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Above about 3 900 m the eastern side of the range is dissected by glacial cirques and by two large U-shaped gorges from which sizeable glaciers debouched during the last glacial episode, with termini extending down to at least 2 700 m. Today they are marked by huge end moraines. Several small cirque glaciers, ice caps, and hanging valley glaciers are active today with a regional snowline at about 5 000 m (cf. Shi, 1980; Ives and Messerli, 1984). Many of the peaks are unclimbed.

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