146 
duced the author to infer that they were due to an eruption in the 
Cape de Verd group. 
In June, 1822, the ship Kingston, of Bristol, bound to Jamaica, 
while passing near Fogo, had her sails covered with a similar brown- 
ish triturated pumice, which it is stated smelt strongly of sulphur. 
Mr. Clarke also mentions the following instances of similar phe- 
nomena. on the authority of the officers of the Roxburgh :-— 
In the lat. of the Canaries, and long. 35° W., showers of ashes 
have been noticed two or three times. At Bombay the decks of the 
vessels were on one occasion covered to the depth of an inch with 
dust, which was supposed to have been blown from Arabia. 
In January, 1838, dust was noticed by the crew of a vessel navi- 
gating the China sea, a considerable distance from the Bashee islands, 
one of which had been previously seen in eruption*. 
In 1812, ashes fell on the deck of a packet bound to the Brazil, 
and when 1000 miles from land. 
Mr. Clarke also mentions the ashes which fell at sea during the 
eruption of Vesuvius in 1822, and 400 miles from that volcano ; 
likewise the reddish dust which fell in the south of Italy and in Sicily 
on the 16th May, 1830, as well as in 1807 and 1818, during eruptions 
of Etna, and at first attributed to those outbursts, but afterwards 
found to be sand similar to that of the desert of Africa. During the 
eruption in May, 1830, a caravan perished beneath a whirlwind of 
sand, and similar storms occurred during the eruptions of 1807 and 
1813. 
A letter was then read from Mr. Caldcleugh, dated St. Jago de 
Chili, 18th February, 1839, containing the following translation of 
Pt aaa of the master and crew of the Chilian schooner 
ily. 
“I, the undersigned, Joseph Napoleon Escofier, master of the said 
vessel, and with the corroborating evidence of my crew, declare as 
follows :— 
««This, the 12th day of February, 1839, at ten minutes past 9 
o'clock in the morning, being in lat. 33° 32/S., and 74° 32! W. long. 
of the meridian of Cadiz (80° 51! W. of Greenwich), we felt an earth- 
quake, which lasted more than a minute. The noise which accom- 
panied it was similar to that caused by the running out of a heavy 
chain cable. At fifteen minutes past 7 o’clook of the same evening 
we saw an island rising out of the sea, of the height of Curauma 
Point, bearing south 79° W. by compass, distant from six to nine miles. 
A considerable time afterwards the island divided itself into the form 
of two pyramids, the most northern one crumbled away diagonally 
towards the north, and the southern one disappeared in pieces, the 
base however always remaining above the surface of the sea. At 
half-past 7 o’clock the same island appeared again, or its size be- 
came considerably increased, but shortly afterwards its summit be- 
* Mr. Clarke believes that this is the first announcement of a voleano in 
that group. 
¢ Bulletin, Soc. Geol. France. 
