The North Shore of Lake Superior runs from Duluth, Minnesota, United States, at the western end of the lake, to Thunder Bay and Nipigon, Ontario, Canada, in the north, to Sault Ste. Marie, Ontario in the east. The shore is characterized by alternating rocky cliffs and cobblestone beaches, with forested hills and ridges through which scenic rivers and waterfalls descend as they flow to Lake Superior.
Lake Superior was settled by Native Americans about 8000 BC when the Wisconsin Glaciers began to recede. By 500 BC the Laurel people had established settlements in the area and had begun to trade metal with other native peoples. The Laurel people were animists and probably created many of the pictographs present on rock faces along the North Shore and other Canadian rock faces in order to communicate with spirits.
In the 12th century, on the easternmost portion of the North Shore, the ancestors of the Ojibwa migrated into the area. These people left behind small pits dug in the ground which archaeologists now call Pukaskwa Pits. On the Minnesota portion of the North Shore there are only three archaeological sites, and it is not known who dug them.[ citation needed ]
By the 18th century the Ojibwa had settled the length of the North Shore approximately as far as the modern Canadian–Minnesota Border. The Minnesota portion of the North Shore was settled mostly by the Cree and the Dakota lived to the south.
The first white explorer to reach Lake Superior was Frenchman Étienne Brûlé who was sent out by Samuel de Champlain to search for the Northwest Passage in 1623 or 1624. [1] His exploration allowed Champlain to create the first map of the lake in 1632. [1]
Charles Raymbault and Isaac Jogues, Jesuit missionaries, were the next significant explorers, who tried to establish a more permanent missionary post further west but only got as far as Sault Ste. Marie. [2] In 1658 two French explorers, Pierre-Esprit Radisson and Médard des Groseilliers, became the first whites to circumnavigate Lake Superior by sailing south along the North Shore. When they returned, they brought a flotilla of Native Americans with fur pelts, beginning interest in the fur trade in the Lake Superior region.
Conflicts between native tribes began to escalate toward war during this period when an alliance of Anishinaabe tribes was formed and defeated the Dakota in a battle west of Sault Sainte Marie in 1662. This warfare between the tribes along Lake Superior prevented European trade in the area for several years.
In 1670, the Hudson's Bay Company was founded, which began the fur trade nonetheless. In the late 1670s, Daniel Greysolon, Sieur du Lhut, helped negotiate a more permanent peace between these tribes, thus providing safe trade across Lake Superior for the French. With this, the foundations for European settlement on the North Shore were laid. Fort Kaministiquia, around modern Thunder Bay, was established in 1683. In 1688 Jacques de Noyon became the first European to visit the present-day Boundary Waters Canoe Area region west of Lake Superior.
A war[ which? ] between Britain and France, followed by a sharp drop in fur prices, slowed exploration for several decades. In 1732 the French-Canadian La Vérendrye built Fort St. Pierre on Rainy Lake near the head of the Rainy River in order to gain access to the west.
In 1763 according to the terms of the Treaty of Paris, the British took possession of all French holdings east of the Mississippi River, including the North Shore. In 1784 the North West Company, the newly organized rival to the Hudson's Bay Company, started moving traders into its new fort at Grand Portage. With new headquarters on the North Shore, the North West Company began to build 40 new forts and ports all along the North Shore and northern Minnesota. In 1821 the North West Company was forced to merge with the Hudson's Bay Company.
With the eventual depletion of fur-bearing animals, the fur trade and associated settlement diminished.
When American settlers moved westward, the governments of the United States and Britain began to dispute the border between the territory that would become Minnesota and the territory which would become Ontario in future years. Many geologic surveys were taken because of these disputes, which revealed the rich mineral resources in this area. In 1854 the LaPointe Treaty surrendered all Ojibwa lands to the United States government.
Because of this white settlers moved into the region in order to mine the natural resources, thus beginning American settlements on the Minnesotan portion of the North Shore. Land claims were made near modern Duluth, Knife River, Beaver Bay, Buchanan, Burlington Bay, French River, Stewart River and Silver Creek. Ninety-nine fishermen had settled in northern Minnesota by 1857, when an economic panic caused most of the claims to be abandoned. In 1865 the Vermilion Lake Gold Rush brought a new wave of settlement to the North Shore.
American settlement began in earnest in 1869. When the Lake Superior & Mississippi Railroad was built, people could move across the country in days instead of months. In 1869 Duluth grew from 14 families in January to a population of 3,500 in July. Construction on the Duluth Harbor was begun to allow steamboat shipping between Duluth, Buffalo, Detroit, and Chicago. The town of Beaver Bay was founded in 1869 as a fishing community, and Grand Marais was founded by Henry Mayhew and Sam Howenstine in 1871. Another panic in 1873 put an end to this growth, and Duluth shrank to a population of 1,300.
