Considering the great wealth of the Dutch Indies, it is a little
surprising that so few young men are tempted to go out there to seek
their fortunes. As is usually the case in the tropics, those parts of the
coasts which are low and marshy are very unhealthy for Europeans, who
cannot stay in such places for any length of time without falling victims
to malaria, though the Malays do not seem to be affected by the climate;
but higher up, from 500 to 1000 feet above the sea, it is healthy enough,
and up the hills, in the larger islands, the climate leaves little to be
desired. The temperature generally varies between 70 and 90 degrees all
the year round, though there is a certain amount of difference between
one island and another. North of the equator the rainy monsoon lasts from
October to April, and the dry season from April to October, while on the
south side these seasons are reversed. On the line, however, the
trade-winds and monsoons appear very irregularly, because there are four
seasons instead of two--that is to say, two rainy and two dry--and the
weather is also subject to frequent changes of a local character,
especially in the neighbourhood of mountain-ranges and volcanoes. With
the exception of Borneo and the central part of Celebes all these islands
are volcanic. In the principal group, which stretches from Sumatra and
Java to the Timor Laut archipelago, there are no less than thirty-three
active volcanoes, of which twelve are in Java, besides a number of
so-called extinct ones which may at any moment burst into renewed life.
Some of the smaller islands are merely sunken volcanoes, such as Gebeh,
for instance, and the Banda Islands, where the 'Goonong Api'
(Fire-Mountain) is a living proof. The best known of all these volcanoes
is the terrible Cracatao, one of the three which may be seen in the
Straits of Sunda. Readers may remember the great eruption of 1886, when
half the island of Cracatao and part of the mountain, which was split
clean in two, were swallowed up in the sea, and parts of the coasts of
Java and Sumatra were overwhelmed by the tidal wave that accompanied the
outburst, ships being lifted bodily on to the land and left perched among
the hills. In one day and night 100,000 persons perished, and except a
slight earthquake, which, as earthquakes are not uncommon in that part of
the world, was naturally not regarded as serious, there was no warning of
the impending disaster, for the crater had shown no signs of life for 200
years. During the eruption a roar as of distant artillery could be heard
in the middle of Java, fully 400 miles from the scene.
Public-domain text, read in full here on John Shaqi.
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