Английская Википедия:Abbé Huard River

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Шаблон:Infobox river Abbé Huard River (Шаблон:Lang-fr) is a river in the Côte-Nord region of the province of Quebec, Canada. It is a tributary of the Romaine River. The lower part of the river, where it meandered through sand and gravel deposits, has been flooded by the Romaine-2 reservoir.

Location

The Abbé-Huard River, a tributary of the Romaine River, originates in Abbé Huard Lake.Шаблон:Sfn The lake is in the unorganized territory of Lac-Jérôme in the Minganie Regional County Municipality.Шаблон:Sfn It is a little more than Шаблон:Convert north of the municipality of Baie-Johan-Beetz on the north shore of the Gulf of Saint Lawrence.Шаблон:Sfn The river is the second northeast branch of the Romaine River.Шаблон:Sfn The mouth of the river, where it meets the Romaine River, is also in Lac-Jérôme.Шаблон:Sfn Before the river was flooded, the Abbé-Huard entered the Romaine at PK 131.Шаблон:Sfn

Name

Abbé Huard Lake is named after the abbé Victor-Alphonse Huard (1853–1929), a naturalist and a professor at the Chicoutimi Seminary. He visited the region between Pessamit and Natashquan in 1895, and described the trip in his Labrador et Anticosti (1897). In his Dictionary of Rivers and Lakes of the Province of Quebec (1914), Eugène Rouillard points out the lake was probably named after the Abbé Huard before the river. The Innu call the river Uauiekamau Hipu, or "Round Lake River". The Naskapi call the river Umuauk Shipu or "Loon River", a literal translation of the French Rivière Huard.Шаблон:Sfn

Basin

The river basin covers Шаблон:Convert.Шаблон:Sfn The river flows along the contact zone between rocks of the Anorthositic Suite of Havre-Saint-Pierre to the north, and deformed rocks to the south.Шаблон:Sfn A map of the ecological regions of Quebec shows the river on the border between sub-regions 6j-S and 6n-T of the east spruce/moss subdomain.Шаблон:Sfn

Flooded section

The lower part of the Abbé-Huard River now forms the northeast arm of the Romaine-2 reservoir.Шаблон:SfnШаблон:Sfn Before the Romaine-2 reservoir was flooded, the mouth of the river flowed between terraces of sand and gravel.Шаблон:Sfn These banks typically rose from Шаблон:Convert above the watercourse.Шаблон:Sfn About Шаблон:Convert of the river's banks were subject to active erosion, mostly on the concave shores. There was a well-developed delta at the river mouth.Шаблон:Sfn Water temperatures at the mouth of the river where it entered the Romaine ranged from an average of Шаблон:Convert in January to Шаблон:Convert in July.Шаблон:Sfn The flooded section was thought to have high archaeological potential, but a survey found no sites.Шаблон:Sfn

Notes

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Sources

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See also