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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.