About: Mount Carleton   Sponge Permalink

An Entity of Type : dbkwik:resource/96Cu_Mm2Wb2LsaPGkXBz4w==, within Data Space : 134.155.108.49:8890 associated with source dataset(s)

Mount Carleton is the highest elevation in the Canadian province of New Brunswick. Mount Carleton is a monadnock, an erosional remnant of resistant ingneous 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 Carleton are part of the Gaspé Belt.

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rdf:type
rdfs:label
  • Mount Carleton
rdfs:comment
  • Mount Carleton is the highest elevation in the Canadian province of New Brunswick. Mount Carleton is a monadnock, an erosional remnant of resistant ingneous 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 Carleton are part of the Gaspé Belt.
sameAs
dcterms:subject
Range
Topographic map
  • NTS 21O/07
Name
  • Mount Carleton
dbkwik:geology/pro...iPageUsesTemplate
Coordinates
  • 47(xsd:integer)
Elevation
  • 817.0
Location
  • Northumberland County, New Brunswick
abstract
  • Mount Carleton is the highest elevation in the Canadian province of New Brunswick. Mount Carleton is a monadnock, an erosional remnant of resistant ingneous 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 Carleton are part of the Gaspé Belt.
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