In the 1880s, growth began again in Minnesota, and significant growth began for the first time in Canada. The Canadian Pacific Railway was opened in 1881 and brought a wave of settlers from the west. In Minnesota, Two Harbors was founded and became a major iron ore port and a source of labor for the inland iron mines on the North Shore. Besides mining, fishing became the other major industry of North Shore communities. In 1885, 195 commercial fishermen lived in Duluth. Duluth fish catches increased to a peak of 10,000 tons of fish caught in 1915. It has since declined. Current annual fish catches have fallen to under 1,000 tons per year.
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In 1875 Philadelphia financier Charlemagne Tower, who owned extensive interests in the Northern Pacific Railroad, began to investigate the possibility of iron mining inland from the North Shore. (Vast quantities of banded iron formations had been deposited about 2,000 million years ago in the Animikie Group.) Although the scare of 1873 had depressed the price of iron to $5.50 per ton, by the 1880s it was back to about $9.25 per ton. Tower started acquiring land in the Vermilion Range, where ore had an iron content of 69%. Tower also acquired the rights to the Duluth Iron & Railway Co., which entitled him to 10 square miles (26 km2) of land for every mile (1.6 km) of rail built between Duluth and Agate Bay (Two Harbors), 25 miles (40 km) northeast along the shore.
Speculators bought up land at Agate Bay; the rail line was not completed until 1887, so all travel to Agate Bay was originally by steamboat. Between 1884 and 1885 two large wooden loading docks were built in the harbor for shipping iron. In 1887, when the railroad was completed, the Minnesota Iron Company owned 95.7 miles (154.0 km) of track, 26,800 acres (108 km2) of property, 13 locomotives, 340 cars, the loading docks at Two Harbors and five pit mines.
This growth attracted the interest of Henry H. Porter, a Chicago railroad owner. He bought 25,000 acres (100 km2) of land further up the North Shore than Tower’s holdings around Two Harbors and Tower, an inland mining settlement named after its founder. Porter coerced Tower into selling the Minnesota Iron Company for 8.5 million dollars. He opened Chandler Mine, Pioneer Mine, Zenith Mine, Savoy Mine and Sibley Mine between 1889 and 1899. In 1896 the iron traveling through Two Harbors exceeded 2,000,000 tons. Two Harbors steadily built more docks and replaced the wooden docks with concrete over the course of the next several decades.
Iron production continued steadily for many more decades; by the 1950s traditional iron mines had exhausted most of their resources. It had been known for many years that northern Minnesota had an ore called taconite, which could be refined into iron through a process called beneficiation. A taconite processing plant was built further north along the North Shore at Silver Bay, and it quickly became the major taconite shipping port. Minnesota taconite produces over half of the iron mined in Minnesota at the present date.
Northern Minnesota is essentially covered with one large forest. Although the potential for a lumber industry was recognized early in the course of European settlement, the distances that it would have to be shipped made it uneconomical. But as eastern forests were logged out, the lumber industry moved into Wisconsin and Minnesota.. Lumber and forest products were shipped by rail from Duluth and Superior, Wisconsin to southern and eastern mills. Because of conservation efforts, many of the forests along the North Shore are now protected from deforestation, but there is still a strong paper industry that relies on pulpwood.[ citation needed ]
In 1855 when a lock system first allowed steamboats onto the lake, eastern tourists began to travel onto Lake Superior for recreational purposes. They would then canoe or be ferried from Duluth up the North Shore and would stay in hunting and fishing camps.
In the 1920s, the North Shore highway was built, which helped make the North Shore accessible by land. At the same time commercial fishermen began to go out of business as catches declined. Many of these fishermen built cabins and resorts, which were inhabited by more rich people on recreational trips. Certain exclusive clubs also bought land for resort and sport purposes. The Naniboujou Club Lodge was built to attract an exclusive clientele, and a group of Duluth businessmen, the Tettegouche Club, bought 9,346 acres (37.8 km2) of land for use as a private retreat.
During the early 20th century, the government decided that continued exploitation of the North Shore would destroy it. In 1909 President Teddy Roosevelt organized the Superior National Forest, putting over 3-million acres (12,000 km2) of the forests between the North Shore and the Canada–US border under protection. The government of Minnesota slowly began to acquire the lands which became the modern North Shore state parks. The first park to be formally organized was Jay Cooke State Park in 1915. In the 1930s the Civilian Conservation Corps established several camps organized along the North Shore and built rustic structures in what would become several North Shore state parks.
