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Longville, Minnesota
Longville is a city in Cass County, Minnesota, United States. The population was 156 at the 2010 census. The city was named after its founder, Jim Long. It is roughly four hours north of the Twin Cities. It is part of the Brainerd Micropolitan Statistical Area. Minnesota State Highway 84 serves as a main route in the community, and Minnesota State Highway 200 is nearby. Longville is home to Longville Municipal Airport. Geography According to the United States Census Bureau, the city has an area of , of which is land and is water. Longville is part of the Northern Minnesota's glacial plain, which was flattened by glaciers during the most recent glacial advance. During the last glacial period, massive ice sheets at least thick ravaged the state's landscape and sculpted its terrain. The Wisconsin glaciation left 12,000 years ago. These glaciers covered all of Minnesota except the far southeast, an area characterized by steep hills and streams that cut into the bedrock. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
City
A city is a human settlement of notable size.Goodall, B. (1987) ''The Penguin Dictionary of Human Geography''. London: Penguin.Kuper, A. and Kuper, J., eds (1996) ''The Social Science Encyclopedia''. 2nd edition. London: Routledge. It can be defined as a permanent and densely settled place with administratively defined boundaries whose members work primarily on non-agricultural tasks. Cities generally have extensive systems for housing, transportation, sanitation, utilities, land use, production of goods, and communication. Their density facilitates interaction between people, government organisations and businesses, sometimes benefiting different parties in the process, such as improving efficiency of goods and service distribution. Historically, city-dwellers have been a small proportion of humanity overall, but following two centuries of unprecedented and rapid urbanization, more than half of the world population now lives in cities, which has had profound consequences for g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Minnesota State Highway 84
Minnesota State Highway 84 (MN 84) is a highway in north-central Minnesota, which runs from its intersection with Highway 371 in Pine River and continues north to its northern terminus at its intersection with State Highway 200 in Kego Township, four miles north of Longville. The route is two lanes throughout except for a small portion in Pine River near its southern terminus at Highway 371. The route is a winding road with several sharp turns of or less. Route description State Highway 84 serves as a north–south route between the communities of Pine River and Longville in north-central Minnesota. The highway passes through the Chippewa National Forest Chippewa National Forest is a National Forest located in north central Minnesota, United States, in the counties of Itasca, Cass and Beltrami. Forest headquarters are located in Cass Lake, Minnesota. There are local ranger district offices i ... between Longville and State Highway 200. Highway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assiniboine People
The Assiniboine or Assiniboin people ( when singular, Assiniboines / Assiniboins when plural; Ojibwe: ''Asiniibwaan'', "stone Sioux"; also in plural Assiniboine or Assiniboin), also known as the Hohe and known by the endonym Nakota (or Nakoda or Nakona), are a First Nations/Native American people originally from the Northern Great Plains of North America. Today, they are centred in present-day Saskatchewan. They have also populated parts of Alberta and southwestern Manitoba in Canada, and northern Montana and western North Dakota in the United States. They were well known throughout much of the late 18th and early 19th century, and were members of the Iron Confederacy with the Cree. Images of Assiniboine people were painted by 19th-century artists such as Karl Bodmer and George Catlin. Names The Europeans and Americans adopted names that other tribes used for the Assiniboine; they did not until later learn the tribe's autonym, their name for themselves. In Siouan, they traditi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sioux
The Sioux or Oceti Sakowin (; Dakota language, Dakota: Help:IPA, /otʃʰeːtʰi ʃakoːwĩ/) are groups of Native Americans in the United States, Native American tribes and First Nations in Canada, First Nations peoples in North America. The modern Sioux consist of two major divisions based on Siouan languages, language divisions: the Dakota people, Dakota and Lakota people, Lakota; collectively they are known as the Očhéthi Šakówiŋ ("Seven Council Fires"). The term "Sioux" is an exonym created from a French language, French transcription of the Ojibwe language, Ojibwe term "Nadouessioux", and can refer to any ethnic group within the Great Sioux Nation or to any of the nation's many language dialects. Before the 17th century, the Dakota people, Santee Dakota (; "Knife" also known as the Eastern Dakota) lived around Lake Superior with territories in present-day northern Minnesota and Wisconsin. They gathered wild rice, hunted woodland animals and used canoes to fish. Wars ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ojibwe
The Ojibwe, Ojibwa, Chippewa, or Saulteaux are an Anishinaabe people in what is currently southern Canada, the northern Midwestern United States, and Northern Plains. According to the U.S. census, in the United States Ojibwe people are one of the largest tribal populations among Native American peoples. In Canada, they are the second-largest First Nations population, surpassed only by the Cree. They are one of the most numerous Indigenous Peoples north of the Rio Grande. The Ojibwe population is approximately 320,000 people, with 170,742 living in the United States , and approximately 160,000 living in Canada. In the United States, there are 77,940 mainline Ojibwe; 76,760 Saulteaux; and 8,770 Mississauga, organized in 125 bands. In Canada, they live from western Quebec to eastern British Columbia. The Ojibwe language is Anishinaabemowin, a branch of the Algonquian language family. They are part of the Council of Three Fires (which also include the Odawa and Potawatomi) and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Indigenous Peoples
