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o is described as apothecary to the Grand Duke, first detected the presence of boracic acid in the lagoon Orcherio, near Monte Botardo. Masgagin, a professor of anatomy, found the mineral in a concrete state in several streams issuing from the lagoons, and suggested the propriety of establishing manufactories of borax. As late, however, as 1801, in consequence of the failure of numerous experiments, Professor Gazzeri arrived at the conclusion that the quantity of acid contained in the water of the lagoons was too small to render the working of them profitable. But this opinion was based on the old practice of attempting the extracting the mineral by the use of charcoal furnaces. It was M. Larderel who introduced the improved method of employing the hot vapors of the lagoons themselves in the elaboration of the acid, and may be said to have invented the present method, which will probably go on improving for ages. The system of the Chevalier Larderel, now Comte de Pomerasce, displays at once great ingenuity and courage. The _soffioni_, or vapors, having been observed to burst forth with more or less vehemence in various parts of the mountains--which, fortunately for industry and commerce, are copiously irrigated with streams of water--the idea was conceived of forming an artificial lagoon on the site of the most elevated vent. A large basin having been excavated, the nearest stream was turned into it. The burning blasts from below forcing up their way through the water, keep it in a state of perpetual ebullition, and by degrees impregnate it with boracic acid. Nothing can be more striking than the appearance of such a lagoon. Surrounded by aridity and barrenness, its surface presents the aspect of a huge caldron, boiling and steaming perpetually, while its margin trembles, and resounds with the furious explosions from below. Sometimes the vapor issues like a thread from the water, and after rising for a considerable height, spreads, and assumes an arborescent form as it is diluted by the atmospheric air. It then goes circling over the surface of the lagoon, till, meeting with other bodies of vapor in a similar condition, the whole commingling, constitute a diminutive cloud, which is wafted by the breeze up the peaks of the mountains, or precipitated into the valleys, according to its comparative density. To stand on the brink of one of these deadly lakes, stunned by subterranean thunder, shaken by incessant earthquak
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