The Goose Lake region formed in the post Wisconsin glaciation period as a flat, wet area dominated by layers of sand and silt laid down by postglacial outwash. The Des Plaines River and Kankakee River converge near here to form the Illinois River.Until heavily exploited for its natural resources during the 19th and early 20th centuries, the Goose Lake area was a stable wetland, with swathes of prairie grass surrounding the shallow Goose Lake. The region is in the Central forest grasslands transition ecoregion.
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