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We cannot question that the earth, when split open and shaken by shocks, sometimes emits gaseous substances into the atmosphere in places remote from active volcanoes. At Cumana, as we have already observed, flames and vapors mixed with sulphurous acid rise from the most arid soil. In other parts of the same province the earth throws up water and petroleum. At Riobamba, a muddy, inflammable mass, called moya, issues from crevices that close up again and pile up into hills. Seven leagues from Lisbon, near Colares, during the terrible earthquake of the 1st of November 1755, flames and a column of thick smoke rose up from the rock face of Alvidras and, according to some witnesses, from the depths of the sea. This smoke lasted several days and was thicker when the underground noises accompanied the strongest tremors.

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