Jump to content

Aspy River

Coordinates: 46°53′31.6″N 60°27′19.6″W / 46.892111°N 60.455444°W / 46.892111; -60.455444
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Frietjes (talk | contribs) at 15:05, 7 April 2016. The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Aspy River
Beulach Ban waterfall on the Aspy River
Map
Physical characteristics
Mouth 
 • location
Aspy Bay
 • elevation
sea level
Length40 km (25 mi)

The Aspy River is a river on northeastern Cape Breton Island which rises in the Cape Breton Highlands and empties into Aspy Bay. The river valley follows the ancient Aspy Fault which extends for 40 km inland from the coast and extends along the upper section of the northeast Margaree River. This geological fault is thought to be a part of the Cabot Fault (Newfoundland)/ Great Glen Fault (Scotland) system of Avalonia.[1][2]

It is believed by some sources that John Cabot landed at Aspy Bay in 1497. In 1856, a submarine cable was laid across the Cabot Strait from Aspy Bay to Newfoundland establishing a telegraph link between St. John's, Newfoundland and New York City.

A dirt road in Cape Breton Highlands National Park leads to the Beulach Ban falls on the North Aspy River. "Beulach Ban" is Gaelic for "white gorge".

See also

  1. ^ Wilson, Tuzo (14 July 1962). "Cabot Fault, An Appalachian Equivalent of the San Andreas and Great Glen Faults and some Implications for Continental Displacement". Nature. 195 (4837): 135–138. Bibcode:1962Natur.195..135W. doi:10.1038/195135a0.
  2. ^ Dewey, John F.; Kennedy, Michael J.; Kidd, William S.F. (1983). "A geotraverse through the Appalachians of northern Newfoundland". Profiles of Orogenic Belts (PDF). Geodynamics Series. Vol. 10. American Geophysical Union. {{cite book}}: Unknown parameter |editors= ignored (|editor= suggested) (help)

46°53′31.6″N 60°27′19.6″W / 46.892111°N 60.455444°W / 46.892111; -60.455444