Indigenous peoples are culturally distinct ethnic groups whose members are directly descended from the earliest known inhabitants of a particular geographic region and, to some extent, maintain the language and culture of those original peoples. The term ''Indigenous'' was first, in its modern context, used by Europeans, who used it to differentiate the Indigenous peoples of the Americas from the European settlers of the Americas and from the Sub-Saharan Africans who were brought to the Americas as enslaved people. The term may have first been used in this context by Sir Thomas Browne in 1646, who stated "and although in many parts thereof there be at present swarms of ''Negroes'' serving under the ''Spaniard'', yet were they all transported from ''Africa'', since the discovery of ''Columbus''; and are not indigenous or proper natives of ''America''." Peoples are usually described as "Indigenous" when they maintain traditions or other aspects of an early culture that is assoc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woman Lake
Woman Lake is a lake in Cass County, Minnesota, United States. The lake has 3 public accesses. The lake is part of a 4 lake chain called the Woman Lake Chain. Other lakes in the chain include Child Lake, Girl Lake and Little Woman Lake. The town of Longville, Minnesota can be accessed by boat from Woman Lake. The lake is very well known for its impressive Walleye, Northern, Perch, Smallmouth Bass and Muskie fishing. The lake is stocked by the Minnesota Department of Natural Resources. In the game NASCAR: Dirt To Dayton, one of the sponsors for the truck racing series is called Schneider Boats. The address on the letter you receive from them is Woman Lake MN. It is a fictional company, one of many Minnesota references in the game. Woman Lake was named in commemoration of Ojibwe women who were killed there in a battle against the Sioux. Fishing Woman lake has always been known for its Walleye fishing. The lake also has a very good population of Yellow perch, Northern pike, La ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Post-glacial Rebound
Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy), the deformation of the Earth's crust in response to changes in ice mass distribution. The direct raising effects of post-glacial rebound are readily apparent in parts of Northern Eurasia, Northern America, Patagonia, and Antarctica. However, through the processes of ''ocean siphoning'' and ''continental levering'', the effects of post-glacial rebound on sea level are felt globally far from the locations of current and former ice sheets.Milne, G.A., and J.X. Mitrovica (2008) ''Searching for eustasy in deglacial sea-level histories.'' Quaternary Science Reviews. 27:2292–2302. Overview During the last glacial period, much of northern Eu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bedrock
In geology, bedrock is solid Rock (geology), rock that lies under loose material (regolith) within the crust (geology), crust of Earth or another terrestrial planet. Definition Bedrock is the solid rock that underlies looser surface material. An exposed portion of bedrock is often called an outcrop. The various kinds of broken and weathered rock material, such as soil and subsoil, that may overlie the bedrock are known as regolith. Engineering geology The surface of the bedrock beneath the soil cover (regolith) is also known as ''rockhead'' in engineering geology, and its identification by digging, drilling or geophysics, geophysical methods is an important task in most civil engineering projects. Superficial deposition (geology), deposits can be very thick, such that the bedrock lies hundreds of meters below the surface. Weathering of bedrock Exposed bedrock experiences weathering, which may be physical or chemical, and which alters the structure of the rock to leave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wisconsin Glaciation
The Wisconsin Glacial Episode, also called the Wisconsin glaciation, was the most recent glacial period of the North American ice sheet complex. This advance included the Cordilleran Ice Sheet, which nucleated in the northern North American Cordillera; the Innuitian ice sheet, which extended across the Canadian Arctic Archipelago; the Greenland ice sheet; and the massive Laurentide Ice Sheet, which covered the high latitudes of central and eastern North America. This advance was synchronous with global glaciation during the last glacial period, including the North American alpine glacier advance, known as the Pinedale glaciation. The Wisconsin glaciation extended from approximately 75,000 to 11,000 years ago, between the Sangamonian Stage and the current interglacial, the Holocene. The maximum ice extent occurred approximately 25,000–21,000 years ago during the last glacial maximum, also known as the ''Late Wisconsin'' in North America. This glaciation radically altered the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial History Of Minnesota
The glacial history of Minnesota is most defined since the onset of the last glacial period, which ended some 10,000 years ago. Within the last million years, most of the Midwestern United States and much of Canada were covered at one time or another with an ice sheet. This continental glacier had a profound effect on the surface features of the area over which it moved. Vast quantities of rock and soil were scraped from the glacial centers to its margins by slowly moving ice and redeposited as drift or till. Much of this drift was dumped into old preglacial river valleys, while some of it was heaped into belts of hills (terminal moraines) at the margin of the glacier. The chief result of glaciation has been the modification of the preglacial topography by the deposition of drift over the countryside. However, continental glaciers possess great power of erosion and may actually modify the preglacial land surface by scouring and abrading rather than by the deposition of the drift. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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