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Since the mid-19th century, Minnetonka has evolved from heavily wooded wilderness through extensive farming and thriving industrialization to its present primarily residential suburban character. The Minnetonka area was home to the Dakota and Ojibwe Native American tribes before Euro-Americans arrived in the 1800s. They believed Lake Minnetonka (mni meaning water, and tanka meaning big, anglicized to Minnetonka) and the land around it to be sacred. The first recorded exploration of the area by Euro-Americans was in 1822, when a group from newly constructed Fort Snelling made its way up Minnehaha Creek (then known as Brown's Creek or Falls Creek) to the lake. In 1851, the Dakota sold the area including Minnetonka to the United States with the Treaty of Traverse des Sioux. The first census, the Territorial Census of 1857, lists 41 households. Twenty-nine of the heads of households are listed as farmers. The occupations of the remaining twelve are associated with the operations of Minnetonka Mill and a nearby hotel.
In 1852, a claim was staked on Minnehaha Creek near McGinty Road. The sawmill that was constructed in the thick woods of maple, oak, elm, red cedar and basswood was the first privately operated mill in Minnesota west of the Mississippi River. Oak timbers from this mill were used to build the first suspension bridge across the Mississippi River at Saint Anthony Falls in 1853. The settlement of Minnetonka Mills that grew up around the mill was the first permanent European–American settlement west of Minneapolis in Hennepin County. In 1855, a two-story sawmill was constructed with a furniture factory on the second floor. A building for varnishing furniture was built on the south side of the creek, at the present Bridge Street. Production consisted mainly of chairs and bedsteads. The Minnetonka Republican at St. Anthony published a short article describing the area. The February 12, 1857, issue said:
In 1860, after only 8 years of operation, the sawmill closed. In 1869, a flour and grist mill were constructed and operated until the late 1880s. In 1874, Charles H. Burwell came to manage the Minnetonka Mill Company, and he built a Victorian home on the north bank of Minnehaha Creek (Minnetonka Boulevard at McGinty Road East) for his family. The Charles H. Burwell House is now on the National Register of Historic Places and is owned by the city. There were two other mills in Minnetonka. The St. Alban's Mill, which was less than 1 mile (2 km) downstream from Minnetonka Mills on Minnehaha Creek, operated as a flour mill from 1874 to 1881. A grist mill built on Purgatory Creek was washed out in a flood shortly after construction. Minnetonka Mills, with its post office and port for Lake Minnetonka, was the principal business and trading center for a large area until the 1870s.
Between 1883 and 1956, the area within the original 36-square-mile (93 km2) township grew smaller as Wayzata, Hopkins, Deephaven, Woodland and Saint Louis Park incorporated or annexed portions of then-Minnetonka Township.
As of the census of 2010, there were 49,734 people, 21,901 households, and 13,619 families living in the city. The population density was 1,846.8 inhabitants per square mile (713.1/km2). There were 23,294 housing units at an average density of 865.0 per square mile (334.0/km2). The racial makeup of the city was 90.0% White, 3.7% African American, 0.3% Native American, 3.1% Asian, 0.7% from other races, and 2.1% from two or more races. Hispanic or Latino of any race were 2.4% of the population.
There were 21,901 households, of which 25.9% had children under the age of 18 living with them, 52.1% were married couples living together, 7.3% had a female householder with no husband present, 2.8% had a male householder with no wife present, and 37.8% were non-families. 31.1% of all households were made up of individuals, and 11.9% had someone living alone who was 65 years of age or older. The average household size was 2.25 and the average family size was 2.85.
The median age in the city was 45 years. 20.8% of residents were under the age of 18; 6% were between the ages of 18 and 24; 23.2% were from 25 to 44; 33.3% were from 45 to 64; and 16.7% were 65 years of age or older. The gender makeup of the city was 47.5% male and 52.5% female.
As of the census of 2000, there were 51,301 people, 21,393 households, and 14,097 families living in the city. The population density was 1,893.0 persons per square mile (729.7/km2). There were 22,228 housing units at an average density of 818.9 per square mile (316.2/km2). The racial makeup of the city was 94.40% White, 1.50% African American, 0.20% Native American, 2.29% Asian, 0.03% Pacific Islander, 0.57% from other races, and 1.03% from two or more races. Hispanic or Latino of any race were 1.28% of the population. 24.7% were of German, 13.8% Norwegian, 9.1% Irish, 8.2% Swedish and 6.7% English ancestry.
