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KASBEK AND THE OSSETE DISTRICT 93<br />
above the sea, and it was most undesirable to hazard by any rash<br />
or hasty move our chance of reaching terra cognita ere nightfall.<br />
One plan suggested was to tiu'n to the left and cross a gap<br />
west of our mountain which we had good reason to believe con-<br />
nected the plateau we were on with the nere of the glacier by<br />
whirli we had ascended. This course, if successfully<br />
carried ovit,<br />
would have brouii-ht us back to our tent and baofcraofe, but its<br />
probable length was a fatal objection. Eventually<br />
we determined<br />
to keep nearly due north across the snowfield, towards a ridge<br />
which divides the two glaciei's flowing respectively into the glens<br />
of Devdorak and Chach. We descended for some distance under<br />
the rocks along the left bank of the Devdorak Glacier, until the<br />
ice became so steep and broken that further progress promised<br />
to be difficult. We thereupon halted, Avhile Devouassoud climbed<br />
up again to the ridge<br />
side.<br />
and made a i-econnaissance on its northern<br />
After some delay, a shout from above called on us to follow, and<br />
we rejoined our guide, after a sharp scramble, at the base of a veiy<br />
remarkable tower of rock which crowns the ridge, and is visible<br />
even from the Darial road. It will be useful as a finger-post to<br />
future climbers. From this point the view of Kasbek is superb ;<br />
its whole north-eastern face is a sheet of snow and ice, broken by<br />
the steepness of the slope into magnificent towei's, and seamed<br />
by enormous blue chasms.<br />
We were glad to find that there was a reasonable prospect of<br />
descending from our eyrie to the lower world without too much<br />
difficulty. The ci-est of the ridge between the two glaciers fell<br />
rapidly before us, and offered for some way an easy route. We<br />
followed it— sometimes crossing a snowy plain, sometimes huirying<br />
down rocky banks— until we saw beneath us, on our left, a series<br />
of long snow-slopes leading directly to the foot of the northern<br />
glacier. Down these we glissaded merrily, and at 5.30 halted on<br />
the rocks below the end of the glacier, which was of considerable<br />
size and backed by two lofty summits. The view of the lower<br />
part of the glen was shut out by a rocky barrier, and before we<br />
reached its brow, mists, which we had previously observed collecting