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The trail, which has a comparative change in elevation of 1,000 feet (300 m) (steep for the U.S. Midwest) covers much of the length of the Marquette Iron Range, a historically and commercially significant range of hematite and magnetite mined for more than 150 years as iron ore. The trail celebrates the geological and human heritage of the ...
The Marquette Iron Range is a deposit of iron ore located in Marquette County, Michigan in the United States. The towns of Ishpeming and Negaunee developed as a result of mining this deposit. A smaller counterpart of Minnesota's Mesabi Range, this is one of two iron ranges in the Lake Superior basin that are in active production as of 2018. The ...
County Road 492 (CR 492, Co. Rd. 492) is a primary county road in Marquette County, Michigan.The road serves as an alternate route between Negaunee and Marquette.Several historic sites line the roadway as it runs south and parallel to the main highway, U.S. Highway 41 (US 41) and M-28, through the Marquette Iron Range in Michigan's Upper Peninsula.
The museum also displays the mineral collections of the Ishpeming Rock and Mineral Club. The shaft site and museum are served by the Iron Ore Heritage Trail, a 47-mile (76 km) bicycle and hiking trail that covers much of the length of the Marquette Iron Range. The Cliffs Shaft Mine Museum is the starting location for the Marquette Marathon. [8]
William Austin Burt discovered iron ore in the Marquette Range near Negaunee, Michigan in 1844. Iron ore was discovered on the Menominee Range in 1867 and on the Gogebic Range in 1884. It was first discovered in Minnesota on the Vermilion Range in 1885, the Mesabi Range in 1890, and the Cuyuna Range in 1903. [2]
The Jackson Mine is an open pit iron mine in Negaunee, Michigan, extracting resources from the Marquette Iron Range.The first iron mine in the Lake Superior region, [3] Jackson Mine was designated as a Michigan State Historic Site in 1956 [2] and listed on the National Register of Historic Places in 1971. [1]
Since the two ranges of hills are made up of dissimilar rock types, the rock formation containing the iron ore deposits is located exclusively within the southern (Gogebic) Range. The Gogebic Range experienced a speculative iron boom in the mid-1880s, and had recurring booms and busts from 1884 to 1967 as demand shifted.
Houghton-to-Chassell Rail-Trail 8.6 13.8 Houghton: Duluth, South Shore and Atlantic Railway [16] Iron Ore Heritage Trail: 47 76 Marquette: Duluth, South Shore and Atlantic Railway [17] Keweenaw Trails 58 93 Houghton, Keweenaw: Copper Range Railroad [18] Little Falls Trail 6.5 10.5 Ontonagon: Chicago and North Western Railroad [19] Ontonagon to ...