The First Descent Down The Terminal Wall Of The Crater Is Very Precipitous, But It And The Slope Which Extends

To the second descent are thickly covered with ohias, ohelos (a species of whortleberry), sadlerias, polypodiums, silver grass, and a

Great variety of bulbous plants many of which bore clusters of berries of a brilliant turquoise blue. The "beyond" looked terrible. I could not help clinging to these vestiges of the kindlier mood of nature in which she sought to cover the horrors she had wrought. The next descent is over rough blocks and ridges of broken lava, and appears to form part of a break which extends irregularly round the whole crater, and which probably marks a tremendous subsidence of its floor. Here the last apparent vegetation was left behind, and the familiar earth. We were in a new Plutonic region of blackness and awful desolation, the accustomed sights and sounds of nature all gone. Terraces, cliffs, lakes, ridges, rivers, mountain sides, whirlpools, chasms of lava surrounded us, solid, black, and shining, as if vitrified, or an ashen grey, stained yellow with sulphur here and there, or white with alum. The lava was fissured and upheaved everywhere by earthquakes, hot underneath, and emitting a hot breath.

After more than an hour of very difficult climbing we reached the lowest level of the crater, pretty nearly a mile across, presenting from above the appearance of a sea at rest, but on crossing it we found it to be an expanse of waves and convolutions of ashy-coloured lava, with huge cracks filled up with black iridescent rolls of lava, only a few weeks old.

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