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Ausable Chasm





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Ausable Chasm is a sandstone gorge and tourist attraction located near the hamlet of Keeseville, New York, United States.[1] It is due west of Port Kent. The Ausable River runs through it and then empties into Lake Champlain. The gorge is about two miles (3.2 km) long and is a tourist attraction in the Adirondacks region of Upstate New York. It is fed by the Rainbow Falls at its southern extreme.

Ausable Chasm
Ausable Chasm
Ausable Chasm is located in New York
Ausable Chasm

Location in New York

Ausable Chasm is located in the United States
Ausable Chasm

Location in United States

LocationKeeseville,New York
Coordinates44°31′45N 73°27′40W / 44.52917°N 73.46111°W / 44.52917; -73.46111
Established1870
WebsiteOfficial website

Geological formation

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Bridge at Ausable Chasm

The Ausable Gorge was carved out of 500 million-year-old Potsdam Sandstone from the Cambrian Period. Since the end of the Pleistocene Epoch ice age 10,000 years ago, the movement and subsequent melting of glaciers created a series of caves and tunnels, which the Ausable River linked up and exploited on its one mile (1.6 km) journey to Lake Champlain. During this time, the headward erosion of ancestral Rainbow Falls led to its location today, where the visitor's center was built.[2] The chasm has a continuous exposure of a section of Potsdam Sandstone more than 520 feet (160 m) thick, which has yielded a rare, mid-Cambrian Scyphomedusae jellyfish fossil.[3]

 
Rapids in the gorge.

Some of the rock formations have been given names such as Cathedral, The Devil's Oven, Elephant's Head, The Flume, Sentinel Rock, and Table Rock.[citation needed]

Tourism

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In 1760, Major John Howe explored the chasm on ropes. Five years later, Irish settler William Gilliland wrote about the Chasm in his journal: "It is a most admirable sight, appearing on each side like a regular built wall, somewhat ruinated, and one would think that this prodigious clift was occasioned by an earthquake, their height on each side is from 40 to 100 feet in the different places; we saw about a half a mile of it, and by its appearance where we stopped it may continue very many miles further."[4][5] Called by some the "Little Grand Canyon of the East", the 1.5-mile-long (2.4 km) chasm opened to the public in 1870.[6]

Cultural attractions

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References

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  1. ^ "AuSable Chasm". Amazing Adirondack Wonders. Adirondack Wilderness Foundation. 2011. ISBN 9781458364159.
  • ^ "Ausable Chasm". Hudson Valley Geologist. November 2013.
  • ^ Hagadorn, James W. & Belt, Edward S. (2008). "Stranded in Upstate New York: Cambrian Scyphomedusae from the Potsdam Sandstone" (PDF). PALAIOS. 23 (7): 424–441. doi:10.2110/palo.2006.p06-104r. S2CID 129933062. Archived from the original (PDF) on 2012-06-19. Retrieved 2012-08-02.
  • ^ Brown, Phil (1999). Longstreet Highroad Guide to the New York Adirondacks. Taylor Trade Publishing. p. 112. ISBN 9781461661986.
  • ^ "Ausable Chasm - Grand Canyon of the Adirondacks-Discovery of Ausable Chasm | History". ausablechasm.com. Retrieved 2019-02-06.
  • ^ "Ausable Chasm". Fodor's.
  • ^ "North Star Underground Railroad Museum". northcountryundergroundrailroad.com.
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    Last edited on 13 July 2024, at 18:52  





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    This page was last edited on 13 July 2024, at 18:52 (UTC).

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