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THE NEW ZEALAND ALPS

Plateau; and, lastly, the northern ridge, connecting with the main divide between Mount Tasman and St. David's Dome. A comparatively low rock saddle in this ridge occurs between the highest peak of Aorangi and the junction with the main divide, leading on one hand into the Linda Glacier, and on the other to the head of the Hooker Glacier. Aorangi is thus quite cut off from the west coast, and has, in fact, no 'western flanks,' as is generally supposed.

It was an intensely hot day, and scarcely a breath stirred as Harper, Annan, and I struck out on the now well-known route across the Ball and Hochstetter Glaciers for the Haast Ridge, but the clear mountain air seemed to rush into our lungs, putting health and strength into every fibre.

The mountains were glorious in the noonday glare, and the foliage on their lower slopes was in its gayest height of blossom. Now and then an avalanche would thunder down in the ice-fall or from the higher slopes above, or the whistle of a kaka down the valley could be detected. These and the merry tinkling of the surface streams were the only sounds to break the spell of silence and benignant peace which seemed to reign over all. These are the scenes which go straight to the heart of the true nature-loving mountaineer.

To reach the foot of the couloir by which three years previously Dixon, Inglis, and I had descended involved the usual amount of hot scrambling up tali or fans of detritus from the rocks above. Once in the couloir (which was snow-filled in places) we were not long in reaching our old bivouac, where we deposited our first batch of provisions, &c., our plan being