Today the North Shore Scenic Drive remains a popular tourist route, starting at the historic Glensheen Mansion, passing several state parks, all the way to Grand Portage.
The North Shore lies on the north side of the Midcontinent Rift System which ran 1,300 miles (2,000 km) northwest from southern Michigan, through what is now Lake Superior, and south-southwest into Kansas. [4] As the granitic crust was torn apart by continental drift, lava flowed out from 30–60 miles (50–100 km) under the crust and formed basalt. Tectonic forces were not strong enough to continue to separate the two sides of the continental rift; when the rifting stopped, the lava cooled and the heavy crust sank and was filled with sediment.
During recent glaciations, a large amount of the basalt and sandstone, which erode much more easily than granite, was removed by the glaciers. This formed the rough, rugged shoreline on the North Shore today. As the glaciers retreated, they left behind eroded igneous material, much of which covers the rocky beaches on the North Shore. The Wisconsin side of the basin and the bottom of the basin filled with the residue from the eroded sandstone and thus are sandy beaches today.
The melting water from the retreat of the glaciers ran into the basin and began to fill, forming the Great Lakes. The shoreline at its maximum reached over 500 feet (150 m) above its current height, and at its minimum fell to 250 feet (75 m) below its current level. When the levels of Lake Michigan and Lake Huron fell 2,000 years ago, it created rapids at Sault Sainte Marie, which restricted the release of water from Lake Superior and brought the shoreline to its present level.
The modern shoreline is composed of basalt lava flows. In the south, near Duluth, other materials, such as slate, greywacke and sandstone, are found a short distance inland; but in the north, the entire bedrock made of basalt and gabbro is exposed in patches miles from shore. When the bedrock hits the surface of the lake at a shallow enough angle, the beach is covered with washed up rocks. When it hits the lake at a steep angle, it breaks off and makes sharp cliffs ending at the lake.
To people who camp in the state parks along Minnesota's North Shore, the term North Shore refers to both the shore of the lake and all the rivers which run into the lake. Thus there are numerous "North Shore state parks," most of which are not actually on the lakeshore, and several of which are not even particularly close to it.
The majority of Ontario Provincial Parks are undeveloped nature reserves with no formal campgrounds or visitor centers.
Isle Royale National Park is an American national park consisting of Isle Royale, along with more than 400 small adjacent islands and the surrounding waters of Lake Superior, in the state of Michigan.
Lake Superior is the largest freshwater lake in the world by surface area and the third-largest freshwater lake by volume, holding 10% of the world's surface fresh water. Located in central North America, it is the northernmost and westernmost of the Great Lakes of North America, straddling the Canada–United States border with the Canadian province of Ontario to the north and east and the U.S. states of Minnesota to the west and Michigan and Wisconsin to the south. It drains into Lake Huron via St. Marys River, then through the lower Great Lakes to the St. Lawrence River and ultimately the Atlantic Ocean.
Duluth is a port city in the U.S. state of Minnesota and the county seat of St. Louis County. Located on Lake Superior in Minnesota's Arrowhead Region, the city is a hub for cargo shipping. Commodities shipped from the Port of Duluth include coal, iron ore, grain, limestone, cement, salt, wood pulp, steel coil, and wind turbine components. Duluth is south of the Iron Range and the Boundary Waters Canoe Area Wilderness.
St. Louis County is a county located in the Arrowhead Region of the U.S. state of Minnesota. As of the 2020 census, the population was 200,231. Its county seat is Duluth. It is the largest county in Minnesota by land area, and the largest in the United States by total area east of the Mississippi River. St. Louis County is included in the Duluth, MN–Superior, WI Metropolitan Statistical Area.
Lake County is a county in the U.S. state of Minnesota. As of the 2020 census, the population was 10,905. Its county seat is Two Harbors.
Two Harbors is a city in and the county seat of Lake County, Minnesota, United States, along the shore of Lake Superior. The population was 3,633 at the 2020 census. Minnesota State Highway 61 serves as a main route in Two Harbors. Gooseberry Falls State Park is 13 miles (21 km) to the northeast. The city is home to a cargo shipping port for mined iron ore.
The Pigeon River forms part of the Canada–United States border between the state of Minnesota and the province of Ontario, west of Lake Superior. In pre-industrial times, the river was a waterway of great importance for transportation and the fur trade.
