Kames are irregularly shaped hills or mounds formed by glacial deposition, specifically by the accumulation of sand and gravel. They typically occur in regions once covered by glaciers and are the result of meltwater streams depositing sediment as the glacier retreats. Kames are an important feature of the glacial landscape, often found alongside other glacial formations such as eskers and moraines, and they play a key role in understanding past glacial activity and sediment transport processes.
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