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128 THE EXPLORATION OF THE CAUCASUS<br />
unreadable. I shall be content to<br />
generally succeed in becoming<br />
summarise only some of the chief indications of the new survey.<br />
In this group it shows one peak over 15,000, nine over 14,000 feet.<br />
The lowest pass over the main chain fells just under 11,000 feet.<br />
About sixty-five square miles are covered with snow and ice. The<br />
Karagom Glacier is ten miles, the Zea Glacier six, and the Songuta<br />
Glacier three and a half miles in length.<br />
In 1868, when the three young Englishmen whose travels<br />
are recorded in my Central Caucasus undertook to examine<br />
amhulando the nature of the chain between Kasbek and Elbruz,<br />
t,he second object of their journey was the exploration of this<br />
Adai Khokh Group. We had no trustworthy map to guide us<br />
at that date. Our information was limited to the notes, mainly<br />
archfeological, of Brosset, to a very confused notice in Klaproth<br />
of the snow-passes between Stir-Digor and Gebi,^ and to the<br />
vague indications and blue smears of the five-verst majj. The<br />
excursions of Dr. Abich and Dr. Radde had been limited to the<br />
lower ends of the two great frozen streams which, issuing<br />
from far<br />
invisible and unknown fountains in the recesses of the range,<br />
stretch their icy tongues down into the forest region. One of<br />
these, the Zea Glacier, flows into a glen some ten miles long<br />
that opens on the Ardon valley at St. Nikolai. Beyond the<br />
of men or the tracks of hunters all was obscure.<br />
paths<br />
Our intention in 1868 was to have gone up the Zea valley,<br />
and crossed from its head to the Mamison. But the difliculties<br />
we experienced with the inhabitants in traversing the deep and<br />
isolated basins that hold the sources of the Nardon made us<br />
give up a project which involved separation from our baggage.<br />
Consequently we carried out but half our plan, and were content,<br />
in the first instance, to ci'oss the Mamison to the soutliern side.<br />
We found ourselves at Chiora in the liion valley, at the foot of<br />
a native glacier pass, leading<br />
to the north side of the chain.<br />
' The best explanation tliat has been given of Khiproth's very curious description of the<br />
passage with liorses of the Gebi Passes— the Giirdzivsek, and Gebivsek or Gezevsek (new<br />
map)^ls that he took down hearsay information and turned it into a narrative in the first<br />
person.