Stretching over to the eastern side of the channel we passed close to Crozier Island, having Cape Constitution full in view. Its appearance coincides exactly with the description given by Morton.
This cape is the northern extreme of a bay called, by Kane, Lafayette Bay. It is steep and precipitous, and has no ice-foot adhering. Indeed, the base of the headland, as well as the adjacent one, Cape Independence, has the appearance of having been partially undermined by the action of the sea, thus forming an overhanging terrace, up which it would be impossible to ascend. Morton found its ascent totally impracticable, on account of the steep and rugged nature of the cliff. We were unable to detect any signs of a _mer de glace_ over this land, although a light tinge along the summit to the southward of Lafayette Bay would lead one to suppose that it existed. This, however, was the only indication of an ice-cap that was perceived, and it was one on which little or no reliance was placed.
The positions of the various points along this coast are very fairly correct, being as nearly as possible in the latitudes ascribed to them by Dr. Bessels of the "Polaris," affording a striking contrast to the places on the opposite side of the channel, where the positions are so egregiously inaccurate. The deep inlet on the American chart called Carl Ritter Bay was not to be seen. The only indentation in the land in its assigned position was Richardson Bay, which we must naturally conclude was the one seen and named Carl Ritter by Dr. Hayes.
It was a curious fact that, whereas the land on the west side of the channel was completely covered with snow, the land on the east side was entirely free. This was not the only peculiar feature in which the two sides of the channel differed. Although apparently of the same geological formation, there was a great dissimilarity between the physical appearance of the land on either side. That on the east was flat and table-topped, rising to the height of about one thousand feet, separated into hills by broad valleys, whilst the stratification of the cliffs was regular and horizontal. That on the west side was, on the contrary, composed of conical-shaped hills, rising to an altitude of from two to four thousand feet, and intersected by deep ravines, whilst the stratifications were so distorted that the dip varied as much as from 10° to 45°.