Chaloupe River (Anticosti Island)
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Chaloupe River (Anticosti Island)
The Chaloupe River (french: Rivière à la Chaloupe, Shallop River) is a river of the Côte-Nord region of Quebec. It flows from north to south and empties into the Gulf of Saint Lawrence. Location The mouth of the Chaloupe River is halfway between Sept-Îles and Havre-Saint-Pierre. 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 cal ...
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Minganie Regional County Municipality
Minganie is a regional county municipality in the Côte-Nord region of Quebec, Canada. It includes Anticosti Island. Its seat is Havre-Saint-Pierre, Quebec, Havre-Saint-Pierre. It has an area of according to Quebec's ''Ministère des Affaires municipales, des Régions et de l'Occupation du territoire'' (which includes coastal, lake, and river water territory and also Labrador boundary dispute, disputed land within Labrador), or a land area of according to Statistics Canada. The population from the Canada 2011 Census was 6,582 and in 2016 Canadian Census, 2016 it was 11,323. The majority live in Havre-Saint-Pierre. Minganie and the neighbouring Le Golfe-du-Saint-Laurent Regional County Municipality are grouped into the single Census divisions of Canada, census division of Minganie—Le Golfe-du-Saint-Laurent (known as Minganie–Basse-Côte-Nord before 2010). The combined population at the Canada 2011 Census was 11,708. Until 2002, Minganie RCM encompassed the entire lower n ...
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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 from the ice. They include kames, kame terraces and eskers formed in ice contact and outwash fans and outwash plains below the ice margin. Typically the outwash sediment is carried by fast and turbulent fluvio-glacial meltwater streams, but occasionally it is carried by catastrophic outburst floods. Larger elements such as boulders and gravel are deposited nearer to the ice margin, while finer elements are carried farther, sometimes into lakes or the ocean. The sediments are sorted by fluvial processes. They differ from glacial till, which is moved and deposited by the ice of the glacier, and is unsorted. Ice-contact deposits A subglacial megaflood may cut cavities into the base of the ice. As the flood dies down, sediment is deposited ...
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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 part of a strategy being used toward the conservation of the world's natural environment and biodiversity. The IUCN has developed the protected area management categories system to define, record and classify the wide variety of specific aims and concerns when categorising protected areas and their objectives. This categorisation method is recognised on a global scale by national governments and international bodies such as the United Nations and the Convention on Biological Diversity. Categories Category Ia – strict nature reserve A strict nature reserve (IUCN Category Ia) is an area which is protected from all but light human use in order to protect its biodiversity and also possibly its geological/geomorphical features. These are ...
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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 ('' Leptodiaptomus ashlandi'', '' L. minutus'', '' L. sicilis''), and other small organisms, but are aggressive and will eat almost any fish they find. They are anadromous spring spawners and prefer clean streams with light flow and light siltation. The rainbow smelt face several barriers. They are weak swimmers and struggle to navigate fish ladders preventing them from making it past dams to the headwater streams where they spawn. The rise in erosion and dams helped to decimate the smelt population in the 1980s. There are currently plans to try to reduce damming and to help control erosion. Description The body of the rainbow smelt is slender and cylindrical. It has a silvery, pale green back and is iridescent purple, blue, and pink on the ...
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American Eel
The American eel (''Anguilla rostrata'') is a facultative catadromous fish found on the eastern coast of North America. Freshwater eels are fish belonging to the elopomorph superorder, a group of phylogenetically ancient teleosts. The American eel has a slender, snake-like body that is covered with a mucus layer, which makes the eel appear to be naked and slimy despite the presence of minute scales. A long dorsal fin runs from the middle of the back and is continuous with a similar ventral fin. Pelvic fins are absent, and relatively small pectoral fins can be found near the midline, followed by the head and gill covers. Variations exist in coloration, from olive green, brown shading to greenish-yellow and light gray or white on the belly. Eels from clear water are often lighter than those from dark, tannic acid streams. The eel lives in fresh water and estuaries and only leaves these habitats to enter the Atlantic Ocean to make its spawning migration to the Sargasso Sea. Spa ...
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Brook Trout
The brook trout (''Salvelinus fontinalis'') is a species of freshwater fish in the char genus ''Salvelinus'' of the salmon family Salmonidae. It is native to Eastern North America in the United States and Canada, but has been introduced elsewhere in North America, as well as to Iceland, Europe, and Asia. In parts of its range, it is also known as the eastern brook trout, speckled trout, brook charr, squaretail, brookie or mud trout, among others. A potamodromous population in Lake Superior, as well as an anadromous population in Maine, is known as coaster trout or, simply, as coasters. The brook trout is the state fish of nine U.S. states: Michigan, New Hampshire, New Jersey, New York, North Carolina, Pennsylvania, Vermont, Virginia, and West Virginia, and the Provincial Fish of Nova Scotia in Canada. Systematics and taxonomy The brook trout was first scientifically described as ''Salmo fontinalis'' by the naturalist Samuel Latham Mitchill in 1814. The specific epithet "''fontina ...
