The History of Java, v. 1-2Raffles, Thomas Stamford, Sir
History
The History of Java, v. 1-2
Raffles, Thomas Stamford, Sir
Java (Indonesia) -- History
which are excavated, in a similar manner, by the streams of the
descending water.
"Near the centre, somewhat inclining to the west side, it contains
an irregular oval lake, or collection of water, whose greatest
diameter is nearly one hundred yards: it dilates into several
branches. The water is white, and exhibits truly the appearance
of a lake of milk, boiling with a perpetual discharge of large
bubbles, which rise with greatest force from the eastern side.
The heat is 112° of Fahrenheit's scale: the apparent boiling
arises from a constant development of fixed air. The water has a
sulphureous odour; its taste is astringent, somewhat saline. Shaken
in a bottle it explodes its fixed air with great violence. The
sides of the lake, to some distance, are lined by a white aluminous
earth, most impalpably fine, and very loose, on which account it is
very difficult to approach the water. In attempting to examine its
temperature, and to collect for analysis, I sunk into the earth to
a considerable distance, and found it necessary to dispose large
fragments of basaltes before I was able to pass over it. This
earth consists of the clay (alumine) of the lavas dissolved by the
sulphureous steams on the bottom of the crater; it is of the purest
kind, and divided to a degree minute almost beyond conception.
Large quantities have been several times thrown out of the ancient
craters of the island. One eruption of this substance occurred
in the year 1761 from the mountain Gedé: it was considered as an
eruption of ashes.
"I was witness to a similar eruption, which occurred from the
mountain of _Klut_, in the month of June last year. The earth very
much resembled ashes, and was so impalpably fine and light, that
the common breeze of the monsoon carried it from this mountain,
situated in the longitude of Surabáya, to Batavia and farther
westward. It possessed the properties of the purest clay, and being
mixed with water became viscid and ductile. It can easily be formed
into vessels, and if procurable in large quantities, might usefully
be employed in the arts. All its properties indicated sufficiently
that it was the alumine of the lavas, divided in an extreme
degree by the causes above-mentioned. The Javanese are not wholly
unacquainted with the properties of this earth. It is a custom
amongst silversmiths to collect the ashes thrown out by similar
eruptions, for the purpose of making _moulds_ for the finest works.
Public-domain text, read in full here on John Shaqi.
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