The Boundary Waters Canoe Area Wilderness comprises 1,090,000 acres (440,000 ha) of pristine forests, glacial lakes, and streams in the Superior National Forest. Located entirely within the U.S. state of Minnesota at the Boundary Waters, the wilderness area is under the administration of the United States Forest Service. Efforts to preserve the primitive landscape began in the 1900s and culminated in the Boundary Waters Canoe Area Wilderness Act of 1978. The area is a popular destination for canoeing, hiking, and fishing, and is the most visited wilderness in the United States.
Taconite is a variety of banded iron formation, an iron-bearing sedimentary rock, in which the iron minerals are interlayered with quartz, chert, or carbonate. The name "taconyte" was coined by Horace Vaughn Winchell (1865–1923) – son of Newton Horace Winchell, the Minnesota State Geologist – during their pioneering investigations of the Precambrian Biwabik Iron Formation of northeastern Minnesota. He believed the sedimentary rock sequence hosting the iron-formation was correlative with the Taconic orogeny of New England, and referred to the unfamiliar and as-yet-unnamed iron-bearing rock as the 'taconic rock' or taconyte.
The Iron Range is collectively or individually a number of elongated iron-ore mining districts around Lake Superior in the United States and Canada. Much of the ore-bearing region lies alongside the range of granite hills formed by the Giants Range batholith. These cherty iron ore deposits are Precambrian in the Vermilion Range and middle Precambrian in the Mesabi and Cuyuna ranges, all in Minnesota. The Gogebic Range in Wisconsin and the Marquette Iron Range and Menominee Range in Michigan have similar characteristics and are of similar age. Natural ores and concentrates were produced from 1848 until the mid-1950s, when taconites and jaspers were concentrated and pelletized, and started to become the major source of iron production.
Minnesota State Highway 61 is a 150.321-mile-long (241.918 km) highway in northeast Minnesota, which runs from a junction with Interstate 35 (I-35) in Duluth at 26th Avenue East, and continues northeast to its northern terminus at the Canadian border near Grand Portage, connecting to Ontario Highway 61 at the Pigeon River Bridge. The route is a scenic highway, following the North Shore of Lake Superior, and is part of the Lake Superior Circle Tour designation that runs through Minnesota, Ontario, Michigan, and Wisconsin.
Canoe camping, also known as touring, tripping or expedition canoeing, is a combination of canoeing and camping. Canoe campers typically carry enough supplies with them to travel and camp for several days via a canoe.
The Arrowhead Region is located in the northeastern part of the U.S. state of Minnesota, so called because of its pointed shape. The predominantly rural region encompasses 10,635.26 square miles (27,545.2 km2) of land area and includes Carlton, Cook, Lake and Saint Louis counties. Its population at the 2000 census was 248,425 residents. The region is loosely defined, and Aitkin, Itasca, and Koochiching counties are sometimes considered as part of the region, increasing the land area to 18,221.97 square miles (47,194.7 km2) and the population to 322,073 residents. Primary industries in the region include tourism and iron mining.
The Pukaskwa River is a river in Thunder Bay District and Algoma District in Northern Ontario, Canada. It is in the Great Lakes Basin and is a tributary of Lake Superior, which it enters at the south end of Pukaskwa National Park. It is a remote, pristine, free-flowing, medium-sized Shield river, with lots of whitewater, best travelled in spring.
Grand Portage State Park is a state park at the northeastern tip of the U.S. state of Minnesota, on the Canada–United States border. It contains a 120-foot (37 m) waterfall, the tallest in the state, on the Pigeon River. The High Falls and other waterfalls and rapids upstream necessitated a historically important portage on a fur trade route between the Great Lakes and inland Canada. This 8.5-mile (13.7 km) path as well as the sites of historic forts at either end are preserved in nearby Grand Portage National Monument.
Jay Cooke State Park is a state park of Minnesota, United States, protecting the lower reaches of the Saint Louis River. The park is located about 10 miles (16 km) southwest of Duluth and is one of the ten most visited state parks in Minnesota. The western half of the park contains part of a rocky, 13-mile (21 km) gorge. This was a major barrier to Native Americans and early Europeans traveling by canoe, which they bypassed with the challenging Grand Portage of the St. Louis River. The river was a vital link connecting the Mississippi waterways to the west with the Great Lakes to the east.
Minnesota Point, also known as the Park Point neighborhood of Duluth, Minnesota, United States; is a long, narrow sand spit that extends out from the Canal Park tourist recreation-oriented district of the city of Duluth. The Point separates Lake Superior from Superior Bay and the Duluth Harbor Basin.
The Great Lakes Circle Tour is a designated scenic road system connecting all of the Great Lakes and the St. Lawrence River. It consists of routes for circumnavigating the lakes, either individually or collectively. It was designated by the Great Lakes Commission in 1988.
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