The Damma Glacier (German: Dammagletscher) is a small glacier situated in the central Swiss Alps.
[1][2] It has been in retreat since around 1850.
[3] The area between the front of the retreating glacier and the moraine from the most recent glacier recession – called the glacial forefield[4] – measures 10.7 square kilometres (4.1 sq mi) and is composed of granitic rocks.
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