In the Ridge-and-Valley Appalachians of the eastern United States[1]

Contents

[edit] Description

The carboniferous Pottsville Formation consists of a gray conglomerate, fine to coarse grained and is known to contain sandstone, siltstone and shale, as well as anthracite coal.[2] It is considered a classic orogenic molasse.[3]

[edit] Age

Relative age dating of the Pottsville places it in the Pennsylvanian period.

[edit] Members

  • Connoquenessing sandstone

[edit] References

  1. ^ Kempler, Steve (2007-01-19). Geomorphology : Chapter 2 Plate T-12 : Folded Appalachians. NASA, Goddard Earth Sciences (GES), Data and Information Services Center (DISC). Retrieved on 2008-03-16. “The major ridge makers are the Tuscarora (T), Pocono (Po), and Pottsville (Pt) Formations.”
  2. ^ Geology : Pottsville (Pp). LEO EnviroSci Inquiry. Lehigh University. Retrieved on 2008-03-16.
  3. ^ Robinson, R.A.J.; Prave, A.R. (1995). "Cratonal contributions to a" classic" molasse; the Carboniferous Pottsville Formation of eastern Pennsylvania revisited". Geology 23 (4): 369-372. “The Carboniferous Pottsville Formation of eastern Pennsylvania in the central Appalachian foreland basin is considered a classic orogenic molasse …” 

[edit] See also