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Updated: August 4, 2026
The prevailing rock in this neighbourhood is the black, calcareous, compact shale, whilst in the valley-basin of the Yeso the purplish red sandstone or mudstone predominates, both being associated with gypseous strata of exactly the same nature.
Beyond these lakes there was a ridge, which we had no sooner crossed than a dismally grand prospect opened before us. We overlooked a valley-basin, marked with belts of stunted birch, and stretching away for several miles to the foot of a bleak snowy mountain, which I at once recognised as Lippavara.
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