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Katepwa, Saskatchewan
Katepwa ( 2016 population: ) is a resort village in the Canadian province of Saskatchewan within Census Division No. 6. It is on the eastern and southern shores of Katepwa Lake in the Rural Municipality of Abernethy No. 186. The name ''Katepwa'' likely comes from the Cree word ''Kahtapwao'' meaning "What is calling?" The name was given to the last in the chain of four lakes, Katepwa Lake. Legend has it that spirits inhabited the shores of the lake and First Nation people would hear voices on the lake. The Resort Village of the District of Katepwa was incorporated on July 24, 2004. Its incorporation was the result of the amalgamation of three separate resort villages – Katepwa Beach, Katepwa South and Sandy Beach. Katepwa Beach and Katepwa South originally incorporated as a resort villages on August 1, 1957 and January 1, 1990 respectively. History The Qu'Appelle Valley was formed approximately 14,000 years ago as retreating glaciers and their meltwater sculpted the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Resort Villages In Saskatchewan
A resort village is a type of incorporated List of communities in Saskatchewan#Urban municipalities, urban municipality in the Provinces and territories of Canada, Canadian province of Saskatchewan. A resort village is created from an organized Hamlet (place), hamlet by the Minister of Municipal Affairs by ministerial order via section 51 of ''The Municipalities Act'' if the community has: *been an organized hamlet for three or more years; *a population of 100 or more; *50 or more dwellings or businesses; and *a taxable assessment base that meets a prescribed minimum. Saskatchewan has 40 resort villages that had a cumulative population of 4,118 and an average population of 103 in the Canada 2011 Census, 2011 Census. Saskatchewan's largest and smallest resort villages are Candle Lake (Saskatchewan), Candle Lake and the Lumsden Beach, Saskatchewan, Lumsden Beach with populations of 765 and 10 respectively. A resort village council may request the Minister of Municipal Aff ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Saskatchewan Provincial Highways
This is a list of Saskatchewan's highways: Only Highways 1, 2, 5, 6, 7, 11, 12, 16, and 39 contain sections of divided highway. Speed limits range from 90 km/h (55 mph) to 110 km/h (70 mph). Saskatchewan is the only province bordering the United States with no direct connection to the Interstate Highway System. Named routes * Can Am Highway *Circle Drive *Hanson Lake Road * Little Swan Road *Louis Riel Trail * McBride Lake Road *Northern Woods and Water Route * Ring Road *Red Coat Trail *Regina Bypass *Saskatoon Freeway * Saskota Travel Route * Trans-Canada Highway * Veterans Memorial Highway * Yellowhead Highway Primary (1–99) These are primary highways maintained by the provincial government. Almost all of these highways are paved for most of their length. Highways 1, 11, and 16 are the most important highways and are divided highways for much of their lengths, with some sections at expressway or freeway standards. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pasqua Lake
Pasqua Lake is a lake along the course of the Qu'Appelle River in the Canadian province of Saskatchewan. Pasqua Lake was named after Chief Joseph Pasqua who formed what became the Pasqua First Nation. It is one of four lakes that make up the Fishing Lakes, which are all nestled in the Qu'Appelle Valley. The deep-cut Qu'Appelle Valley was formed about 14,000 years ago during the last ice age as meltwater from the glaciers carved out the valley. As water levels rose and fell, alluvium was left in the wake. These piles of alluvium are what created the separations between the lakes. Pasqua Lake is the farthest west and upstream of the four Fishing Lakes. The Qu'Appelle River enters the lake at the far western end and exits the lake at the eastern end through Sioux Crossing. Sioux Crossing is a short channel cut through the isthmus that separates Pasqua from Echo Lake. While the Qu'Appelle River is the primary inflow for the lake, other smaller creeks flow into the lake from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fishing Lakes
