ment we made 3,640 feet—much the same altitude as our Ball Glacier camp. The survey of the glacier has, however, since been effected, and this point determined as 3,305 feet.
The moraine is composed of unusually large polyhedral masses of rock, and is 200 feet in height at the main exit of the river, which is situated about the middle of the terminal face.
A backward view down the valley revealed but one distant peak—Mount Sealy—the northernmost of the Ben Ohau Range. This peak was evidently the only one from which the clear ice of the Murchison can be seen, if we except those of the Liebig and Malte Brun Ranges, and as none of these peaks have been ascended, this fact probably accounts for the Murchison Glacier, which is the second largest in New Zealand, having lain so long unexplored.
Proceeding up on the western side of the moraine, a new branch glacier descending from the Malte Brun Range opened out on our left, its lower ice forming a fine frozen cascade, whilst a waterfall of some 200 feet descends over a rocky face from its southern and hanging portion. To this glacier and fall we have given the name of 'Onslow,' in honour of his Excellency the Earl of Onslow.
As it was now getting dark we decided to bivouac for the night, and selecting a bed of small gravel amongst the larger stones of the moraine, we dined scantily on cold mutton and tea, and wriggling into our waterproof blanket-bags were soon ready for sleep. At first all our attempts at slumber were rendered futile by a congregation of keas, who hopped around
