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The Grand Kankakee Marsh is the result of the last glacial age. The Wisconsin Glacial Episode began 70,000 years ago [2]: 34 and removed all traces of the previous glacial topography. It wasn't until the last 3,000 years that the glaciers left the topography we know today.
The Kankakee River also forms the southern boundary of Porter County, delimiting an area of farm land and wetland forest. Throughout this area, the Kankakee is also called the Marble Power Ditch. This is the heart of the Grand Kankakee Marsh, which was drained in the early 20th century.
This area is part of the Grand Kankakee Marsh system and the site of the largest natural lake in Indiana until it was drained. Beaver Lake was 7 miles (11 km) long and 5 miles (8.0 km) wide. As a shallow lake, only 10 feet (3.0 m) deep, it was filled with vegetation and wildlife. It was drained by the 1880s.
The drainage process began in 1854, when a ditch running from Beaver Lake to the Kankakee River was dug. The Indianapolis Journal correctly predicted that Michael Bright intended to drain the lake and claim ownership of the land. Indeed, once Bright purchased the entire shoreline of the lake, he declared that he owned, "the bed of said lake ...
The sprawling wetland known as the Grand Kankakee Marsh once served as a detoxifying cleanser of the South Bend region's waters, including what residents drank.. People drained it decades ago and ...
The lake drained about 13,000 YBP, until reaching the level of the Momence Ledge. The outcropping of limestone created an artificial base level, holding water throughout the upper basin, creating the Grand Kankakee Marsh. Lake Kankakee was a prehistoric lake during the Wisconsin glacial epoch of the Pleistocene Era.
By nature, this was once a rich, biodiverse land that sat just beyond the sprawling wetland known as the Grand Kankakee Marsh, a detoxifying cleanser of local water, which people had drained ...
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 .