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fl A Ik ^<br />

C H A P T E K VIII<br />

r.AI.KAI! AND P-KZIXt;<br />

Cold, insipid, smouchy Tartars.<br />

CHARLES LAMU<br />

\K limits of the Ceutial Ciroup, the<br />

heart of the Caucasus, have been de-<br />

tined very conveniently by Nature. The<br />

geologist as well as the topographer<br />

Hnds a clear boundar}^ laid down for<br />

lam.<br />

The gfranite stretches from the<br />

\ ^ J, 7^ Agashtan Pass westward to the Zanner ;<br />

on both these tracks the traveller finds<br />

crumbling slopes of crystalline schists.<br />

The Central Group comprises the main<br />

chain from Fytnargyn to Gestola, with<br />

the great spur which circles horse-shoe-<br />

wise round the Mishirgi Cilacier and includes Dykhtau and Kosh-<br />

tantau.<br />

In 1868 nobody knew anything about these mountains, except<br />

that two of them had been measured and called Koshtantau<br />

and Dykhtau by the Ilussian Surveyors. The first English<br />

mountain explorers were puzzled, and we naturally made some<br />

serious mistakes. So did ^Ir. Craufurd Grove and Mr. Clinton<br />

Dent, who followed us. The Koshtantau of the old five-<br />

verst map (now called Dykhtau) we identified with Shkara ;<br />

our<br />

successors confused Gestola with Tetnuld. Tt was not until<br />

1887 that I was able to show positively that the gigantic Shkara<br />

had been ignored by the earlier survey, and that Mr. Dent's

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