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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,

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