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Nipissing Great Lakes was a prehistoric proglacial lake. Parts of the former lake are now Lake Superior, Lake Huron, Georgian Bay and Lake Michigan. It formed about 7,500 years before present (YBP). The lake occupied the depression left by the Labradorian Glacier. [1] This body of water drained eastward from Georgian Bay to the Ottawa valley.
Paleontology in Michigan. The location of the state of Michigan. Paleontology in Michigan refers to paleontological research occurring within or conducted by people from the U.S. state of Michigan. During the Precambrian, the Upper Peninsula was home to filamentous algae. The remains it left behind are among the oldest known fossils in the world.
Lake Rouge in Michigan south of Detroit. Lake St. Clair and the Detroit River: Early Lake St. Clair: 12,500 – 5,500 YPB in Lake St. Clair; Michigan and Ontario. [1] Lake Huron basin Later Lake Saginaw in Saginaw Bay on the lower peninsula of Michigan. Nipissing Great Lakes; 5,500 [9] - 4,500 YBP [10]
Lake Algonquin was a prehistoric proglacial lake that existed in east-central North America at the time of the last ice age. Parts of the former lake are now Lake Huron, Georgian Bay, Lake Superior, Lake Michigan, Lake Nipigon, and Lake Nipissing. The lake varied in size, but it was at its biggest during the post-glacial period and gradually ...
The Old Copper complex or Old Copper culture is an archaeological culture from the Archaic period of North America's Great Lakes region. Artifacts from some of these sites have been dated from 7500 to 1000 BCE. [1][page needed] It is characterized by widespread copper artifacts, including tools and weapons, as well as ornamental objects.
pluvial lake (a paleolake created by a change in water balance in the basin) Etymology. Benjamin Bonneville. Surface area. ~20,000 sq mi (51,000 km 2) (at max. lake level) Max. depth. over 980 ft (300 m) Lake Bonneville was the largest Late Pleistocene paleolake in the Great Basin of western North America.
Lake Chicago. Map of middle stage of glacial Lake Chicago, USGS Report of 1915. Lake Chicago was a prehistoric proglacial lake that is the ancestor of what is now known as Lake Michigan, one of North America 's five Great Lakes. Formed about 13,000 years ago and fed by retreating glaciers, it drained southwest through the Chicago Outlet River.
The Moccasin Bluff site (also designated 20BE8) is an archaeological site located along the Red Bud Trail and the St. Joseph River north of Buchanan, Michigan.It was listed on the National Register of Historic Places in 1977, [1] and has been classified as a multi-component prehistoric site with the major component dating to the Late Woodland/Upper Mississippian period.