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36 THE EXPLORATTON" OF THE CATICASrS<br />

15,400, JWrttB. peak 15,409; Tiktengen, 15,127; Gefffcola, 15,932:<br />

Tetnukl, 15,319; Janga, 16,569; Skkara, 17,038; ami a crowd of<br />

otlier peaks of between 15,000 and 13,000 feet. In a space aome<br />

ten miles square in the Central Grroup there are found to be no<br />

less than twenty distinct aummita of over 14,000 feet.<br />

To orogra.pher3 anri map-makera the importance of Shkara long<br />

remained unrecogni.aed. This noble mountain ia the Monte Puosa<br />

of the Caucasus. Conspicuous from, the southern plains<br />

from, the seaboard, it culminates like its Alpine<br />

and even<br />

rival in a five-<br />

crested ridge. It has its Gomer Glficier in the Bezingi Glacier,<br />

and its Val Anzasca in the glen of the Zena.<br />

E am responsible for the erroneous identification (in 1868) of<br />

Shka.ra with the Koshtantau of the five-verst map, now called<br />

Dykbtau. Twenty-seven yeara ago, when I drew the view from<br />

the Shtuluvaek, we saw two great mountaina where only one was<br />

ma,rked on the raa,p. Here was a dilemma. Shkara from this<br />

point of view wa^ fe.r the more imposing,<br />

and we called it Kosh-<br />

tantaTi, while the peak that had been measured under that name<br />

on the raa.p we called an '<br />

unknown peak.' Con.seqnently,<br />

atiidenta of Caucasian literature must be careful to remember that<br />

the TT .«] 1*^,1 atau, not only of my Central Caucasus, but also of<br />

Mr. book and Mr. Dent's early articles, ia always Shkara.<br />

In addition to Shkaxa we have found and climbed, and the<br />

surveyors have now measured, three more great peaks on the actual<br />

watersherl, and one projecting slightly from it on the aouth towarda<br />

Suanetia. These are the broad-fe^ed Janga—an exaggerated PLz<br />

Pabi ; the saildle-sha-ped crest of Katuintau ; the cone of Gestola ;<br />

and the white pyramid of Tetnuld. All these mountains are<br />

between 15,900 and 17,100 feet in height — higher, that ia, than<br />

Mont Blanc. On the other side of the trench— at their northern<br />

base— filled by the Bezingi and Dykhsu Glaciers, the Dykhtau-<br />

Koshtantau ridge rises in the form of a horseshoe, with at least<br />

five peaks of over 15,000 feet.<br />

Ne:?t In prominence to the Central Group, on the main chain,<br />

are to the west the peak of Tlktengen, the Schreckhorn of the<br />

Cancasu."*, which dominates the head -waters of the Gara-auz ; the

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