lofty snowy mountains on the southern side. On the north only one glacier of any size joins in, and it is evident that the southern range gets far the greater portion of the snowfall, although the mountains on the north are in some cases very little inferior in height. The Crevasse Glacier seemed to me to be retiring ; at any rate I should certainly say it was not advancing, for the moraine was deposited some few hundred yards in advance of the ice of the glacier, and there were marks of glacial action on the mountain-sides far above the present level of the glacier. The small glaciers—those resembling clotted cream—on the mountain slopes were certainly retiring. The glacier was very much lower in the centre than at the sides, and at the sides were the remains of successive beds of conglomerate, compact and hard, and level at the top, of a different character altogether to glacial moraine, so that it appeared as if there had formerly been a thick bed of conglomerate filling up the valley, and that it had now been swept out by the glacier. This, however, is only in the lower half, where the mountain slopes are comparatively gentle and formed of shingle ; higher up, the sides are precipitous, and there are no signs of the conglomerate formation. The fall of the glacier as far as we went was two thousand two hundred and eighty feet in twenty-four thousand four hundred yards, or about one in thirty-two. Its general direction is N.N.W.
It was a glorious morning as we descended the glacier—
clear and bright, as it can be only at these great mountain heights. I set off at a good pace ahead of the men and ponies, so as to get back to the luxury of my larger tent, table, chairs, books, and papers as quickly as possible. As I approached the Suget Jangal camp, the men, when they saw me alone came rushing out, thinking something desperate must have happened. I told them that all the matter was that I wanted some lunch and a change of lower garments, for I had had
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