from the new islet, there was
thrown up a chain of black calcined rocks, followed by volumes of thick
black smoke, having a sulphurous smell. A few days thereafter the water
all around the spot became hot, and many dead fishes were thrown up.
Then, with loud subterraneous noises, flames arose, and fresh quantities
of stones and other substances were ejected, until the chain of black
rocks became united to the first islet that had appeared. This eruption
continued for a long time, there being thrown out quantities of ashes
and pumice, which covered the island of Santorin and the surface of the
sea--some being drifted to the coasts of Asia Minor and the Dardanelles.
The activity of this miniature volcano was prolonged, with greater or
less energy, for about ten years.

In 1866 similar phenomena took place in the Bay of Santorin, beginning
with underground sounds and slight shocks of earthquake, which were
followed by the appearance of flames on the surface of the sea. Soon
after there arose, out of a dense smoke, a small islet, which gradually
increased until in a week's time it was 60 feet high, 200 long and 90
wide. The people of Santorin named it "George," in honor of the King of
Greece. In another week it joined and became continuous with the Little
Cammeni. The detonations increased in loudness, and large quantities of
incandescent stones were thrown up from the crater.

About the same time, at the distance of nearly 150 feet from the coast,
to the westward of a point called Cape Phlego, there rose from the sea
another island, to which was given the name of Aphroessa. It sank and
reappeared several times before it established itself above water. The
detonations and ejection of incandescent lava and stones continued at
intervals during three weeks. From the crater of the islet George, which
attained a height of 150 feet, some stones several cubic yards in bulk
were projected to a great distance. One of them falling on board of a
merchant vessel, killed the captain and set fire to the ship.

By the 10th of March the eruptions had partially subsided, but were then
renewed, and a third island, which was named Reka, rose alongside of
Aphroessa. They were at first separated by a channel sixty feet deep;
but in three days this was filled up, and the two islets became united.

Reference may properly be made here to Monte Nuovo and Jorullo, not that
they appertain to the present subject, but that they form examples of
the