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Terminal moraine

View on map:39.727509°N 84.202409°W

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Terminal moraine
39.728109°N 84.202494°W

In Carillon Park

The hill marks the furthest the glaciers expanded during the ice age from a more than mile thick sheet of ice more than 10,000 years ago. 

Description


Terminal moraine

A terminal moraine, also called end moraine, is a type of moraine that forms at the snout (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, and has been pushed by the front edge of the ice, is driven no further and instead is dumped in a heap. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice.

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