An Obstructed Cave Passage in the Cobleskill Plateau: A Gravimetric Study
The Cobleskill Plateau of central New York, part of the greater Helderberg Plateau, is comprised of Silurian and Devonian limestone. This area displays caves and karst landforms subsequently altered by glaciation. The glacially mantled and in-filled pre-existing karst topography of the area was caus...
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| Format: | Article |
| Language: | English |
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AIMS Press
2015-12-01
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| Series: | AIMS Geosciences |
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| Online Access: | http://www.aimspress.com/geosciences/article/577/fulltext.html |