Page:Du Faur - The Conquest of Mount Cook.djvu/239

From Wikisource
Jump to navigation Jump to search
This page has been validated.
MOUNTS DAMPIER AND LENDENFELD
185

on a day's rest at the bivouac. The following day, weather permitting, we would make an attempt on Mount Lendenfeld, a fine snow peak immediately north of Mount Tasman. It is 10,551 feet in height and ranks next to Mount Dampier, being the fourth highest mountain in New Zealand. Mount Lendenfeld was first ascended by the Rev. H. E. Newton and Alex Graham, in February 1907, and had not been attempted since then. They climbed from a high bivouac situated at about 8,000 feet at the head of the Fox Glacier. On reaching the saddle between Lendenfeld and Haast, they first ascended Mount Haast, and then descending to the saddle again, followed the north-east arête to the summit of Mount Lendenfeld. Ours would thus be the first attempt made from the eastern side; if we could once make our way through the maze of broken ice and gain the saddle, we could follow their route up the north-east arête.

In the afternoon Graham and Milne set out to cross the Great Plateau and take a look at the morrow's route. On their return they reported that it seemed practicable as far as they had gone. Well satisfied with our prospects, we made all possible preparations to ensure an early start, and crept into our sleeping-bags at 8 p.m. After sundry twistings and turnings in search of the softest and least stony spot, we relapsed into silence which unfortunately was not always that of sleep.

On April 2nd, at 4 a.m., we stood in the chill starlight outside the tent, putting on the rope and enumerating the contents of the rucksac, to be sure nothing was forgotten. Then we set off, stumbling in the dim light over the boulders that surround the camp. An hour's work brought us to the Great Plateau. The snow was crusty in places, and I reaped the advantage of being about four stone lighter in weight than my guides. They were continually breaking through where I just managed to skim over the surface.