Geography
Conneaut Lake was formed as a kettle lake at the end of the Pleistocene. A large block of ice broke off the receding ice front and was surrounded by accumulating sediment. After the ice melted, the resulting depression was filled with water forming the lake. Water flows into Conneaut Lake through Inlet Run, a small stream on the north end of the lake. Water exits through the Conneaut Outlet, a larger creek which flows to the south through the Conneaut Marsh. The Conneaut outlet flows into French Creek, making it part of the Mississippi River drainage.
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