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  1. The history of the U.S. state of Minnesota is shaped by its original Native American residents, European exploration and settlement, and the emergence of industries made possible by the state's natural resources. Early economic growth was based on fur trading, logging, milling and farming, and later through railroads and iron mining.

    • Overview
    • Relief
    • Drainage
    • Soils
    • Climate

    Minnesota, constituent state of the United States of America. It became the 32nd state of the union on May 11, 1858. A small extension of the northern boundary makes Minnesota the most northerly of the 48 conterminous U.S. states. (This peculiar protrusion is the result of a boundary agreement with Great Britain before the area had been carefully surveyed.) Minnesota is one of the north-central states. It is bounded by the Canadian provinces of Manitoba and Ontario to the north, by Lake Superior and the state of Wisconsin to the east, and by the states of Iowa to the south and South Dakota and North Dakota to the west.

    Minnesota’s thousands of rivers flow northward via the Red and Rainy rivers to Hudson Bay, eastward through the Great Lakes to the Atlantic Ocean, and southward through the Mississippi River to the Gulf of Mexico. Indeed, Minnesota received its name from the Dakota (Sioux) word for the Mississippi’s major tributary in the state, the Minnesota River, which means “sky-tinted water.”

    Minnesota’s terrain stretches from the edge of a subarctic forest to the heart of the Corn Belt. Most of the state was covered by glaciers several times, and the land’s surface was shaped by the alternate freezing, thawing, and movement of those glaciers. Prominent geomorphic reminders of this glacial activity are the rolling farmlands, thousands of lakes, steep hillsides, and flat glacial lake and outwash plains that make up Minnesota’s present-day landscape. The state’s rich prairie soils developed on the finely ground mineral materials left by the retreating glaciers. Minnesota’s elevations range from 602 feet (184 metres) above sea level at Lake Superior to 2,301 feet (701 metres) above sea level at Eagle Mountain, located about 12 miles (19 km) from the lake’s north shore.

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    The majority of Minnesota’s lakes are located in the areas of glacial moraine, where glaciers deposited hills of sand and gravel. Lakes more than 100 square miles (260 square km) in area include Red Lake, Mille Lacs Lake, Leech Lake, Lake Winnibigoshish, Lake of the Woods, and Rainy Lake. The shoreline of Lake Superior, one of the largest freshwater lakes in the world, forms the state’s northeastern border for some 160 miles (260 km). In northeastern Minnesota there are stream valleys and deep, clear lakes that were scoured by glaciers from the granite bedrock.

    The largest glacial lake plain (more than 100,000 square miles [260,000 square km]) was formed by Lake Agassiz, which held the meltwaters as the latest glaciers retreated northward some 8,000 years ago. The southern part of the former lake bed lies along the Minnesota–North Dakota border and is known as the Red River valley. Red Lake, Lake of the Woods, and Canada’s Lake Winnipeg are all remnants of this huge body of glacial meltwater. Its southward drainage created the wide valley of the Minnesota River, the flow of which eventually reversed as ice blockage to the north melted.

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    The most fertile soils in Minnesota formed beneath the original grasslands of the south and west and are rich in organic matter and soluble minerals. Soils that formed under the original coniferous forest in northeastern Minnesota are light-coloured, acidic, and low in organic matter. Those that formed under the original hardwood forest, which occu...

    Temperature variations in Minnesota occur not only seasonally but also from one part of the state to another. Southern Minnesota is hot in the summer. In the northern regions of the state, frost is possible in any month.

    Average daily maximum temperatures in July range from the mid-80s F (about 29 °C) in southern Minnesota to the low 70s F (about 21 °C) along the shore of Lake Superior. Average daily January highs range from the mid-20s F (about −4 °C) in the south to about 15 °F (−9 °C) in the north; minimums are from about 5 °F (−15 °C) to about −5 °F (−21 °C). Record-breaking lows have been known to occur; in 1996 a temperature of −60 °F (−51 °C) was recorded near the northeastern city of Tower. The average frost-free periods vary from fewer than 90 days in parts of the north to more than 160 days in parts of the south.

  2. 5 days ago · Early history. Minnesota: Pipestone National Monument Quarries in Pipestone National Monument, southwestern Minnesota. Until the middle of the 19th century, two major peoples occupied what is now Minnesota: the Ojibwa (also called Chippewa or Anishinaabe) in the north and east and the Dakota (Sioux) in the south and west.

  3. Nov 9, 2009 · The first people arrived in the area now known as Minnesota around 12,000 years ago. By the 1600s, two main Indigenous groups lived in Minnesota: the Dakota and the Anishinaabe. They relied...

  4. Great Britain wins claim to what is now eastern North America (east of the Mississippi River) and Canada. 1770-1804. Grand Portage (Minnesota) evolves into the western fur-trading headquarters of the British Empire in North America.

  5. en.wikipedia.org › wiki › MinnesotaMinnesota - Wikipedia

    Minnesota, which gets its name from the Dakota language, has been inhabited by various Native Americans since the Woodland period of the 11th century BCE. Between roughly 200 and 500 CE, two areas of the indigenous Hopewell tradition emerged: the Laurel complex in the north, and Trempealeau Hopewell in the Mississippi River Valley in the south.

  6. The Minnesota Territory, established in 1849, included present-day Minnesota and the eastern sections of North and South Dakota. Minnesota became the 32nd U.S. state in 1858. The Sioux Uprising in southern Minnesota in 1862 resulted in the death of more than 500 civilians, soldiers, and Dakota.

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