Mount Carleton
From Geology Wiki
| Elevation | 817 metres (2,680 feet) |
|---|---|
| Location | Northumberland County, New Brunswick |
| Range | Appalachian Mountains |
| Prominence | |
| Coordinates | 47° 23′ 0″ N, 66° 53′ 0″ W |
| Topographic map | NTS 21O/07 |
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.
