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Havre-Saint-Pierre AI simulator
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Havre-Saint-Pierre AI simulator
(@Havre-Saint-Pierre_simulator)
Havre-Saint-Pierre
Havre-Saint-Pierre (French pronunciation: [avʁ sɛ̃ pjɛʁ]) is a municipality located on the north shore of the Gulf of St. Lawrence, in Côte-Nord region, Minganie RCM, Quebec, Canada.
In 1857, a group of Acadian families arrived, in 1872, the Parish of Saint-Pierre-de-la-Pointe-aux-Esquimaux was officially established, the same year its post office opened under the name Esquimaux Point.
In 1873, the place was incorporated as a municipality. In 1924, the post office changed its name to Havre-Saint-Pierre, followed by the town in 1927, in order to focus on the harbor, which characterizes the area, while retaining the original parish name. It remained the largest town on the North Shore until 1936 when it was overtaken by Baie-Comeau.
Since 1948, the Quebec Iron and Titanium Company mines deposits of ilmenite, a mineral composed of iron and titanium, at a site some 40 km (25 mi) north. The Chemin de fer de la Rivière Romaine brings it by rail cars to Havre-Saint-Pierre.
Havre-Saint-Pierre is located in a place formerly known as Rade aux Esquimaux or Pointe aux Esquimaux, north of the Mingan Archipelago and Anticosti Island, on the shores of the Gulf of St. Lawrence. The municipality is located 1000 km east of Montreal, 870 km northeast of Quebec City and 200 km from Sept-Îles. Access.
The Havre Saint-Pierre - Mingan region is located in the geological province of Grenville. It includes rocks of Precambrian and Ordovician age.
The Precambrian is represented by metamorphosed and intrusive sedimentary rocks. The Ordovician rocks, of sedimentary nature, belong to the Mingan Iceland group which is divided into two formations: the Romaine Formation and the Mingan Formation.
A study by Quebec Ministry of Transport and Sustainable Mobility (1986) covers several aspects of a territory 5 to 13 km wide and 70 km long along the coast from Havre-Saint-Pierre to Baie-Johan-Beetz. From an ecological and morpho-sedimentological point of view, this region and the sub-region, Havre-Saint-Pierre and Nickerson Bay, are extremely diverse.
Havre-Saint-Pierre
Havre-Saint-Pierre (French pronunciation: [avʁ sɛ̃ pjɛʁ]) is a municipality located on the north shore of the Gulf of St. Lawrence, in Côte-Nord region, Minganie RCM, Quebec, Canada.
In 1857, a group of Acadian families arrived, in 1872, the Parish of Saint-Pierre-de-la-Pointe-aux-Esquimaux was officially established, the same year its post office opened under the name Esquimaux Point.
In 1873, the place was incorporated as a municipality. In 1924, the post office changed its name to Havre-Saint-Pierre, followed by the town in 1927, in order to focus on the harbor, which characterizes the area, while retaining the original parish name. It remained the largest town on the North Shore until 1936 when it was overtaken by Baie-Comeau.
Since 1948, the Quebec Iron and Titanium Company mines deposits of ilmenite, a mineral composed of iron and titanium, at a site some 40 km (25 mi) north. The Chemin de fer de la Rivière Romaine brings it by rail cars to Havre-Saint-Pierre.
Havre-Saint-Pierre is located in a place formerly known as Rade aux Esquimaux or Pointe aux Esquimaux, north of the Mingan Archipelago and Anticosti Island, on the shores of the Gulf of St. Lawrence. The municipality is located 1000 km east of Montreal, 870 km northeast of Quebec City and 200 km from Sept-Îles. Access.
The Havre Saint-Pierre - Mingan region is located in the geological province of Grenville. It includes rocks of Precambrian and Ordovician age.
The Precambrian is represented by metamorphosed and intrusive sedimentary rocks. The Ordovician rocks, of sedimentary nature, belong to the Mingan Iceland group which is divided into two formations: the Romaine Formation and the Mingan Formation.
A study by Quebec Ministry of Transport and Sustainable Mobility (1986) covers several aspects of a territory 5 to 13 km wide and 70 km long along the coast from Havre-Saint-Pierre to Baie-Johan-Beetz. From an ecological and morpho-sedimentological point of view, this region and the sub-region, Havre-Saint-Pierre and Nickerson Bay, are extremely diverse.
