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The Chaloupe River (french: Rivière à la Chaloupe,
Shallop Shallop is a name used for several types of boats and small ships (French ''chaloupe'') used for coastal navigation from the seventeenth century. Originally smaller boats based on the chalupa, the watercraft named this ranged from small boats a l ...
River) is a river of the
Côte-Nord Côte-Nord (, ; ; land area ) is the second-largest administrative region by land area in Quebec, Canada, after Nord-du-Québec. It covers much of the northern shore of the Saint Lawrence River estuary and the Gulf of Saint Lawrence past Tadous ...
region of Quebec. It flows from north to south and empties into the
Gulf of Saint Lawrence , image = Baie de la Tour.jpg , alt = , caption = Gulf of St. Lawrence from Anticosti National Park, Quebec , image_bathymetry = Golfe Saint-Laurent Depths fr.svg , alt_bathymetry = Bathymetry ...
.


Location

The mouth of the Chaloupe River is halfway between Sept-Îles and
Havre-Saint-Pierre Havre-Saint-Pierre is a town on Pointe-aux-Esquimaux, which is on the Quebec north shore (Côte-Nord) of the Saint Lawrence River in Canada. Located along Route 138 some east of Sept-Îles, it is the largest town and seat of the Minganie RCM, ...
. It flows from north to south. The river can only be navigated in small craft. Tributaries include the Guillaume, Vibert and Robichaud rivers, which are all small. The mouth of the Chaloupe River is in the municipality of Rivière-au-Tonnerre in the Minganie Regional County Municipality. The hamlet of Rivière-à-la-Chaloupe is on the east of the river's estuary.


Name

A ''chaloupe'' r/sup> is a small French boat such as a lug-rigged fishing boat. The Abbé Huard visited the hamlet of La Chaloupe on the east shore at the end of the 19th century. When he asked what the name meant, he was told it was a river with greater volume than the Rivière aux Graines earby to the west and it is precise to call it the Rivière Chaloupe. He added that boats of this type were much used in these parts, and found an excellent harbor there. An English variant of the name is Shallop River. A peat bog that extends northeast of the hamlet is called the Grande Plaine de la Chaloupe.


Description

The ''Dictionnaire des rivières et lacs de la province de Québec'' (1914) describes the river as,


Terrain

The coastal plain along the Gulf of Saint Lawrence is wide in this region, with relatively flat terrain rising gradually to of elevation in the north. The
Goldthwait Sea The Goldthwait Sea was a sea that emerged during the last deglaciation, starting around 13,000 years ago, covering what is now the Gulf of Saint Lawrence and surrounding areas. At that time, the land had been depressed under the weight of the Laur ...
deposited large amounts of clay and silt on the plain, later covered by deltaic sandy sediments. Most of the basin is in the piedmont region of rounded rocky hills, with average altitude increasing to in the north. The highest point is high in the northern end. The bedrock is undeformed
magma Magma () is the molten or semi-molten natural material from which all igneous rocks are formed. Magma is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural sa ...
tic rock. The north part is an
anorthositic Anorthosite () is a phaneritic, intrusive igneous rock characterized by its composition: mostly plagioclase feldspar (90–100%), with a minimal mafic component (0–10%). Pyroxene, ilmenite, magnetite, and olivine are the mafic minera ...
massif. The south is
granitoid A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar. Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quartz- ...
orthopyroxene and an assemblage of
granite Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies under ...
and pegmatite. In the piedmont the rock is covered with a thin layer of
glacial till image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is d ...
less than thick, with areas of exposed rock on the hills and valley walls. An old U-shaped valley in the north of the watershed holds some
glaciofluvial deposits Glaciofluvial deposits or Glacio-fluvial sediments consist of boulders, gravel, sand, silt and clay from ice sheets or glaciers. They are transported, sorted and deposited by streams of water. The deposits are formed beside, below or downstream ...
.


Basin

The Chaloupe River basin is partially in the unorganized territory of Lac-Jérôme (74.8%), partly in the municipality of Rivière-au-Tonnerre (25.2%). It covers . It is elongated, with north-south length of and an average east-west width of . It lies between the basins of the Manitou River to the west and the
Sheldrake River The Sheldrake River is a freshwater stream located in Southern Westchester, Southern Westchester County, New York (state), New York. The river forms in White Plains, New York, White Plains and flows south until it joins the Mamaroneck River. A ...
to the east. The Lake Vibert, at the source of the Vibert River, is the only lake of any size. Water bodies cover 2.37 of the river basin, and
ombrotrophic Ombrotrophic ("cloud-fed"), from Ancient Greek ὄμβρος (''ómvros'') meaning "rain" and τροφή (''trofí'') meaning "food"), refers to soils or vegetation which receive all of their water and nutrients from precipitation, rather than ...
peatlands cover 2.18%. The streams and rivers follow angular courses dictated by fractures in the bedrock, with straight line sections and right-angled junctions. In the downstream section of the Chaloupe in the south of the piedmont section the river winds through its alluvial sediments, and in the coastal plain it meanders. There is a estuary at the river mouth with several channels and shoals. The river is from north to south, with a vertical drop of . The annual average flow at its mouth is estimated at . Flow varies during the year from .


Environment

The Rivière-au-Tonnerre weather station is east of the river mouth. It records an average annual temperature of and average annual precipitation of . A map of the
ecological regions of Quebec The Ecological regions of Quebec are regions with specific types of vegetation and climates as defined by the Quebec Ministry of Forests, Wildlife and Parks. Given the size of this huge province, there is wide variation from the temperate deciduou ...
shows the river in sub-regions 6j-T and 6m-T of the east spruce/moss subdomain. Black spruce (''Picea mariana'') dominate the forests on the coastal plain, while the piedmont area has mixed black spruce and
balsam fir ''Abies balsamea'' or balsam fir is a North American fir, native to most of eastern and central Canada (Newfoundland west to central Alberta) and the northeastern United States (Minnesota east to Maine, and south in the Appalachian Mountains to ...
(''Abies balsamea''). In the past there has been heavy logging in the lower part of the river basin. In the late 1990s and early 2000s there was a major infestation of hemlock looper (''Lambdina fiscellaria'') moths, which caused large scale defoliation of the firs. Fish in the river consist of brook trout (''Salvelinus fontinalis''), American eel (''Anguilla rostrata'') and
rainbow smelt The rainbow smelt (''Osmerus mordax'') is a North American species of fish of the family Osmeridae. Walleye, trout, and other larger fish prey on these smelt. The rainbow smelt prefer juvenile ciscoes, zooplankton such as calanoid copepods ('' L ...
(''Osmerus mordax''). There is no wildlife sanctuary, controlled use zone or outfitter in the watershed. The Aire de concentration d'oiseaux aquatiques de la Rivière aux Graines, Anse à Georges (River Aux Graines – George's Cove water fowl gathering area), a
IUCN Management Category IUCN protected area categories, or IUCN protected area management categories, are categories used to classify protected areas in a system developed by the International Union for Conservation of Nature (IUCN). The enlisting of such areas is par ...
IV protected area, extends along the coast at the river mouth and includes the estuary.


Notes


Sources

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