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kettle hole

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kettle hole

Pit or depression formed when a block of ice from a receding glacier becomes isolated and buried in glacial debris (till). As the block melts the till collapses to form a hollow, which may become filled with water to form a kettle lake or pond.

Kettle holes range from 5 m/15 ft to 13 km/8 mi in diameter, and may exceed 33 m/100 ft in depth.

As time passes, water sometimes fills the kettle holes to form lakes or swamps, features found throughout much of northern North America. Lake Ronkonkoma, the largest lake on Long Island, New York, is an example.



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Some of the marl pits from long ago, where clay was dug out to improve the quality of the soil, also kettle holes, made when the glaciers retreated, had developed into ponds.
Pout Pond is a kettle hole created by the retreat of a glacier during the last ice age.
Houghton's Pond is a spring-fed kettle hole pond formed by receding glaciers approximately 10,000 years ago.
 
 
 
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