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Until concrete evidence suggesting its existence was discovered in 1975, biologists typically discounted the idea that a grizzly bear had once roamed northern Quebec. Various reports of brown bears from 1900 to 1950 were written off as colour morphs of the more common American black bear.
Caniapiscau Reservoir Robert-Bourassa Reservoir Manicouagan Reservoir Meech Lake from Blanchet beach by south-west coast Lac des Nations Clearwater Lakes (Lac a l'Eau-Claire) Île aux Tourtes Bridge across Lake of Two Mountains, with Mont Oka in the background Pingualuit crater lake Looking south over Lake Timiskaming from Fort Témiscamingue near Ville-Marie, Quebec.
The rivière de l'Ours, also known as Bear River, is a tributary of the Gulf of St. Lawrence, flowing in the municipality of L'Île-d'Anticosti, in the Minganie Regional County Municipality, in the administrative region of Côte-Nord, in the province of Quebec, in Canada. A forest road serves the upper and intermediate part of its course.
It is located near Moffet in Témiscamingue Regional County Municipality. Simard Lake covers an area of 170 km². With a length of 18 km and a width of 12 km, the lake is located about 25 km west of Decelles Reservoir and more than 50 km to the east of Lake Timiskaming .
The Pikauba River, in 1940.. Parc des Laurentides was created in 1895 as a forest reserve and as a recreational area for the public. In 1981, two large parcels were split off to become Jacques-Cartier National Park in the south and the Grands-Jardins National Park in the east, while the remaining territory was established as a wildlife reserve.
La Vérendrye wildlife reserve is one of the largest reserves in the province of Quebec, Canada, covering 12,589 square kilometres (4,861 sq mi) [1] of contiguous land and lake area (Assinica wildlife reserve is the largest in the province, but its territory is broken up in four non-contiguous parts).
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The Jacques-Cartier River drains an area of 2,515 square kilometres (971 sq mi), starting in and flowing for nearly 160 kilometres (99 mi) through the Laurentian Mountains in the geological region of Grenville (one of the youngest sections of the Canadian Shield, formed 955 million years ago), then flows through the sedimentary rocks of the St. Lawrence Lowlands for approximately 17 kilometres ...