The first intelligence of the breaking out of the volcano, which is the subject of the present paper, was brought to Malta, on the 16th of July last, by a merchant vessel. It was confirmed soon after by Captain Swinburne, of H. M. S. Rapid, who had succeeded in approaching very near the island. The crater of the volcano, which was in great activity, was then only a few feet above the level of the sea. Several shocks of an earthquake had been felt near the same spot about a month before the eruption. The volcano continued active till the 16th of August, and the island it was forming gradually enlarged in all its dimensions; but since that period there has been no fresh eruption. In the end of August, a survey of the island was carefully made by Captain Wodehouse, R. N. of H. M. brig Ferret; and a plan drawn by him is annexed to the present paper. The circumference of the island is about 3240 feet, and its greatest height 107 feet; the circumference of its crater is about 780 feet. The surface of the island is composed entirely of ashes and cinders, without any lava. The crater contained turbid salt water, having a temperature of 200° Fahr. and emitting a constant supply of gas. The water in the immediate neighbourhood of the island was very shallow, not exceeding three or four feet, and the crater was rapidly filling up by the falling in of its margin. The author could not learn that anything unusual had been noticed as having occurred in any of the neighbouring volcanic regions, either at the time of the eruption or immediately antecedent to it. He describes the phænomena, which fell under his own observation, on a visit which he made to the island on the 5th of August. During the most violent eruptions, a large quantity of dense white vapour, resembling snow or bleached wool, rose to a great height in the atmosphere, and assumed various extraordinary forms; this was followed by columns of perfectly black matter, rising to the height of three or four thousand feet, and spreading out very widely, even to windward. The subterranean sounds attending the eruptions were not very loud, and were much exceeded by that of the electrical explosions accompanying the lightning, which was seen to dart in various directions in the atmosphere of the eruption. To leeward of the volcano, the sea was much discoloured by the admixture of ashes and fine dust, and an abundance of light cinders were floating on its surface. Even when the author was enveloped in the dark cloud of ashes falling from the volcano, not the smallest odour of bitumen, of sulphuretted hydrogen, or of sulphureous or any other acid, was perceptible; nor was any inconvenience felt in respiration. No appearance of flame, and but little light, was exhibited during these eruptions.
Read full abstract