| Mont Yamaska Wigwômadenek | |
|---|---|
 Aerial Shot of Mount Yamaska | |
| Highest point | |
| Elevation | 411 m (1,348 ft) |
| Coordinates | 45°27′25″N 72°52′19″W / 45.45694°N 72.87194°W |
| Geography | |
| Location | Saint-Paul-d'Abbotsford, 12 kilometers northwest of Granby, Quebec, Canada |
| Parent range | Monteregian Hills |
| Topo map | NTS 31H7 Granby |
| Geology | |
| Age of rock | Early Cretaceous |
| Mountain type | Intrusive stock |
Mont Yamaska (in English, Mount Yamaska) (in Abenaki, Wigwômadenek[1]) is part of the Monteregian Hills in southern Quebec. Its summit stands 411 m (1,348 ft) above sea level. This mountain is largely covered with deciduous forest dominated by sugar maple. Some apple orchards are raised on lower slopes.
Geology
[edit]Mont Yamaska is composed of igneous rock and hornfels. The igneous rock is mostly mafic with much gabbro, essexite, and a titanium-rich pyroxenite. There also is a small area of nepheline syenite. Mont Yamaska might be the deep extension of a vastly eroded ancient volcanic complex, which was probably active about 125 million years ago.[2] The mountain was created when the North American Plate moved westward over the New England hotspot,[2] along with the other mountains of the Monteregian Hills that form part of the Great Meteor hotspot track.
See also
[edit]References
[edit]- ^ Paré, Pierre (1985). La toponymie des Abénaquis (in French). Gouvernement du Québec. ISBN 2-551-09122-5.
- ^ a b A Hundred-Million Year History of the Corner Rise and New England Seamounts Archived 2006-05-03 at the Wayback Machine Retrieved on 2007-08-01
External links
[edit]
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