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Lambdina Fiscellaria
''Lambdina fiscellaria'', the mournful thorn or hemlock looper, is a moth of the family Geometridae. It is found in North America, from the Pacific to the Atlantic coast and from Canada south to Pennsylvania, Wisconsin and California. The adult is grey to cream coloured with scalloped wing borders and resembles the oak besma. Darker line across forewings and hindwings, a second line across forewings. Area between lines may be shaded or unshaded. The wingspan is about 35 mm. The moth flies from August to early October depending on the location.Sogaard, Jim. (2009) Moths and Caterpillar of the North Woods. Duluth, MN:Kollath+Stensaas, p.53. The larvae feed on hemlock, balsam fir, white spruce, oak An oak is a tree or shrub in the genus ''Quercus'' (; Latin "oak tree") of the beech family, Fagaceae. There are approximately 500 extant species of oaks. The common name "oak" also appears in the names of species in related genera, notably ''L ... and other hardwoods. Sub ...
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Abies Balsamea
''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 West Virginia). Description Balsam fir is a small to medium-size evergreen tree typically tall, occasionally reaching a height of . The narrow conic crown consists of dense, dark-green leaves. The bark on young trees is smooth, grey, and with resin blisters (which tend to spray when ruptured), becoming rough and fissured or scaly on old trees. The leaves are flat and needle-like, long, dark green above often with a small patch of stomata near the tip, and two white stomatal bands below, and a slightly notched tip. They are arranged spirally on the shoot, but with the leaf bases twisted so that the leaves appear to be in two more-or-less horizontal rows on either side of the shoot. The needles become shorter and thicker the higher they ...
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Picea Mariana
''Picea mariana'', the black spruce, is a North American species of spruce tree in the pine family. It is widespread across Canada, found in all 10 provinces and all 3 territories. It is the official tree of the province of Newfoundland and Labrador and is that province's most numerous tree. The range of the black spruce extends into northern parts of the United States: in Alaska, the Great Lakes region, and the upper Northeast. It is a frequent part of the biome known as taiga or boreal forest.. The Latin specific epithet ''mariana'' means “of the Virgin Mary”. Description ''P. mariana'' is a slow-growing, small upright evergreen coniferous tree (rarely a shrub), having a straight trunk with little taper, a scruffy habit, and a narrow, pointed crown of short, compact, drooping branches with upturned tips. Through much of its range it averages tall with a trunk diameter at maturity, though occasional specimens can reach tall and diameter. The bark is thin, scaly, and ...
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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 deciduous forests of the southwest to the arctic tundra of the extreme north. Vegetation zones Quebec covers more than of land between 45° and 62° north, with vegetation that varies greatly from south to north. Most of the natural vegetation is forest, with various species of trees and other plants, and these forests are the habitat for diverse fauna. Energy, precipitation and soil are all important factors in determining what can grow. The climate influences the natural disturbances that affect forests: western Quebec has a drier climate than the east, and experiences more fires. For most species these disturbances are not disasters, and some need them to regenerate. The climate in Quebec supports rich deciduous forest in the southern region ...
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Ombrotrophic
Ombrotrophic ("cloud-fed"), from Ancient Greek ὄμβρος (''ómvros'') meaning "rain" and τροφή (''trofí'') meaning "food"), refers to Soil, soils or vegetation which receive all of their water and nutrients from precipitation, rather than from streams or springs. Such environments are hydrology, hydrologically isolated from the surrounding landscape, and since rain is acidic and very low in Plant nutrition, nutrients, they are home to organisms tolerant of acidic, low-nutrient environments. The vegetation of ombrotrophic peatlands is often bog, dominated by ''Sphagnum'' mosses. The hydrology of these environments are directly related to their climate, as precipitation is the water and nutrient source, and temperatures dictate how quickly water evaporates from these systems. Ombrotrophic circumstances may occur even in landscapes composed of limestone or other nutrient-rich substrates – for example, in high-rainfall areas, limestone boulders may be capped by acidic om ...
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Sheldrake River (Minganie)
The Sheldrake River (french: Rivière Sheldrake) is a river in the Côte-Nord region of Quebec, Canada. It flows into the Gulf of Saint Lawrence. There is a 25 MW hydroelectric power station on the river. Location The Sheldrake River rises between Lake Manitou and Lake Magpie in a mountainous area where the peaks reach heights of almost . The river flows south in a winding course of , with a series of waterfalls and rapids. The East Sheldrake River, a tributary, joins the main river about upstream from its mouth. It enters the Saint Lawrence to the west of the village of Sheldrake, halfway between Sept-Îles and Havre-Saint-Pierre. The entrance to the river is blocked to vessels of any size by a shifting sandbar and a steel bridge. The mouth of the river is in the municipality of Rivière-au-Tonnerre in the Minganie Regional County Municipality. P.J. Touzel, from Jersey, was the first European to settle on the Sheldrake in 1851, where he founded a large fishing stati ...
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