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THE ASCENT OF MOUNT EREBUS. resembled a lion couchant. To our surprise the lion appeared now to be blowing smoke out of his mouth.

The origin of the mounds was no longer a mystery; they were the outward and visible signs of fumaroles. In ordinary climates, a fumarole, or volcanic vapour well, may be detected by the thin cloud of steam above it, like breath exhaled on a frosty day, and usually one can at once feel the warmth, by passing one’s hand into the vapour column; but, in the rigour of the Antarctic climate, the fumaroles of Erebus have their vapour turned into ice as soon as it reaches the surface of the snow plain. Thus ice mounds, somewhat similar in shape to the sinter mounds formed by the geysers of New Zealand, of Iceland, and of Yellowstone Park, are built up around the orifices of the fumaroles of Erebus. When exploring one of these fumaroles, Mackay fell suddenly up to his thighs into one of its concealed conduits; he saved himself however, from falling in deeper still, with his ice axe. Marshall had a nearly similar experience at about the same time. Eventually we all arrived safely at our camp soon after 6 p. m., and found Brocklehurst progressing as well as could be expected.

As we sat on the rocks at tea, we had a glorious view to the west. While the foothills of Erebus