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We know now that it consists of an inextricable entanglement of valleys, the mean altitude of which exceeds three thousand metres; we know that it is dominated by the peaks of Gouroumdi and Kauffmann, twenty-two thousand feet high, and the peak of Tagarma, which is twenty-seven thousand feet; we know that it sends off to the west the Oxus and the Amou Daria, and to the east the Tarim; we know that it chiefly consists of primary rocks, in which are patches of schist and quartz, red sands of secondary age, and the clayey, sandy loess of the quaternary period which is so abundant in Central Asia.
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