Abstract
Two distinct medial moraines are located on the tongue of Ghiacciaio dei Forni (Rhaetian Alps, Italy); they are formed by the confluence of three ice streams. The two ice-cored medial moraines originate from rock outcrops situated below the snow line. Nourishment of the moraines seems to be due primarily to the supraglacial debris derived from the rock walls. -from Author
Cite
CITATION STYLE
APA
Smiraglia, C. (1989). The medial moraines of Ghiacciaio dei Forni, Valtellina, Italy: morphology and sedimentology. Journal of Glaciology, 35(119), 81–84. https://doi.org/10.3189/002214389793701428
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