This landform can be observed after the glacier has melted and the delta's asymmetrical triangular shape is visible.
Kame deltas form in association with other glacial features such as kettles and eskers.
These formations give indication that kame deltas formed during times of glaciation.
This type of formation causes the asymmetrical triangular shaped mound, with a flat top.
The Fonthill Kame Delta is the highest point in the Niagara Peninsula region.