Voyage to the East IndiesPaulinus, a S. Bartholomaeo
History
Voyage to the East Indies
Paulinus, a S. Bartholomaeo
India -- Description and travel -- Early works to 1800
and from four to four and a half in height, is not
common even in India, and is to be found only in
the thickest forests. He gives place to no animals
but the lion, elephant, and rhinoceros.--The Indian
parrots are, in a literal sense, almost innumerable,
for every traveller brings home new kinds to Europe.
The old Grecian name ψιττακη, seems to be of Egyptian
origin: Π-ϹΙΤΤΑΚΗ. The Π is an article: the Germans,
therefore, have omitted it, and converted the word
into _Sittich_. _F._
[69] Many instances may be found, both in ancient and
modern history, of great changes having been
produced on the surface of the earth, and on the
coasts of the ocean, by hurricanes and earthquakes,
as well as by the waters of the sea and by rivers.
That piece of water, known by the name of the Dead
Sea, arose by a fiery eruption from the earth; and
in Egypt, along the northern bank of the Delta, and
on both sides, there are large lakes, particularly
the lakes Mœris and Serbau, which were indebted for
their origin to storms, earthquakes, and inundations
of the Nile. In Peloponnesus, or the present Morea,
the cities of Helice, Bura, and some others in
Achaia, were swallowed up by the sea, two years
before the battle of Leuctra. Even in the eighteenth
century, Callao in Peru was overwhelmed, and, with
all its houses, inhabitants, and the ships in the
harbour, became a prey to the waves of the ocean.
The great changes effected by the earthquake in
Calabria, are still fresh in the memory of every
one: during that horrid catastrophe whole mountains
and rocks were precipitated into the sea. _F._
[70] The low inundated land at the bottom of the Gauts,
which consists of marl or clay and strata of chalk,
together with the higher strata where the mountains
are steep towards the sea, being violently torn away
in the rainy season by the streams and currents
collected in the mountains, form, at their influx
into the sea, banks and accumulations which are
still raised higher, and are driven back by the sea
towards the land. In this manner are formed plains,
islands, and little hills; the origin of which can,
in this manner, be very naturally explained. _F._
[71] In the time of the Romans a freedman of Annius
Plocanus experienced a similar fate. See _Plin.
Hist. Nat._ lib. vi. c. 22. _A._
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