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We’re a team of twenty-three web, digital marketing, SEO, and operations professionals. Heaviside Group was founded in 2011 as a side project and has continued to grow and expand year after year.
Our group is divided into four internal teams: Web, Digital Marketing, SEO, and Operations. Each team has specialists in those disciplines, and they work together to deliver projects accurately and on-time. Everything is managed by our operations team, which provides sales, customer service, and project management support to our clients.
In 2017, we launched our Heaviside Digital platform, designed to provide high-quality web, digital marketing, and SEO services to businesses with lower marketing budgets.
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An SEO firm can provide you with valuable organic rankings, but only if you work alongside them. If you attempt to create your own campaigns, it is highly likely that you will fail. The truth of the matter is that most of the online marketing strategies used today simply do not work. However, a good SEO company knows that marketing online requires tactics that are unique and effective. They will provide you with tactics that will drive more traffic to your site while building brand awareness that will make your online presence memorable.
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The Mdewakanton Dakota were the earliest inhabitants who came through the Minnesota River, following water fowl and game animals. As part of the greater migration of the Mdewakanton from their ancestral area around Mille Lacs Lake to the river confluence of the Minnesota and Mississippi Rivers, Chief Black Dog, around 1750, established his band at a permanent village at the isthmus between Black Dog Lake (from which is named after him) and the Minnesota River, near the present site of the Black Dog Power Plant. The permanent camp was reported by early settlers as being inhabited by over 250 Dakota. At the south end of Burnsville, Crystal Lake, recorded as "Minne Elk" was utilized for abundant fish, leisure and burial. It was also a gathering spot where Dakota watched deer or bucks drink at the lake from the top of Buck Hill, in which was named by early settlers who witnessed this activity. Three large burial mounds were discovered after European settlement.
The Dakota nation ceded land in 1851 and many relocated to Chief Shakopee's village—the current Shakopee-Mdewakanton Indian Reservation in nearby Prior Lake. The first European settlers were Irish, Scottish and Norwegian farmers who came upriver from Saint Paul. One of these Irish settlers was William Byrne, who had immigrated in 1840 from County Kilkenny, Ireland to Hamilton, Ontario, Canada. In 1855, he settled at the present day junction of County Road 34 and Judicial Road near the Scott County line, just southeast of old downtown Savage. He subsequently donated land there for a church, school, and a cemetery as well as serving Town Chairman. In 1858, the Dakota County Board authorized Byrnsville Township in the north by the Minnesota River, east by Eagan and Apple Valley, south by Lakeville, and west by Scott County. There is some ambiguity of if the name actually derived from William Byrne since there were people with the surname "Burns" living in the area (a Scottish variant). The Town Clerk recorded variations between "Burns" and "Byrnes" but at the 1960s city incorporation, the "Burnsville" spelling prevailed. The school district was organized during this time as well. Burnsville originally comprised the present-day downtown of Savage (then known as Hamilton) until county border revisions by the legislature. The Irish and Scottish settlers of this time left their names on many area roads and parks and their religion in Presbyterian, Protestant, and Catholic churches.
In the 19th century, Burnsville was considered a long distance from downtown Minneapolis. Rail access came in 1864 and Burnsville became a resort town, with cottages along Crystal Lake as well as Orchard Lake and Marion Lake in nearby Lakeville. The Bloomington Ferry provided river crossings until 1889 when the original Bloomington Ferry Bridge was built. By 1920, the Lyndale Avenue Drawbridge opened next to Black Dog Lake, extending Minneapolis' first north south highway to the rural communities of southern Minnesota. Later the bridge, upgraded several times, would be replaced by the I-35W Minnesota River bridge. In 1950, just before the World War II postwar housing boom, Burnsville was still a quiet township with a population of 583 people. School was taught in a one-room schoolhouse containing eight grades.
After the arrival of Interstate 35W in 1960, the next two decades saw the largest boom in population when post-war pressures forced the community to develop at rapid pace. Byrnesville Township was officially incorporated in 1964 after defeating an annexation attempt by the city of Bloomington. Mass housing development followed and a former mayor, Connie Morrison said city managers had foresight in producing shopping nodes in walking distance of most homes. The city became a regional pull when Burnsville Center opened in 1977 and produced the heavily traveled retail strip on County Road 42. The next decades leading to the 21st century dealt with managing Burnsville's increasing population and growth which led to providing alternative transportation options, diverse housing projects, and ultimately the "Heart of the City" project. The city approached build-out in the late 1990s and changed focus from new development to redevelopment and rehabilitation of existing structures.
Descendants of the Byrne family still remain in greater Minnesota with the original spelling in their surname. A relative who dedicated William Byrne Elementary in the 1960s considered petitioning to correct the spelling but most of the family had moved away for several decades.
The earliest settlers were roughly 250 Mdewakanton Dakota who lived permanently at Black Dog camp. Starting in the 1850s, Old stock Americans from the east coast and French Canadians moved into eastern Dakota County near Saint Paul. A decade later, major European immigration began with settlers from Ireland, Scotland, and Great Britain. By the 1900s there were a few Scandinavians from Sweden, Norway, and Denmark but these ethnic groups were mostly concentrated towards Lakeville. Those from Germany and Eastern Europe would gradually join the minority from the packing jobs in nearby South St. Paul. Irish descendants maintained the majority through the early 1950s owing to the town's origin, overall land ownership, and the practice of marrying within ethnic clans. The early 20th century's permanent population remained very low as the Minnesota River's lack of bridges and streetcar connection isolated the area from development, preventing people from moving south of the river. The lake-side houses around Crystal Lake and Orchard Lake however attracted several various immigrant and first-generation wealthier individuals to temporarily settle or own land in the town limits.
In 1960, the U.S. Census Bureau recorded the population of Byrnesville Township at 2,716 people and soon after, the postwar growth was instantaneous, filling the city with second to third generation European descendants from Minneapolis; more American than ethnic. From 1960 to 1970, the total population accelerated to nearly 20,000 people and by the year 2000, the population arrived at roughly 60,000 people.
As of the census of 2010, there were 60,306 people, 24,283 households, and 15,656 families residing in the city. The population density was 2,421.0 inhabitants per square mile (934.8/km2). There were 25,759 housing units at an average density of 1,034.1 per square mile (399.3/km2). The racial makeup of the city was 77.5% White, 10.0% African American, 0.4% Native American, 5.0% Asian, 0.1% Pacific Islander, 3.5% from other races, and 3.5% from two or more races. Hispanic or Latino of any race were 7.9% of the population.
There were 24,283 households, of which 32.1% had children under the age of 18 living with them, 48.4% were married couples living together, 11.5% had a female householder with no husband present, 4.6% had a male householder with no wife present, and 35.5% were non-families. 27.6% of all households were made up of individuals, and 8% had someone living alone who was 65 years of age or older. The average household size was 2.47 and the average family size was 3.03.
The median age in the city was 35.9 years. 110% of residents were under the age of 18; 9% were between the ages of 18 and 24; 28.6% were from 25 to 44; 26.7% were from 45 to 64; and 11.7% were 65 years of age or older. The gender makeup of the city was 48.7% male and 51.3% female.
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.