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THE ADAI KtlOKll GROUP 137<br />

which the sun's last rays rested longest. Clouds spoilt my panorama<br />

from the summit of Shoda, but this short glimpse had been enough<br />

to suggest a solution of the problem.<br />

In 1889, before undertaking the search for traces of our friends<br />

lost in the previous year on Koshtantau, we gave our Swiss guides<br />

a training walk in the Adai Khokh Group. We forced the glacier<br />

pass I had planned in 18G8, between the Zea Valley and the<br />

Mamison Pass. We left the half- ruined refuge on the south side<br />

of the Mamison at 2 a.m., and knocked up the Cossacks at St.<br />

Nikolai at 9 p.m. The ascent was by the glacier which gives<br />

birth to the Ardon. We had a very extensive view over Ossetia<br />

to the south, a region of isolated mountains and high grass-passes,<br />

where the main chain changes its character, as the Alps do<br />

beyond the Simplon. What we saw on the farther side was<br />

more limited and less agreeable. Four hours were spent in<br />

descending a very difficult rock-wall, only 400 feet high, on to<br />

the Zea snowfields. There was seldom foothold and handhold at<br />

the same time ; and, as all the grooves and hollows Avere sheeted<br />

with ice, there was much of that interminable w^ork known to<br />

climbers as step-cutting. We were a party of eight, on two<br />

ropes it is true, but still more than twice too many. Our Oberlanders<br />

were somewhat out of condition and heart ; they had not yet<br />

taken the measure of life in the Caucasus. We on the last rope<br />

were hampered by the terror of sending down stones on those<br />

in front. Wherever it was possible to find a perch we halted till<br />

they were out of range, and I succeeded in utilising such leisure<br />

moments in making rough outlines and notes of the peaks and<br />

ridges that encompassed us. Opposite was the Mamison Peak,<br />

or Khamkhaki Khokh. From this side it loses its symmetry<br />

and exhibits a long rib of rock and ice, running down to sepa-<br />

rate the two basins of the Zea. The northern snowfield is by<br />

far the more extensive. Over this appeared the double peak of<br />

the Piion Valley, masking the summits beyond it. To its right,'<br />

hemming in the head of the invisible Songuta Glacier, rose a<br />

' I doubt if there be any direct pass from the Zea nSve to the Songuta Glacier.

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