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During the last Ice Age, the glacier reached its southernmost extent in Indiana, stopping near the southern tip of the state around the Ohio River. This boundary is often referred to as the "glacial boundary," where glacial deposits can be found in the northern regions, while the southern areas are primarily characterized by non-glacial sediments. The influence of the glacier has shaped Indiana's topography, leaving behind features such as moraines and kettle lakes in the northern part of the state.

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