| Skunnemunk Conglomerate | |
|---|---|
Stratigraphic range: | |
 Conglomerate rock typical of Schunemunk Mountain, New York. | |
| Type | Geological formation |
| Unit of | Green Pond Outlier |
| Overlies | Bellvale Sandstone |
| Thickness | About 3,000 ft.[1] |
| Lithology | |
| Primary | Conglomerate, Sandstone |
| Location | |
| Extent | New Jersey, New York |
The Skunnemunk Conglomerate (also spelled Schunemunk) is a mapped bedrock unit in New Jersey and New York from the Middle Devonian period.[1] It forms the resistant ridge of Schunemunk Mountain in New York and Bearfort Mountain in New Jersey.[2]
- ^ a b Volkert, Richard A. "OFM 104, Bedrock Geologic Map of the Wawayanda Quadrangle and the New Jersey Part of the Pine Island Quadrangle, Sussex and Passaic Counties, New Jersey and Orange County, New York" (PDF). New Jersey Geological and Water Survey.
- ^ "The Green Pond Outlier". U.S. Geological Survey.