Ledger Formation Stratigraphic range: Cambrian |
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Type | Formation |
Sub-units | Lower dolomite member, Willis Run Member, upper dolomite member |
Overlies | Kinzers Formation |
Lithology | |
Primary | Dolomite |
Location | |
Region | Pennsylvania |
Country | United States |
Extent | Pennsylvania, Maryland, Virginia |
Type section | |
Named by | Stose, G.W., and Jonas, A.I. |
The Ledger Formation or Ledger Dolomite is a geologic formation in Pennsylvania, United States.
The Ledger is described as light-gray, locally mottled, massive, pure, coarsely crystalline dolomite. It may be siliceous in the middle part.
Named from exposures at Ledger, Pennsylvania, formerly 3 miles northeast of Kinzers, Lancaster County, Pennsylvania.
At Valley Forge National Historical Park, the visitor center parking lot is built within an old quarry of the Ledger, and the former quarry walls are exposed. The rocks contain stromatolites. In the nearby Port Kennedy Quarry, the Triassic unconformably overlies the folded Ledger.
The Ledger is exposed at a roadcut on the south side of Route 30 at the interchange with Route 23 (East Walnut Street) on the northeast side of Lancaster.