Midcontinent Rift System

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Geological map of North America showing (in white) the Midcontinent Rift, here labeled Keweenawan Rift.
Geological map of North America showing (in white) the Midcontinent Rift, here labeled Keweenawan Rift.

The Midcontinent Rift System (MRS) or Keweenawan Rift is a 2000 km. long geological rift in the center of the North American continent and south-central part of the North American plate. It trends north from central lower Michigan, turns west through Lake Superior with its outer arc following the line of the north shore of that lake in Minnesota and Ontario, then turns southwest through portions of Wisconsin, Minnesota, Iowa, Nebraska and Kansas.[1] It is approximately 1,100 million years old, from the Precambrian Mesoproterozoic era.

Cliffs at Palisade Head on Lake Superior in Minnesota, view northeast to Shovel Point; both are surficial relics of the Midcontinent Rift.
Cliffs at Palisade Head on Lake Superior in Minnesota, view northeast to Shovel Point; both are surficial relics of the Midcontinent Rift.

Near Lake Superior, rocks produced by this rift can be found on the surface along the shores of the Keweenaw Peninsula of Upper Michigan,[2] and on the North Shore of the lake in Minnesota.[3] The lake itself lies in the rift valley formed by the rifting. Further south, the rift is buried thousands of feet below the surface. Where buried, it has been mapped by gravity anomalies (its dense basaltic rock increases gravity locally),[4] aeromagnetic surveys,[5] and seismic data.[6] Deep drilling for commercial oil and gas exploration has penetrated the rift and made rock samples available.

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