About: Mount Edward (New Brunswick)   Sponge Permalink

An Entity of Type : dbkwik:resource/96Cu_Mm2Wb2LsaPGkXBz4w==, within Data Space : dbkwik.org associated with source dataset(s)

Mount Edward is the second highest elevation in the Canadian province of New Brunswick. Mount Edward is a monadnock, an erosional remnant of resistant ingenous rocks that remained after an ancient Mesozoic peneplain surface was uplifted in the Cenozoic to form a plateau. Erosion from glaciers, water, wind has eroded the mountains for hundreds of millions of years. The mountain consists of 400 million-year-old rhyolitic and basaltic volcanics. The underlying rocks of Mount Edward are part of the Gaspé Belt. This mountain is about 6 miles from Mount Carleton the New Brunswick Highlands highest peak.

AttributesValues
rdf:type
rdfs:label
  • Mount Edward (New Brunswick)
rdfs:comment
  • Mount Edward is the second highest elevation in the Canadian province of New Brunswick. Mount Edward is a monadnock, an erosional remnant of resistant ingenous rocks that remained after an ancient Mesozoic peneplain surface was uplifted in the Cenozoic to form a plateau. Erosion from glaciers, water, wind has eroded the mountains for hundreds of millions of years. The mountain consists of 400 million-year-old rhyolitic and basaltic volcanics. The underlying rocks of Mount Edward are part of the Gaspé Belt. This mountain is about 6 miles from Mount Carleton the New Brunswick Highlands highest peak.
dcterms:subject
Range
  • Appalachian Mountains
Topographic map
  • NTS 21O/07
Name
  • Mount Edward
dbkwik:geology/pro...iPageUsesTemplate
Coordinates
  • 47(xsd:integer)
Elevation
  • 800.0
Location
  • Northumberland County, New Brunswick
abstract
  • Mount Edward is the second highest elevation in the Canadian province of New Brunswick. Mount Edward is a monadnock, an erosional remnant of resistant ingenous rocks that remained after an ancient Mesozoic peneplain surface was uplifted in the Cenozoic to form a plateau. Erosion from glaciers, water, wind has eroded the mountains for hundreds of millions of years. The mountain consists of 400 million-year-old rhyolitic and basaltic volcanics. The underlying rocks of Mount Edward are part of the Gaspé Belt. This mountain is about 6 miles from Mount Carleton the New Brunswick Highlands highest peak.
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