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
Along the northern coast, almost every district has its principal
river, and most of them are navigable up to the maritime capitals
for native vessels of considerable burthen; but they all have the
disadvantage of being partially blocked up at their discharge by
extensive bars and mud banks, an evil which is extending with the
increase of agriculture, by reason of the quantify of soil necessarily
washed down in the process of irrigating the land for the rice
cultivation. Most of them require the application of jetties or piers
to deepen the passages at their entrance.
There are no lakes of any considerable size on Java, for that name
cannot be given to the _ráwas_, or swamps, which though swelled to
a considerable size in the wet season, are for the rest of the year
either dried up or choked by vegetation. Of this description are
two extensive tracts; one inland of _Japára_, usually termed by the
Dutch the _Binnen Zee_, or inland sea; and another in the district
of _Semárang_. In _Báglen_ also (one of the native provinces on the
southern side of the island) there is a lake which supplies the
neighbouring country with fish, and along the coast of which a traffic
is carried on in boats.
Extensive swamps are also found in some parts of the native provinces,
and in the mountainous districts of the _Súnda_ country. Several very
beautiful lakes, of small dimensions, are discovered among the hills,
and some of them can evidently be shown to have been formed of the
craters of extinct volcanos.
The general aspect of Java on the northern coast is low, in many places
swampy and overgrown with mangrove trees and bushes, particularly
towards the west. The southern coast, on the contrary, consists almost
entirely of a series of rocks and cliffs, which rise perpendicularly
to a considerable height. In the interior, stupendous mountains
stretch longitudinally throughout the island, while others of an
inferior elevation, and innumerable ranges of hills running in
various directions, serve to form and confine plains and valleys of
various elevations and extent. On the northern side, the ascent is in
general very gradual, from the sea-coast to the immediate base of the
mountains; particularly in the western parts of the island, where it
has the greatest breadth, and where the mountains are situated far
inland. In approaching the mountains, which lie at the back of Batavia,
there is a gradual but almost imperceptible acclivity for about forty
miles. In other parts, where the mountains and hills approach nearer to
the coast, the ascent is of course more abrupt, as may be observed in
the vicinity of _Semárang_.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account