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32 THE EXPLORATION OF THE CAUCASUS<br />
nearly equal height, separated by a gap some 1500 feet in deiith,<br />
and 17,000 feet above the sea-level. Each of these cones preserves<br />
the features of a crater in a horseshoe ridge broken down on one<br />
side, and enclosing a shallow snow-filled basin. Observers from<br />
a distance, including M. Favre, have erroneously conjectured the<br />
deep hollow between the peaks to be a gap<br />
in an immense terminal<br />
crater, a supposition which the ascents by Mi-. Grove and myself<br />
have now finally disposed of ^<br />
Kasbek has a far less regular outline than its great rival, and<br />
the passing traveller who only sees it from the high-road may<br />
be excused for not recognising its volcanic origin. From the<br />
south its outline, if compared with the figures (on p. 123) iu<br />
Judd's Volcanoes, has something of the aspect of a breached cone.<br />
Signor Lerco, a Piedmontese gentleman, who climbed the mountain<br />
in 1887,' has sent me a photograph taken on the top of the buttress<br />
conspicuous from the post-station (about 14,500 feet), which shows<br />
the crags that there pi'otrude to be contorted masses of<br />
A great neve now clothes the northern face of the peak.<br />
lava.^<br />
Were<br />
a hut built on the ridge between the Devdorak and Chach glaciers,<br />
the mountain would be less dangerous than Mont Blanc, and<br />
not more ditficult of ascent. It was by this route that we de-<br />
scended in 1868.<br />
Generalities such as these, first gleaned from maps<br />
and books<br />
and scattered observations, the mountaineer summarises and fixes<br />
in his memory in the vivid moments spent on the mountain tops.<br />
De Saussure and Tyndall have both asserted the value of such<br />
bird's-eye views as a basis for scientific reasoning. I do not<br />
pi'etend<br />
to speak with authority on such high matters. Yet<br />
possibly an observer may not bring down less knowledge from<br />
these Pisgah-heights because he goes up to them without either<br />
a theory to support or a reputation to endanger. Of this much<br />
I am certain, that even to men not '<br />
' Grove's Frosty Caucasus, 1S75.<br />
2 See Schweizer Alpenzeitung, Nos. 17-21. Zurich, 1S88.<br />
physically minded,' panoramas<br />
' M. E. Favre has reported as follows on a piece of rock brought from the top and submitted<br />
to him by my guide, Fran(;ois Devouassoud :<br />
containing white crystals of oligoclase.'<br />
'<br />
It is a grey rock of a semi-vitrified substance,