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Updated: May 4, 2025


I was prevented by the bad weather from making trips to any distance, but one afternoon I drove to Tivoli. The road leading thither is called the Tiburtinian. After travelling for about six miles we become conscious of a dreadfully offensive sulphurous smell, and soon find that it proceeds from a little river running through the Solfatara.

It was as weak as water, and tasted like the solfatara of Tivoli, but it came from his own vineyard in Germany, and was at least fifty years old. If he has a vineyard, he has a castello, of course. And if he has a castello, he is a gran' signor, eh? what do you think, Sor Conte? You know about such things." "I did once, maestro mio. It is very likely."

We recall the fact that the whole Solfatara phenomenon had its origin in a flame being swayed over one of the fango holes.

Guadaloupe, an active volcano, the height of which, according to Leboucher, is 799 toises; according to Amie, 850 toises. Montserrat, a solfatara; fine porphyritic lavas with large crystals of feldspar and hornblende near Galloway, according to Mr. Nugent. Nevis, a solfatara. St. Christopher's, a solfatara at Mount Misery. St.

Now, I wish you would take a carriage, and go and take the ladies on an excursion along the bay to the westward, and show them Virgil's Tomb, and the Grotto of Posilipo, and Pozzuoli, where the apostle Paul landed on his famous journey to Rome, and the temple of Serapis, half under water, and the great amphitheatre, and the Solfatara, which is the crater of a volcano almost extinct.

South of Burauen rises the mountain ridge of Manacagan, on the further slope of which is a large solfatara, which yields sulphur for the powder manufactory in Manila, and for commerce. A Spanish sailor accompanied me. Where the road passed through swamp we rode on carabaos.

At present, as we hear from travellers who have ascended it, the crater, like that of Popocatepetl, is in the condition of a solfatara, sending out jets of steam and sulphurous acid gas.

I did not reach the place, as the guide whom I had with difficulty obtained, pretended, after a couple of miles, to be dead beat. From the inquiries I made, however, I apprehend that it is a kind of solfatara. Several deposits of it appear to exist at the foot of the Makiling. Upon the shore, on a bare rock, I found four eggs containing fully developed young crocodiles.

This last substance is very common at Teneriffe, where it forms the basis of the tephrinic lava. These analogies between the peak of Teneriffe and the Solfatara of Puzzuoli, might no doubt be shown to be more numerous, if the former were more accessible, and had been frequently visited by naturalists.

That the response in a place like the Solfatara is what we have seen it to be, is the result of an extraordinary lability of the equilibrium between gravity and levity, a characteristic appertaining to the earth's volcanism in general.

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