Valley are instructive and interesting. The highest of them are distinctly marked all down the valley for a distance of forty miles from Sebastopol—a large face of ice-worn rock near the Hermitage—on the eastern slopes of the Ben Ohau Range. The story of the ancient glacier can be read as the eye follows these strange terraces from their starting point 2,000 feet above the valley bed, down a gentle declination to the terminus of the Ben Ohau Range.
Before going into the narrative of my five seasons' climbing amongst the peaks and glaciers around Aorangi, it would be as well for me to describe, as concisely as possible, the general topography of the Mueller, Hooker, and Tasman Glaciers.
We will suppose ourselves in the main Tasman Valley, into which all these glaciers drain, close to the point where the valley first branches. As we look northward, Aorangi and the range running southward for twelve miles from the main body of the mountain bound the view, and divide the valley into two branches. Let us take the one to the north-west first. Proceeding up this valley of the Hooker for a few miles, we arrive at a branch valley from the left or west—the Mueller Valley— completely occupied by the glacier of the same name. Close to the Mueller Glacier is situated the Hermitage, presided over by Mr. F. F. C. Huddleston, a true haven of refuge and comfort for the wearied tourist or mountaineer.
We step on to the Mueller Glacier, here completely covered by moraine, and, turning westwards, strike up its course. On our right, 8,500 feet above us, clad in ice and snow and glittering in the sunlight, rises the
