Lake Kankakee

The glaciers were static, only in that the glacial fronts melted at a rate matching the southward push of the ice mass. The meltwaters from the eastern edge of the Michigan Lobe and the western edge of the Saginaw Lobe ran through the Dowagiac River valley of western Michigan. Joining the ancestral St. Joseph River, reversing the flow southward towards the flat plain till plain, where South Bend, Indiana now stands. From the east, the St. Joseph River valley drained the meltwaters from the southern edge of the Saginaw Lobe and the northwestern shoulder of the Huron-Erie Lobe. The Valparaiso Moraine formed the southern flank of the Michigan Lobe as well as the northern ridge of the Kankakee Valley. and the Marseilles moraine. On the west, the Marseilles moraine formed the final and lowest barrier. In the vicinity of Marseilles, Illinois the waters crested the divide and created an outlet into the pre-glacial Mississippi River, creating the modern Illinois River. This event is known as the Kankakee Torrent. ==Description==

Lake Kankakee covered over of northern Indiana and the border of Illinois. The lake had two open bodies of water, split by the Iroquois Moraine, which formed a peninsula from the west. The northern waters stretched from just west of Momence, Illinois, along the main stem of the Kankakee River to the marshes southwest of South Bend, Indiana. The southern waters stretched from near Watseka, Illinois eastward to the Tippecanoe River. These two basins were linked across of the nearly level Tipton Till Plain, west of the Tippecanoe River. The valley of the Tippecanoe from Monticello, north pass Winimac and reaching to Rochester was a part of this lake. ==Development==

Beginning around 15,000 years ago, the Michigan lobe of the Laurentian glacier had retreated back to a line along the Valparaiso Moraine, from Wisconsin along a line, inland of Lake Michigan, southward, around the City of Chicago, and the southern tip of Lake Michigan, through Indiana, curving northward into the State of Michigan, only inland from the shoreline. Meanwhile, the Huron-Saginaw lobe had melted back to the north and east along a line in Michigan extending from Holland eastward through Kalamazoo to Jackson. Beginning 14,000 years ago, the glacial lobes had cleared the valley of the Kankakee River of ice. At this point, the forward movement of ice coming from the north equaled the rate of melting over the summer season. Now stagnant, glacier provided a continuing source of ground rock and soil to the southern edge of the glacier, creating the Valaparaiso Moraine and releasing vast quantities of water, sand and silt into the valley beyond. Lacustrine deposits are those deposited in lake water and only when the lake drains or the land rises, does it become dry land. Most of the soils throughout the counties surrounding the Kankakee are loamy (up to a quarter clay, quarter to half silt with less than half being sand.)[3] The outwash plain is underlain by sand with gravel inter-bedded throughout. The prevailing westerly winds began to treat the 'Lake Kankakee' like the shores of Lake Michigan. Dunes began to form along the south and eastern shoreline. Where ice blocks had been left behind, sand filled the depressions. Runoff from the Valparaiso Moraine built [2] outwash ridges of sand leading into the lake. On the south, the winds built dunes. As the volume of water decreased from the glacier melting northward, the lake slowly drained and filled. Not being able to cut a channel through the limestone ridge in Momence, the Kankakee Lake became 500,000 acres (202,346 ha) of marshland. ==Aeolian sand==

The Aeolian sands form the southern boundary of Lake Kankakee as they result from the wind moving sand from the shoreline inland. This feature begins in the northeast along the Maxinkuckee moraine of the Saginaw ice lobe in Marshall County, Indiana near Lake Maxinkuckee and Culver, Indiana. While a few dunes are found on the moraine, the sand beds are along the western edge. The Maxinkuckee moraine follows the north side of Tippecanoe River into Fulton County eastward towards Rochester. The southeastern edge of the sands, swings south and west through Cass County, to west of Logansport, turning west and passing north of Lake Cicott. Here a sand ridge forms the east border of the till plain sloping westward to the Tippecanoe River. This ridge runs westward in continuous line to the Tippecanoe Valley at Monticello. This is a lateral moraine between the Saginaw lobe on the north and the Erie lobe on the south. The ridge continue westward and becomes hard to distinguish as it passes west of Kentland, Indiana. ==Outlet==

Lake Kankakee was over higher than the current river. It topped the western divide near Morris, Illinois, where a lake had formed as the glacier retreated from the Marseilles moraine. Initially, this water body, drained through numerous gaps in the moraine at the to above sea level, until the gap on the present Illinois River dropped lower than the rest, becoming the outlet for this lake. This outlet crosses exposed bedrock implying that it was a long slow process. Thus, this lake and Lake Kankakee were held in check. The terraces and beaches in the Morris Basin are above sea level or above the present head of the Illinois River. This shows that this lake existed during the Valparaiso Moraine stage. The lakes level extended up the Kankakee River Valley about as far as Braidwood, where the sand dunes set in. Once this breach in the Marseilles moraine was created, it became the discharged for Lake Chicago . Combined with Lake Wauponsee's waters, the outlet deepened. Lake Kankakee at this time was draining much of the St. Joseph Rivers watershed, which was fed by the Saginaw lobe. The erosion by this quantity of water created many of the features along the Illinois River and the lower Kankakee River. The rock barrier at Momence halted erosion further upriver. The various lakes formed by the glacial retreats and its moraines were at their maximum levels at this time. The outlet was at or above above sea level. ==See also==