Keweenaw Fault

The Keweenaw Fault is a reverse fault that bisects the Keweenaw Peninsula of the Upper Peninsula of Michigan.^[1] The fault thrusts lava flows of the Midcontinent Rift System onto sedimentary rocks of the Jacobsville Sandstone. The fault is part of the inversion of the Midcontinent Rift where a region that had previously undergone extension experienced significant contraction. This contraction occurred during the final stages of the Grenvillian orogeny.^[2] The Keweenaw Peninsula, itself, is the southeastern side of a large syncline beneath Lake Superior. The northwestern side forms Isle Royale.^[3]

The fault is more than 100 miles (160 kilometers) long and extends from the tip of the Keweenaw Peninsula in the northeast to a termination near the Michigan-Wisconsin border in the southeast.^[4] The fault is most likely younger than the Jacobsville Formation and the Devonian Period.^[5]

A seismic event in 1906 claimed to be an earthquake has been attributed to a rock burst, as the area has been significantly mined.^[6]

^ Brandes, Paul. "Geology of the Keweenaw Peninsula, Michigan". mindat.org. Retrieved March 4, 2012.
^ Hodgin, E. B., Swanson-Hysell, N. L., DeGraff, J. M., Kylander-Clark, A. R. C., Schmitz, M. D., Turner, A. C., Zhang, Y., Stolper, D. A. (2022), Final inversion of the Midcontinent Rift during the Rigolet Phase of the Grenvillian Orogeny, Geological Society of America
^ Huber, N. King (1975). "The Geologic Story of Isle Royale National Park". United States Geological Survey. Retrieved February 2, 2008.
^ Hamblin, W.M. Kenneth (1958). The Cambrian Sandstones of Northern Michigan (PDF) (Report). State of Michigan Department of Conservation. p. 47. Retrieved February 16, 2012.
^ Hamblin, W.M. Kenneth (1958). The Cambrian Sandstones of Northern Michigan (PDF) (Report). State of Michigan Department of Conservation. p. 48. Retrieved February 16, 2012.
^ McLaren, Noël (August 30, 2011). "Could the Keweenaw Fault become active?". Upper Michigan's Source. Retrieved March 4, 2012.

[1] Brandes, Paul. "Geology of the Keweenaw Peninsula, Michigan". mindat.org. Retrieved March 4, 2012.

[Hodgin2022-2] Hodgin, E. B., Swanson-Hysell, N. L., DeGraff, J. M., Kylander-Clark, A. R. C., Schmitz, M. D., Turner, A. C., Zhang, Y., Stolper, D. A. (2022), Final inversion of the Midcontinent Rift during the Rigolet Phase of the Grenvillian Orogeny, Geological Society of America

[usgs-3] Huber, N. King (1975). "The Geologic Story of Isle Royale National Park". United States Geological Survey. Retrieved February 2, 2008.

[4] Hamblin, W.M. Kenneth (1958). The Cambrian Sandstones of Northern Michigan (PDF) (Report). State of Michigan Department of Conservation. p. 47. Retrieved February 16, 2012.

[5] Hamblin, W.M. Kenneth (1958). The Cambrian Sandstones of Northern Michigan (PDF) (Report). State of Michigan Department of Conservation. p. 48. Retrieved February 16, 2012.

[6] McLaren, Noël (August 30, 2011). "Could the Keweenaw Fault become active?". Upper Michigan's Source. Retrieved March 4, 2012.

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