description Burlington Esker Overview
help Burlington Esker FAQ
What is the Burlington Esker?
The Burlington Esker is a glaciofluvial ridge in the Burlington area of Vermont. It formed from sediment deposited by meltwater during the glacial period.
How did the Burlington Esker form?
Meltwater flowing through or beneath glacial ice carried sand and gravel, which were deposited as the ice changed or melted. The resulting ridge is a remnant of that glaciofluvial process.
Where is the Burlington Esker located?
It is located in the Burlington area of Vermont near the Lake Champlain basin. Its setting reflects the region's glacial history.
What does glaciofluvial mean in relation to an esker?
Glaciofluvial means shaped by meltwater from glaciers. In an esker, that meltwater leaves a long ridge of sand and gravel behind.
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