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Kame delta
A kame delta is a glacial landform made by a stream flowing through glacial ice and depositing material (Kame - distinctive because it has been sorted by the action of the stream) upon entering a lake or pond at the end or terminus of the glacier, thus "in front" of it, a proglacial lake. This landform may often be observed after the glacier has melted and usually has a delta (in the sense of the Greek letter) or triangular shape.
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