Mont Xalibu
From Wikipedia, the free encyclopedia
| Mont Xalibu | |
|---|---|
.jpg) View of Mount Xalibu from Mount Joseph-Fortin. | |
| Highest point | |
| Elevation | 1,120 m (3,670 ft)[1] |
| Parent peak | Monts McGerrigle (Chic-Choc Mountains, Notre Dame Mountains, Appalachian Mountains) |
| Coordinates | 48°57′51″N 66°00′42″W / 48.96417°N 66.01167°W |
| Geography | |
  Mont Xalibu Location in Quebec | |
 | |
| Interactive map of Mont Xalibu | |
| Country | Canada |
| Province | Quebec |
| Administrative region | Gaspésie–Îles-de-la-Madeleine |
| Topo map | NTS 22B16 Mont Albert |
| Geology | |
| Rock age | About 400 million years (13,000 Ts)[2] |
| Mountain type | Cirque glaciaire |
| Rock type(s) | Skarn, cornéenne[2] |
Mount Xalibu is a mountain located in the unorganized territory of Mont-Albert, in Quebec. Culminating at 1,120 metres (3,670 ft) above sea level, it is one of the highest peaks in the Notre Dame Mountains. It is located in Gaspésie National Park.
The mountain, without official designation until 2 February 1989, was given the Mi'kmaq name of an animal that inhabits its flanks, the woodland caribou.[1]
Geography
Situation
Mount Xalibu is located in eastern Canada, in the province of Quebec, on the northern flank of the Gaspé Peninsula. It is 40 kilometres (25 mi) southeast of the town of Sainte-Anne-des-Monts, capital of La Haute-Gaspésie Regional County Municipality, and 450 kilometres (280 mi) northeast of Quebec, provincial capital. The summit rises to 1,120 metres (3,670 ft) of altitude in the McGerrigle Mountains, within the Chic-Choc Mountains of the Notre-Dame range.
Topography
Mount Xalibu is part of the McGerrigle Mountains, formerly called Tabletop (“table top”) because of their constitution in plateaus which surmount steep rock faces.[3]
Geology
About 400 million years ago, during the Devonian, an intrusion granite was inserted into the rocks sedimentary Paleozoic that form the current Gaspé Peninsula. The summit of Xalibu develops around this batholith. The southern flank of the mountain constitutes one of the walls of the glacial cirque of "Lac aux Américains".[4]
Climate
There is no station providing continuous climate data at the top of Mount Xalibu; a nearby station makes it possible to establish climatic normals.
Episodes of rain, melting conditions, the formation of ice shells and numerous snowstorms during the winter combine the conditions conducive to the formation of avalanches, common on the walls of the mountain.[5]
The prevailing winds are from the west. At 12 kilometres (7.5 mi) west of Xalibu, on Mount Albert,[Note 1] winds average at 24 kilometres per hour (15 mph). Gusts of 250 kilometres per hour (160 mph) have already been recorded there.[6]
Fauna and flora
The mountain is populated by the last herd of caribou south of the St. Lawrence River.
