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THE CHARACTERISTICS OF THE CAUCASUS 55<br />
I am told that this is a modei'ate estimate. I may be excused,<br />
therefore, if I tell the truth about that vague old abstraction, '<br />
snow-level.' The figure given for it in an extensive range may<br />
serve as a useful mean, but in most places must be locally inexact.<br />
For 'the Caucasus' it is impossible to lay down any limit wliicl]<br />
shall be even approximately accurate for the whole chain and both<br />
sides of it. The chain extends over five degrees of latitude ; moi"e<br />
than that, its rainfall is at least four times greater at the Black Sea<br />
end than it is at the Caspian end. Naturally, at one extremity<br />
snow lies permanently down to about 9000 feet, at the other ceases<br />
at about 12,000 feet. In the central part of the chain nothing<br />
like a continuous snow-bed, not due to avalanches, is found under<br />
9500 feet, and on the northern spurs, where there is less fall,<br />
and black rock-slopes facing southwards are exposed to a sun<br />
which i-aises the steppe shade-temperature to over 90" F., the<br />
snow-limit will rise in places to over 11,000<br />
the<br />
feet. For the snow-<br />
level in the central chain 10,000 feet may be taken as a fair figure.<br />
But as I have said before, this limit should be represented l)y a<br />
zigzag line going up and down, according to accidents of exposure,<br />
soil, and vicinity to large glaciers. Let us get rid altogether of a<br />
statement frequently repeated, that Dr. Radde found the snow-<br />
level 8400 feet at the Rion sources. What he wrote was, that<br />
in September he found patches of fresh-fallen snow at that height.<br />
This is how error may be created by inaccui'ate copyists !<br />
I have given elsewhere a catalogue of '<br />
Peaks and Passes.' It<br />
may be enough to mention here a few of the most conspicuous.<br />
Before 1870 the Russian surveyors had triangulated only a few<br />
of the snowy peaks — those which are most conspicuous from the<br />
northern steppe — Elbruz, 18,470 feet; Koshtantau, 16,880; Dykhtau,<br />
17,054; Adai Khokh, 15,244: Gimarai Khokh, 15,672; and<br />
Kasbek, 16,546. Between the Marukh Pass and the Mamison<br />
Pass the five-verst map does not give a single height on the<br />
watershed. It was left to the new and still unpublished survey<br />
to find<br />
figures for Dongusorun, 14,605 ; Ushba, north peak<br />
' The figures given are those of the new survey, which differ in many<br />
the five-verst map.<br />
*<br />
cases from those of