One side of the creek was formed by a spur of mica-slate; the head by a cliff of ice about forty feet high; and the other side by a promontory fifty feet high, built up of huge rounded fragments of granite and mica-slate, out of which old trees were growing.

This promontory was evidently a moraine, heaped up at a period when the glacier had greater dimensions.
When we reached the western mouth of this northern branch of the Beagle Channel, we sailed amongst many unknown desolate islands, and the weather was wretchedly bad.

We met with no natives.

The coast was almost everywhere so steep that we had several times to pull many miles before we could find space enough to pitch our two tents: one night we slept on large round boulders, with putrefying sea-weed between them; and when the tide rose, we had to get up and move our blanket-bags.

The farthest point westward which we reached was Stewart Island, a distance of about one hundred and fifty miles from our ship.