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Coordinates: 41°30′37″N 87°3′29″W. Valparaiso Moraine at Mink Lake, north of Valparaiso, Indiana. The Valparaiso Moraine is a recessional moraine (a land form left by receding glaciers) that forms an immense U around the southern Lake Michigan basin in North America. It is a band of hilly terrain composed of glacial till and sand.
Coordinates: 42°54′11.4″N 83°25′30.6″W. The Hadley Hills are a rugged glacial moraine located in The Thumb of Michigan, that extend from northern Oakland County and into southern Lapeer County . The Hadley Hills surround the village of Hadley; [1] The highest points and most prominent outcroppings are: Pinnacle Point at 1,262 feet ...
Tinley Moraine. Coordinates: 41°35′35″N 87°46′33″W. Tinley moraine, a glacial feature of Illinois & Indiana. Based on Publication 6876-12989-1-PB; The Tinley Moraine in Indiana; Allan F. Schneider; Indiana Geological Survey; Indianapolis, Indiana; undated. The Tinley Moraine is a moraine around the Lake Michigan basin in North America.
The medial moraine is the double line of debris running down the centre-line of the glacier. Lateral moraines can rise up to 140 meters (460 ft) over the valley floor, can be up to 3 kilometers (1.9 mi) long, and are steeper close to the glacier margin (up to 80 degrees) than further away (where slopes are typically 29 to 36 degrees. [15]
The Kankakee Torrent was a catastrophic flood that occurred about 19,000 calibrated years ago [1] in the Midwestern United States. It resulted from a breach of moraines forming a large glacial lake fed by the melting of the Late Wisconsin Laurentide Ice Sheet. The point of origin of the flood was Lake Chicago. [1]
1.1.4 Lake Michigan Basin. ... This a partial list of glacial moraines. They are arranged by continents and divided by related hydrologic basins. This list is incomplete.
The Fort Wayne Moraine is considered contemporary to the last stages of the Valparaiso Moraine. Centered on Fort Wayne, Indiana, the northern leg of the moraine is mostly overlaid by the younger Wabash Moraine angling northeastward through Williams County, Ohio. It only becomes identifiable in Lenawee County, Michigan south and northeast of ...
Lake Maumee was a proglacial lake and an ancestor of present-day Lake Erie. It formed about 17,500 calendar years, or 14,000 Radiocarbon Years Before Present (RCYBP) as the Huron-Erie Lobe of the Laurentide Ice Sheet retreated at the end of the Wisconsin glaciation. As water levels continued to rise the lake evolved into Lake Arkona and then ...
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