Calderone glacier

Calderone glacier
"Il Calderone", Europe's second southernmost glacial mass as seen in July 2007, deglaciation has not slowed, making it unlikely the Calderone will survive past 2030
Map showing the location of Calderone glacier
Map showing the location of Calderone glacier
Calderone glacier
Glacier's location in Italy
LocationSouthern slopes of the Corno Grande massif
Coordinates42°28′15.794″N 13°34′0.156″E / 42.47105389°N 13.56671000°E / 42.47105389; 13.56671000
Map

The Calderone glacier (Italian: Ghiacciaio del Calderone) is a glacier located in the Apennine Mountains in Abruzzo, Italy. Found in the Gran Sasso d'Italia mountain group, it lies just beneath the Corno Grande, the highest peak in the Apennines.

With the disappearance of the Corral de la Veleta glacier in the Sierra Nevada in 1913, "Il Calderone" became one of Europe's southernmost known glaciers (42°28′N, 13°33′E), being slightly to the north only compared to Snezhnika (latitude of 41°46′09″ N) and Banski Suhodol Glaciers in Pirin Mountain in Bulgaria.[1][2][3][4] If present deglaciation trends continue, the Calderone may soon disappear as well. The discovery of a number of small glaciers in the Accursed Mountains in 2009 seemed to threaten Calderone's positions.[5]

  1. ^ "(the pirin mountains, bulgaria) in the last ten years" (PDF). igipz.pan.pl. Retrieved 5 February 2014.
  2. ^ Grunewald, K; Scheithauer, J (2010), "Europe's southernmost glaciers: response and adaptation to climate change", Journal of Glaciology, 56 (195): 129–142, Bibcode:2010JGlac..56..129G, doi:10.3189/002214310791190947
  3. ^ Gachev, Emil; Gikov, Alexander; Zlatinova, Cvetelina; Blagoev, Bozidar. "Present state of Bulgarian glacierets" (PDF). Landform Analysis. 11.
  4. ^ Gachev, Emil; Stoyanov, Krasimir (2013). "СЪВРЕМЕННИ СНЕЖНО-ФИРНОВИ ТЕЛА В ПЛАНИНАТА ПРОКЛЕТИЯ (АЛБАНСКИ АЛПИ)" (PDF). Problems of Geography (in Bulgarian).
  5. ^ Grunewald, K; Scheithauer, J (2010), "Europe's southernmost glaciers: response and adaptation to climate change", Journal of Glaciology, 56 (195): 129–142, Bibcode:2010JGlac..56..129G, doi:10.3189/002214310791190947