The Fishing Lakes, also called the Calling Lakes or the Qu'Appelle Lakes, are a chain of four lakes in the Qu'Appelle Valley cottage country about 40 miles (64 km) to the north-east of Regina in the Canadian province of Saskatchewan. The lakes are in a region called the Prairie Pothole Region of North America, which extends throughout three Canadian provinces and five U.S. states. It is also within Palliser's Triangle and the Great Plains ecoregion. The Fishing Lakes all follow the course of the Qu'Appelle River, which flows from the west to the east and is part of the Hudson Bay drainage basin. The lakes sit in the deep-cut Qu'Appelle Valley that was formed about 14,000 years ago during the last ice age. Meltwater from the glaciers carved out the valley and as water levels rose and fell, alluvium was left in the wake. These piles of alluvium are what created the separations between the lakes. The name ''Qu'Appelle'' is French for "Who's calling?" The name comes fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water (fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain shape, and c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...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 Several types of volcanic eruptions—during which lava, tephra (ash, lapilli, volcanic bombs and volcanic blocks), and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists. These are often ..., 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 pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qu'Appelle Valley
The Qu'Appelle River is a river in the Canadian provinces of Saskatchewan and Manitoba that flows east from Lake Diefenbaker in south-western Saskatchewan to join the Assiniboine River in Manitoba, just south of Lake of the Prairies, near the village of St. Lazare. It is located in a region called the Prairie Pothole Region of North America, which extends throughout three Canadian provinces and five U.S. states. It is also within Palliser's Triangle and the Great Plains ecoregion. With the construction of the Qu'Appelle River Dam and Gardiner Dam upstream, water flow was significantly increased and regulated. Most of the Qu'Appelle's present flow is actually water diverted from the South Saskatchewan River. Upper and lower watersheds According to the Saskatchewan Water Security Agency, the Qu'Appelle Valley is made up of two watersheds with the dividing point being Craven Dam on the east side of Craven: Lower Qu'Appelle Watershed The Lower Qu'Appelle Valley is locate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Statistics Canada
Statistics Canada (StatCan; french: Statistique Canada), formed in 1971, is the agency of the Government of Canada commissioned with producing statistics to help better understand Canada, its population, resources, economy, society, and culture. It is headquartered in Ottawa.Statistics Canada, 150 Tunney's Pasture Driveway Ottawa, Ontario K1A 0T6; Statistique Canada 150, promenade du pré Tunney Ottawa, Ontario K1A 0T6 The agency is led by the chief statistician of Canada, currently Anil Arora, who assumed the role on September 19, 2016. StatCan is responsible to Parliament through the Minister of Innovation, Science and Industry, currently François-Philippe Champagne. Statistics Canada acts as the national statistical agency for Canada, and Statistics Canada produces statistics for all the provinces as well as the federal government. In addition to conducting about 350 active surveys on virtually all aspects of Canadian life, the '' Statistics Act'' mandates that Statistic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandy Beach, Saskatchewan
Sandy Beach ( 2006 population: ) is a former resort village in the Canadian province of Saskatchewan within Census Division No. 6. It is now part of the District of Katepwa. Sandy Beach is on the eastern shore of Katepwa Lake in the Rural Municipality of Abernethy No. 186, approximately south-east of the town of Fort Qu'Appelle on Highway 56. History Sandy Beach originally incorporated as a resort village in 1954. It, and the resort villages of Katepwa Beach and Katepwa South, amalgamated on July 24, 2004 to form the Resort Village of the District of Katepwa. Demographics In the 2006 Census of Population conducted by Statistics Canada, the former Resort Village of Sandy Beach recorded a population of living in of its total private dwellings, a change from its 2001 population of . With a land area of , it had a population density of in 2006. In the 2001 Census of Population, the Resort Village of Sandy Beach recorded a population of , a change from its 199 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Katepwa South
Katepwa South ( 2006 population: ) is a former resort village in the Canadian province of Saskatchewan within Census Division No. 6. It is now part of the District of Katepwa. Katepwa South is on the southwest shore of Katepwa Lake in the Rural Municipality of Abernethy No. 186, approximately southeast of the Town of Fort Qu'Appelle on Highway 56. History Katepwa South incorporated as a resort village on January 1, 1990. It, and the resort villages of Katepwa Beach and Sandy Beach, amalgamated on July 24, 2004 to form the Resort Village of the District of Katepwa. Demographics In the 2006 Census of Population conducted by Statistics Canada, the former Resort Village of Katepwa South recorded a population of living in of its total private dwellings, a change from its 2001 population of . With a land area of , it had a population density of in 2006. In the 2001 Census of Population, the Resort Village of Katepwa South recorded a population of , a change ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
