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The epicenters show a clear relationship to tectonic features of the state; four epicenters lie along the Great Lakes tectonic zone. [15] Depths are estimated at 5 to 20 km (3 to 12 mi). [ 15 ] The best-documented event occurred on July 9, 1975, near Morris, Minnesota , with a magnitude of 4.6, and a felt area of 82,000 km 2 (32,000 sq mi ...
Map showing approximate location of many current hotspots and the relationship to current tectonic plates and their boundaries and movement vectors The origins of the concept of hotspots lie in the work of J. Tuzo Wilson , who postulated in 1963 that the formation of the Hawaiian Islands resulted from the slow movement of a tectonic plate ...
These plates are often grouped with an adjacent principal plate on a tectonic plate world map. For purposes of this list, a microplate is any plate with an area less than 1 million km 2 . Some models identify more minor plates within current orogens (events that lead to a large structural deformation of Earth's lithosphere ) like the Apulian ...
The lake is near the Superior National Forest and the Boundary Waters Canoe Area Wilderness (BWCAW). The Minnesota DNR ranks Lake Vermilion as the fifth largest lake by surface area for bodies of water entirely within Minnesota borders. The surface area of Lake Vermilion is 39,271 acres (158.9 km 2) and has a maximum depth of 76 feet (23 m). [3]
Apr. 30—The pandemic push of more people fishing on northern Minnesota lakes, especially with Canadian lakes still off-limits, has spurred the Vermilion Lake Association to ask anglers to keep ...
Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that the Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.
Lake Vermilion is a 1,000 acres (400 ha) reservoir located in Vermilion County, Illinois. It was built for water supply, fishing , and recreation purposes. The lake is 3 miles (4.8 km) long and 0.5 miles (0.80 km) wide.
Obduction zones occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction. [citation needed]