Geodesic
The Shape of a Glacier
Bollettino della Unione matematica italiana, Série 9, Tome 6 (2013) no. 2, pp. 299-317 Cet article a éte moissonné depuis la source Biblioteca Digitale Italiana di Matematica

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During the last hundred years, several theories have been proposed aimed at describing the shape adopted by glaciers and their rate of downhill flow. Geophysicists, however, still cannot agree on the precise explanation of the phenomenon, and the dominant cause controlling the sliding of glaciers. This might be due to pressure arising during melting, or alternatively it might be due to stress concentration. We here derive a simple mathematical model that combines both effects. 
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     author = {Knops, R. J. and Villaggio, Piero},
     title = {The {Shape} of a {Glacier}},
     journal = {Bollettino della Unione matematica italiana},
     pages = {299--317},
     year = {2013},
     volume = {Ser. 9, 6},
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     zbl = {1297.86012},
     mrnumber = {3112981},
     language = {en},
     url = {http://geodesic.mathdoc.fr/item/BUMI_2013_9_6_2_a2/}
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Knops, R. J.; Villaggio, Piero. The Shape of a Glacier. Bollettino della Unione matematica italiana, Série 9, Tome 6 (2013) no. 2, pp. 299-317. http://geodesic.mathdoc.fr/item/BUMI_2013_9_6_2_a2/