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Updated: May 2, 2025


It has been stated by M. Fouqué that the age of the more ancient volcanic beds of Santorin belong, as shown by the included fossils, to the newer Pliocene epoch. These are of course the unsubmerged, and therefore more recent strata, and may have been recently upheaved during one or more of the outbursts of volcanic energy.

We shall have to refer again to these curious vases when we speak of the discoveries made at Troy; we need only add now that the pottery found at Santorin differs completely, alike in form and ornamentation, from the Greek, Phoenician, and Etruscan specimens, of which the museums of Europe contain so many. They are evidently therefore not of foreign origin, but of native manufacture.

This eruption went on until 1870, and the quantity of scoriae vomited forth during its continuance welded three islets, which had hitherto been separate, to the principal island, of which they now form part. On entering the Bay of Santorin we see on every side banks of lava, beds of scoriae, and piles of cinders of a purplish-gray color rising in cliffs to a height of more than 1,312 feet.

But the Nautilus kept on its journey, which, I learned, took us to the Torres Strait, the Papuan coast, through the Red Sea, through a subterranean strait, under the Isthmus of Suez, to the island of Santorin, the Cretan Archipelago, to the South Pole, on whose sterile wastes Captain Nemo reared his black flag with a white "N" upon it, and through the Gulf Stream.

And know also, oh Padishah, that, but the other day, a new island rose up from the sea beside the island of Santorin, and this new island has grown larger and larger during three successive months, and all the time it was growing, the ground beneath Stambul quaked and trembled.

The Bay of Santorin, in the island of that name, which lies immediately to the north of Crete, has long been noted for its submarine volcanoes. According to one account, indeed, the whole island was at a remote period raised from the bottom of the sea; but this is questionable.

Santorin is a striking and brilliant proof of their progress, and we shall appreciate this progress yet more when we have examined the ruins piled up on the hill of Hissarlik. There we shall close this portion of our work, for from the time when the buildings of which these remains were the relics met their doom, the use of metals, copper, bronze, gold, silver, and iron became general.

The Breton megalithic monuments also contained numerous fragments of pottery, some of which had formed part of vases without stands, such as those found at Santorin and at Troy. In other parts of France, similar discoveries have been made; shells often brought from distant shores, glass beads, amber bowls, hatchets and celts made of stone foreign to the country. Dr.

These pieces of wood, the size of which varies considerably, were probably added to give the necessary solidity to the walls in the numerous earthquakes, the disastrous effects of which were only too well known to the ancient inhabitants of Santorin.

We soon left it in our wake, and also passed the Brothers' Islands, and many others, some of them small and uninhabited, besides separate colossal rocks, towering majestically into the sea. Soon afterwards we passed the islands Santorin and Anaph. The latter of these islands is peculiarly beautiful.

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