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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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Daniel Case at the English-language Wikipedia, the copyright holder of this work, hereby publishes it under the following license:
GNU head Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License.
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current04:09, 3 August 2007Thumbnail for version as of 04:09, 3 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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