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Cub Hills
The Cub Hills are a hilly plateau located south-east of the geographical centre of the Canadian province of Saskatchewan. The hills are in the boreal forest ecozone of Canada and the landforms of the hills were shaped more than 10,000 years ago during last ice age. Throughout the Cub Hills, there are dozens of lakes and rivers and several parks. The Cubs Hills are north-east of Prince Albert and are in the Northern Saskatchewan Administration District and Census Division #18. Several highways criss-cross the plateau to provide access to the various parks and other amenities. The principle highway through the Cub Hills is Highway 106, also known as Hanson Lake Road, which begins at Smeaton and travels north into the hills then east to Flin Flon and the border with Manitoba. Other highways through the hills include Highways 120, 912, 913, and 920. Geography The glaciers retreated from the area about 10,000 years ago. And in their wake, they created many of the landfor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landform
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, Stratum, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic Waterbody, waterbodies and sub-surface features. Mountains, hills, Plateau, plat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rapid River (Churchill River Tributary)
The Rapid River is a short river in central Saskatchewan, Canada, about east of the community of Stanley Mission. It is part of the Churchill River drainage basin. The river is about long and flows north from Iskwatikan Lake, which lies downstream from Lac la Ronge, over the Nistowiak Falls, one of the tallest in Saskatchewan, and the Fisher Rapids, to Nistowiak Lake on the Churchill River, which flows to Hudson Bay. The entire river is within Lac La Ronge Provincial Park. Fish species The fish species in the river include: walleye, sauger, yellow perch, northern pike, lake trout, lake whitefish, cisco, white sucker, shorthead redhorse, longnose sucker, lake sturgeon and burbot. See also *List of rivers of Saskatchewan *Hudson Bay drainage basin The Hudson Bay drainage basin is the drainage basin in northern North America where surface water empties into Hudson Bay and adjoining waters. Spanning an area of about , the basin is almost totally in Canada (spanning pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Churchill River (Hudson Bay)
The Churchill River () is a major river in Alberta, Saskatchewan and Manitoba, Canada. From the head of the Churchill Lake it is long. It was named after John Churchill, 1st Duke of Marlborough and governor of the Hudson's Bay Company from 1685 to 1691. The Cree name for the river is ''Missinipi'', meaning "big waters". The Denesuline name for the river is ''des nëdhë́'', meaning "Great River". The river is located entirely within the Canadian Shield. The drainage basin includes a number of lakes in Central-East Alberta which flow into a series of lakes in Saskatchewan and Manitoba. The main tributary, the Beaver River, joins at Lac Île-à-la-Crosse. Nistowiak Falls—the tallest falls in Saskatchewan—are on the Rapid River, which flows north, out of Lac la Ronge into Nistowiak Lake on the Churchill just north of La Ronge. A large amount of flow of the Churchill River after Manitoba–Saskatchewan border comes from the Reindeer River, which flows from Wollas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lac La Ronge
Lac la Ronge is a glacial lake in the Canadian province of Saskatchewan. It is the fifth largest lake in the province and is approximately north of Prince Albert, on the edge of the Canadian Shield. La Ronge, Air Ronge, and the Lac La Ronge First Nation are on the western shore. The lake is a popular vacation spot. Recreational activities include fishing, boating, canoeing, hiking, and camping. Recreation and access Lac La Ronge Provincial Park extends around the lake on three sides, starting at La Ronge and ending along the east shore. The park contains four RV parks, two of which are on the west shore of the lake, one is in the town of Missinipe (Missinipe is the Woodland Cree name for the Churchill River which is on the south-west shore of Otter Lake, which flows through the north side of the park), and the fourth one is on the east shore of Nemeiben Lake. There is also a hunting and fishing lodge 26 km north of La Ronge. Nistowiak Falls, on the Rapid River, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nipekamew River
Nipekamew River is a river in the Canadian province of Saskatchewan. The river's source is Nipekamew Lake at the north-western edge of the Cub Hills and its mouth is in Nipekamew Bay at the southern shore of Lac la Ronge. From the northern tip of Nipekamew Lake, the river travels from south to north through muskeg and boreal forest en route to Lac la Ronge. Lake la Ronge empties north into the Churchill River through Rapid River. Nipekamew River is in the Northern Saskatchewan Administration District and the only highway to cross the river is Highway 165. Highway 912 parallels the river from Nipekamew Lake to Wapawekka Lake and Lac la Ronge. Adjacent to the mouth of the river is Fox Point Indian Reserve. The upper reaches of the river's watershed include East Trout Lake, tributaries from the hills of Clarence-Steepbank Lakes Provincial Park, Nipekamew Creek, and tributaries from the Cub Hills. Nipekamew Sand Cliffs Along the course of river are the provincially pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saskatchewan River
