Un episodio parossistico nell’evoluzione dei ghiacciai del Gruppo del Monviso: il crollo del Ghiacciaio Superiore di Coolidge

A case of sudden evolution of Monviso glaciers: the ice avalanche of Upper Coolidge Glacier

Authors

  • Giovanni Mortara C.N.R. - Istituto di Ricerca per la Protezione Idrogeologica del Bacino Padano, Sezione di Torino, Torino, Italy Author
  • Furio Dutto C.N.R. - Istituto di Ricerca per la Protezione Idrogeologica del Bacino Padano, Sezione di Torino, Torino, Italy Author

Keywords:

Climate, Hazard, Monviso, W. Alps

Abstract

An ice avalanche (about 200,000 m3) occurred in July 1989 from Upper Coolidge Glacier on the northern side of
Monviso. The mass, having plunged throught a vertical depth of 935 m, swept up a considerable amount of morainic
debris. More than 250,000 m2 were covered with a layer of ice, snow and debris. The avalanche travelled uphill on the
opposite side of the valley, attaining a height of 50 m above the valley floor. The Monviso ice avalanche was triggered by
a combination of morphological and climatic factors. No similar event was ever been record. ed before in the region. 

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Published

2024-07-10

Issue

Section

Short communication

How to Cite

Mortara, G., & Dutto, F. (2024). Un episodio parossistico nell’evoluzione dei ghiacciai del Gruppo del Monviso: il crollo del Ghiacciaio Superiore di Coolidge: A case of sudden evolution of Monviso glaciers: the ice avalanche of Upper Coolidge Glacier. Geografia Fisica E Dinamica Quaternaria, 13(2), 187-189. https://www.gfdq.glaciologia.it/index.php/GFDQ/article/view/792

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