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While on the spot I sketched a view (17) of the crater's interior edge as it is seen on the descent through the eastern wall's breach. Nothing is more striking than the superimposition of these lava strata, which reveals similar sinuosities to the calcareous rock of the Alps. These enormous ledges, sometimes horizontal and sometimes sloping or undulating, reminded us that long ago the entire mass had flowed, and that a combination of disruptive causes determined a particular flow. The Crest of the wall exhibits the same strange ramifications we find in coke. The northern edge is the highest. Towards the south-west the wall has considerably subsided and an enormous amount of scoria seems glued to the outer edge. On the west the rock is perforated, and through a wide opening you can see the sea and horizon. Perhaps the force of the steam broke through here just when the lava overflowed from the crater.

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