mali, on the peninsula of Abscheron, in the Caspian Sea; that of Damak, in the province of Samarang, in the island of Java; the Salses of Girgenti in Sicily, and Sassueto in Northern Italy, &c., &c.
One of the most remarkable of this class is the one described by Humboldt. This is situated at Turbaco, near Carthagena, in New Grenada, South America. It consists of some fifteen or twenty cones from nineteen to twenty-five feet high, and measuring round the base from seventy-eight to eighty-five feet each. These cones, or Volcancitos, as they are called in the language of the country, have a hollow on the top, measuring from fifteen to thirty inches in diameter, and filled in the driest seasons with muddy water, through which air-bubbles are constantly escaping: the temperature of the water is not higher than that of the surrounding atmosphere.
Earthquakes are intimately connected with volcanoes; they often precede volcanic eruptions, and arise from the same cause—viz., from the movement of matter in the interior of the earth; only that their action is much more formidable and destructive, and the changes produced by them in the globe are much more varied and extensive. Landslips on the sides of mountains are most frequently attributable to them; they give rise to the formation of new lakes, and cause old ones to disappear; islands are swallowed up by them, and new ones arise in the sea as by magic; parts of continents subside and sink, and others are elevated; the relative positions
