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  • 21 Aug, 2019

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

See also

Wikimedia Commons has media related to Damma Glacier.

References

  1. ^ Frey, Beat; Rieder, Stefan R.; Brunner, Ivano; Plötze, Michael; Koetzsch, Stefan; Lapanje, Ales; Brandl, Helmut; Furrer, Gerhard (2010). "Weathering-Associated Bacteria from the Damma Glacier Forefield: Physiological Capabilities and Impact on Granite Dissolution". Applied and Environmental Microbiology. 76 (14): 4788–4796. Bibcode:2010ApEnM..76.4788F. doi:10.1128/AEM.00657-10. ISSN 0099-2240. PMC 2901745. PMID 20525872.
  2. ^ Magnusson, Jan; Kobierska, Florian; Huxol, Stephan; Hayashi, Masaki; Jonas, Tobias; Kirchner, James W. (2014-01-30). "Melt water driven stream and groundwater stage fluctuations on a glacier forefield (Dammagletscher, Switzerland): STREAM-GROUNDWATER INTERACTIONS ON A GLACIER FOREFIELD". Hydrological Processes. 28 (3): 823–836. doi:10.1002/hyp.9633.
  3. ^ Hindshaw, Ruth S.; Tipper, Edward T.; Reynolds, Ben C.; Lemarchand, Emmanuel; Wiederhold, Jan G.; Magnusson, Jan; Bernasconi, Stefano M.; Kretzschmar, Ruben; Bourdon, Bernard (2011-06-22). "Hydrological control of stream water chemistry in a glacial catchment (Damma Glacier, Switzerland)". Chemical Geology. 285 (1): 215–230. Bibcode:2011ChGeo.285..215H. doi:10.1016/j.chemgeo.2011.04.012. ISSN 0009-2541.
  4. ^ Wojcik, Robin; Eichel, Jana; Bradley, James A.; Benning, Liane G. (2021-07-01). "How allogenic factors affect succession in glacier forefields". Earth-Science Reviews. 218: 103642. Bibcode:2021ESRv..21803642W. doi:10.1016/j.earscirev.2021.103642. hdl:1874/412195. ISSN 0012-8252.

46°37′59″N 8°26′3″E / 46.63306°N 8.43417°E / 46.63306; 8.43417


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