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e. Lima is more than ninety leagues distant from the nearest active volcano, that of Arequipa. But the earthquakes of the Peruvian capital are uniformly independent of any state of activity in that volcano, and it is certain that the town of Arequipa, which lies at the foot of the mountain, experiences fewer earthquakes than Lima. Of the six serious earthquakes, the dates of which I have mentioned, only that of 1687 stands in connection with a decided shock in Arequipa, and an eruption of the volcano. Earthquakes are of rarer occurrence in the mountainous districts than on the coast, yet Huancavellica, Tarma, Pasco, Caramarca, have been visited by heavy shocks; and within a recent period the village Quiquijana, in the Province of Quipichanchi, Department of Cusco, suffered from a serious commotion. In a letter from an eye-witness I received the following account of it. "In November, 1840, the earth began to move faintly back and forward, and a dull, distant, subterraneous noise continued without interruption. The first powerful shock occurred on the 23d of December. During the whole month of January, 1841, heavy thunder prevailed, but without any motion of the earth. On February 11th, we again had a smart shock, and from that day the vibrations recommenced, which, strange enough, were always most violent on Mondays and Thursdays. The subterraneous noise resounded incessantly; but it was heard only in the village; for at the distance of half a league from it all was tranquil. The heaviest shocks were felt in a circuit within the radius of three leagues. From May 21st to June 2d, all was tranquil; after the last-mentioned date the vibrations recommenced, and frequently became heavy commotions. They continued until the middle of July, 1841. From that time we have not been disturbed, and we have now returned to the ruins of our village." The volcano of Arequipa, which is forty-five leagues distant from Quiquijana, manifested, during the whole of this time, no unusual phenomena, a circumstance which speaks forcibly against the idea of any local connection between the earthquake and the volcano. On most men earthquakes make a powerful and extraordinary impression. The sudden surprise, often in sleep, the imminent danger, the impossibility of escape, the dull subterraneous noise, the yielding of the earth under the feet,--altogether make a formidable demand on the weakness of human nature. Humboldt in the Cosmos truly
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