The Saskatchewan River ( Cree: ''kisiskāciwani-sīpiy'', "swift flowing river") is a major river in Canada. It stretches about from where it is formed by the joining together of the North Saskatchewan and South Saskatchewan Rivers to Lake Winnipeg. It flows roughly eastward across Saskatchewan and Manitoba to empty into Lake Winnipeg. Through its tributaries the North Saskatchewan and South Saskatchewan, its watershed encompasses much of the prairie regions of Canada, stretching westward to the Rocky Mountains in Alberta and north-western Montana in the United States. Including its tributaries, it reaches to its farthest headwaters on the Bow River, a tributary of the South Saskatchewan in Alberta. Description It is formed in central Saskatchewan, approximately east of Prince Albert, by the confluence of its two major branches, the North Saskatchewan and the South Saskatchewan, at the Saskatchewan River Forks. Both source rivers originate from glaciers in the Albert ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hudson Bay Drainage Basin
The Hudson Bay drainage basin is the drainage basin in northern North America where surface water empties into Hudson Bay and adjoining waters. Spanning an area of about , the basin is almost totally in Canada (spanning parts of the Prairies, central and northern Canada), with a small portion in the United States (in Montana, the Dakotas, and Minnesota). The watershed's connection to the Labrador Sea is at the Hudson Strait's mouth between Resolution Island in the Qikiqtaaluk Region and Cape Chidley on the Labrador Peninsula. The watershed's headwaters to the south-west are on the Continental Divide of the Americas, bounded at Triple Divide Peak to the south, and Snow Dome to the north. The western and northern boundary of the watershed is the Arctic Divide, and the southern and eastern boundary is the Laurentian Divide. left, Rupert's Land, granted as a commercial monopoly to the Hudson's Bay Company in 1670 Hudson Bay is often considered part of the Arctic Ocean. Fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muskeg
Muskeg (Ojibwe: mashkiig; cr, maskīk; french: fondrière de mousse, lit. ''moss bog'') is a peat-forming ecosystem found in several northern climates, most commonly in Arctic and boreal areas. Muskeg is approximately synonymous with bog or peatland, and is a standard term in Western Canada and Alaska. The term became common in these areas because it is of Cree origin; (ᒪᐢᑫᐠ) meaning low-lying marsh. Muskeg consists of non-living organic material in various states of decomposition (as peat), ranging from fairly intact sphagnum moss, to sedge peat, to highly decomposed humus. Pieces of wood can make up five to fifteen percent of the peat soil. The water table tends to be near the surface. The sphagnum moss forming it can hold fifteen to thirty times its own weight in water, which allows the spongy wet muskeg to also form on sloping ground. Muskeg patches are ideal habitats for beavers, pitcher plants, agaric mushrooms and a variety of other organisms. Composit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dead-ice
Dead ice is ice which, though part of a glacier or ice sheet, is no longer moving. When this melts it does so in situ, leaving behind a hummocky terrain known as dead-ice moraine which is produced by the deposition of glacio-fluvial sediments and ablation till. Such features include kettle holes. Landscapes forming Veiki moraine A Veiki moraine (Swedish: Veikimorän) is a type of moraine found in northern Sweden, Troms og Finnmark in Norway, and parts of Canada. This moraine is characterized by forming a hummocky landscape of irregular moraine plateaus with elevated ri ...s in northern Sweden and Canada have been attributed to the ablation of extensive bodies of till-covered dead ice. References Glaciology {{glaciology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kettle (landform)
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are fluvio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meltwater
Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater can be produced during volcanic eruptions, in a similar way in which the more dangerous lahars form. When meltwater pools on the surface rather than flowing, it forms melt ponds. As the weather gets colder meltwater will often re-freeze. Meltwater can collect or melt under the ice's surface. These pools of water, known as subglacial lakes can form due to geothermal heat and friction. Water source Meltwater provides drinking water for a large proportion of the world's population, as well as providing water for irrigation and hydroelectric plants. This meltwater can originate from seasonal snowfall, or from the melting of more permanent glaciers. Climate change threatens the precipitation of snow and the shrinking volume of glaciers. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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