File:Schunemunk conglomerate and pine.jpg

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Description Pitch pine and conglomeratic rock typical of Schunemunk Mountain. Geological details: The Schunemunk conglomerate (also spelled Schunnemunk or Skunnemunk) represents a Mid-Devonian terrestrial molasse deposit of the Acadian fold belt. The conglomerate has been folded subsequently during the Alleghenian orogeny, the last orogenic event in the Appalachian Mts. Green Pond outlier (downfaulted block with Paleozoic sediments surrounded by precambrian basement) of Orange Co., New York.
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Author Daniel Case
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14 July 2007

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current21:09, 2 August 20072,433 × 1,755 (837 KB)Daniel Case{{Information |Description=Scrub pine and conglomerate rock typical of Schunemunk Mountain |Source=self-made |Date=2007-07-14 |Author= Daniel Case |Permission={{GFDL-user-w|en|English Wikipedia|Daniel Case}}

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