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inhabitants of the countries to the West see the rays of the sun
illuminating a great part of its summit for as much as a quarter of
the longest night. And in the same way, in those countries which lie
to the East.
OF THE STRUCTURE AND SIZE OF MOUNT TAURUS.
[Footnote 73: The statements are of course founded on those of the
'inhabitants' spoken of in 1. 67.] The shadow of this ridge of the
Taurus is of such a height that when, in the middle of June, the Sun
is at its meridian, its shadow extends as far as the borders of
Sarmatia, twelve days off; and in the middle of December it extends
as far as the Hyperborean mountains, which are at a month's journey
to the North [75]. And the side which faces the wind is always free
from clouds and mists, because the wind which is parted in beating
on the rock, closes again on the further side of that rock, and in
its motion carries with it the clouds from all quarters and leaves
them where it strikes. And it is always full of thunderbolts from
the great quantity of clouds which accumulate there, whence the rock
is all riven and full of huge debris [Footnote 77: Sudden storms are
equally common on the heights of Ararat. It is hardly necessary to
observe that Ararat cannot be meant here. Its summit is formed like
the crater of Vesuvius. The peaks sketched on Pl. CXVI-CXVIII are
probably views of the same mountain, taken from different sides.
Near the solitary peak, Pl. CXVIII these three names are written
goba, arnigasar, caruda, names most likely of different peaks. Pl.
1075
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