There were 21,393 households, out of which 29.1% had children under the age of 18 living with them, 56.6% were married couples living together, 6.8% had a female householder with no husband present, and 34.1% were non-families. 27.3% of all households were made up of single individuals and 9.3% had someone living alone who was 65 years of age or older. The average household size was 2.37 and the average family size was 2.92.
In the city, the population was spread out, with 23.1% under the age of 18, 6.0% from 18 to 24, 28.5% from 25 to 44, 28.4% from 45 to 64, and 14.0% who were 65 years of age or older. The median age was 41 years. For every 100 females, there were 91.8 males. For every 100 females age 18 and over, there were 88.7 males.
According to the 2000 US Census, the median income for a household in the city was $83,437.
Minnesota is the state of Minnesota, a state which is bordered by the North & Western rivers and runs along the shoreline of Lake Vermillion. It is bordered on two sides by the Gulf of Minnesota and on the east by the North Dakota border. In modern times Minnesota is the largest county in Minnesota, lying along the western edge of the Minnesota River and bordered on the south by the Gulf of Minnesota and on the west by the North Dakota border. The major urban areas of Minneapolis & St. Paul are situated on the North side of the river while Omaha & Des Moines on the South side. Between these two large metropolitan areas are smaller rural areas such as Maple Lake, Shaklee, Shakope, Coon Rapids, and South Riding.
Minnesota is an extremely wealthy state. The median household income is around sixty-five thousand dollars and the per capita income is around fifteen thousand dollars. Demographics show that this level of wealth is at the very top of the national average. Minnesota has a low population density, which makes it one of the easiest states to politically and economically dominate when it comes to turnout and vote counting.
Geology indicates that Minnesota is made up of three major geological formations. The third formation, the Ice age formation, dates back to fourteen thousand years ago. During this time Minnesota was populated and developed into a state, but was not quite a modern nation until the eleven seventeenth century. During this time Minnesota was part of the fur trade and also was an important trading post for the Native Americans. Minnesota was also a significant role in North American wildlife history; as such, it has a significant fossil record.
The fourth major geological formation in Minnesota is glacial Lake Vermillion. This massive lake, formed from ice during the last Ice age, covered much of Minnesota and the rest of the upper Midwest. This massive lake allowed for easy transportation of ice to other areas of the country. It also left behind large amounts of sand and silt. The sand and silt have eroded away due to the seasonal weather, and there is now a sandy bed between the western edge of Minnesota and the southern end of Lake Vermillion. Sand and silt are very important for groundwater recharge and to monitor and regulate the water levels of lakes and rivers.
The fifth major geology fact is the existence of tundra. While Minnesota is far from the arctic, it does have some prominent tundra where plants and forests grow. This tundra includes the central part of Minnesota, a belt of southern Minnesota, the northern part of northeastern Minnesota, and the southern edge of southern Minnesota. Geologists believe that this tundra was important in the development of wildlife and plant species. Examples of plants that grow well in this area include conifers, alder, blueberries, blackberries, raspberries, and pinonwood.
Sixth, there is Minnesota's largest city, Minneapolis. There are many interesting sites including the Minneapolis Museum of Art, the Minneapolis Aquarium, Cityplace, the Minnesota Zoo, and the Minnesota Center for the Arts. In addition, it is also home to the state's largest university, the University of Minnesota.
The last major geology fact is the formation of Lake Calhoun. This lake lies in northern Minnesota, not far from the Twin Cities. It was formed by an ancient fracture in the Earth's crust. The fracture resulted in islands and Lake Calhoun. Some islands have disappeared and some lakes have become too acidic and are no longer suitable for fish or other wildlife populations.
Geology is an important subject for students studying the Northwoods. Learning about Minnesota's geology helps them learn more about nature and its delicate relationship with man. In order to understand Minnesota, it is necessary to explore the landscape and how each geological formation is formed. Studying Minnesota's geology will give students an idea of how we got here and why we're here. It will also help them better appreciate all that is beautiful and natural in our world.