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Mount Royal Chalet is a building located near the summit of Mount Royal in Montreal, Quebec, Canada. The chalet was constructed in 1932 [1] under the mayoralty of Camillien Houde as a make-work project during the Great Depression. [2] The French Beaux Arts structure was designed by Montreal architect Aristide Beaugrand-Champagne (1876-1950). [3 ...
The Mount Royal Arena (French: Aréna Mont-Royal) was an indoor arena located in Montreal, Quebec, Canada at the corner of Mount Royal and St. Urbain Street. [1] It was home of the National Hockey League (NHL) Montreal Canadiens from 1920 to 1926, before moving to the then two-year-old Montreal Forum. It had a capacity of 6,000 seated, 10,000 ...
Starting in 1745, the urbanized area of Montreal began to extend beyond its fortifications. The Plateau-Mont-Royal was born when the Faubourg Saint-Laurent to the north became the main area of development. In 1792, Montreal expanded, with new official limits about two kilometres (1¼ miles) beyond the original fortifications.
Mount Royal was designed in 1876 by Frederick Law Olmsted, best known as the designer of New York's Central Park. Mount Royal's features include the Chalet and the Kondiaronk Belvedere overlooking downtown Montreal, and man-made Beaver Lake (Lac aux Castors) with its recently renovated pavilion.
The city is named after the most prominent geographical feature on the island, a three-head hill called Mount Royal. [3] Montreal is at the centre of the Montreal Metropolitan Community, and is bordered by the city of Laval to the north, Longueuil to the south, Repentigny to the east and the West Island municipalities to the west.
The first definition of the Monteregian Hills came about in 1903 when Montreal geologist Frank Dawson Adams began referring to Mount Royal (Latin, Mons Regius) and mountains of similar geology in the Saint Lawrence Lowlands as the "Royal Mountains" (French: montagnes royales). [1]
Mount Royal is the deep extension of a vastly eroded ancient volcanic complex, which was probably active about 125 million years ago. [2]The mountain, along with the other mountains of the Monteregian Hills, was formed when the North American Plate moved westward over the New England hotspot. [2]