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as bearing it away from us, unfortunately veiled the interior of the crater, which smoked all round from a thousand crannies. At intervals, however, we caught sight through the smoke of the cracked walls of the rock. The view was neither instructive nor delightful; but for the very reason that one saw nothing, one lingered in the hope of catching a glimpse of something more; and so we forgot our slow counting. We were standing on a narrow ridge of the vast abyss; of a sudden the thunder pealed aloud; we ducked our heads involuntarily, as if that would have rescued us from the precipitated masses. The smaller stones soon rattled, and without considering that we had again an interval of cessation before us, and only too much rejoiced to have outstood the danger, we rushed down and reached the foot of the hill together with the drizzling ashes, which pretty thickly covered our heads and shoulders.... The news [two weeks later] that an eruption of lava had just commenced, which, taking the direction of Ottajano, was invisible at Naples, tempted me to visit Vesuvius for the third time. Scarcely had I jumped out of my cabriolet at the foot of the mountain, when immediately appeared the two guides who had accompanied us on our previous ascent. I had no wish to do without either, but took one out of gratitude and custom, the other for reliance on his judgment--and the two for the greater convenience. Having ascended the summit, the older guide remained with our cloaks and refreshment, while the younger followed me, and we boldly went straight toward a dense volume of smoke, which broke forth from the bottom of the funnel; then we quickly went downward by the side of it, till at last, under the clear heaven, we distinctly saw the lava emitted from the rolling clouds of smoke. We may hear an object spoken of a thousand times, but its peculiar features will never be caught till we see it with our own eyes. The stream of lava was small, not broader perhaps than ten feet, but the way in which it flowed down a gentle and tolerably smooth plain was remarkable. As it flowed along, it cooled both on the sides and on the surface, so that it formed a sort of canal, the bed of which was continually raised in consequence of the molten mass congealing even beneath the fiery stream, which, with uniform action, precipitated right and left the scoria which were floating on its surface. In this way a regular dam was at length thrown up, in wh
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