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  2. Gogebic Range - Wikipedia

    en.wikipedia.org/wiki/Gogebic_Range

    The Gogebic Range is an elongated area of iron ore deposits located within a range of hills in northern Michigan and Wisconsin just south of Lake Superior. It extends from Lake Namakagon in Wisconsin eastward to Lake Gogebic in Michigan, or almost 80 miles.

  3. Montreal, Wisconsin - Wikipedia

    en.wikipedia.org/wiki/Montreal,_Wisconsin

    Montreal was originally incorporated as the Village of Hamilton, [7] on or about 1917, and was the first village formed in Iron County. [8]Montreal, as it was named upon its incorporation as a city on April 1, 1924, [7] was named for the Montreal Mining Company, which had several iron ore mines in the area during the late 1800s.

  4. Gogebic Taconite - Wikipedia

    en.wikipedia.org/wiki/Gogebic_Taconite

    Gogebic Taconite is an iron-ore mining company in development stage, based in Florida, [1] with a presence in Hurley, Wisconsin. [2] [3] The company, owned by the larger mining organizations, Cline Resource and Development Group, is at the center of a dispute among politicians, community groups, environmental organizations, Native American tribal councils and various stakeholders because of a ...

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  6. Iron Range - Wikipedia

    en.wikipedia.org/wiki/Iron_Range

    Erie Mining Company previously mined ore and testing to mine new minerals is ongoing. Keewatin (pop. 1,068) is between Nashwauk and Hibbing. It is home to U.S. Steel's KeeTac taconite mining and processing plant. Kinney (pop. 169) is an old mining boomtown on the Iron Range, between Buhl and Mountain Iron.

  7. Canadian mining company files papers to conduct exploratory ...

    www.aol.com/news/canadian-mining-company-files...

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  8. Geology of Wisconsin - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Wisconsin

    No rocks from the Paleogene or Neogene period are known from Wisconsin; however, abundant Quaternary deposits can be found as a result of the last Ice Age. The most recent glacial cycle, the Wisconsin Glaciation, began about 31,500 years ago and receded from the state by around 7,000 years ago. During this time the Lake Michigan Lobe and the ...

  9. Carbonate-hosted lead-zinc ore deposits - Wikipedia

    en.wikipedia.org/wiki/Carbonate-hosted_lead-zinc...

    World-wide distribution of MVT deposits (red), clastic sediment-hosted (green), and unclassified (blue) lead-zinc deposits. Source: USGS. Carbonate-hosted lead-zinc ore deposits are important and highly valuable concentrations of lead and zinc sulfide ores hosted within carbonate (limestone, marl, dolomite) formations and which share a common genetic origin.