From Sumatra on the W., Java is separated by the Sunda Strait, which at
the narrowest is only 14 m. broad, but widens elsewhere to about 50 m.
On the E. the strait of Bali, which parts it from the island of that
name, is at the northern end not more than 1½ m. across. Through the
former strong currents run for the greater part of the day throughout
the year, outwards from the Java Sea to the Indian Ocean. In the strait
of Bali the currents are perhaps even stronger and are extremely
irregular. Pilots with local knowledge are absolutely necessary for
vessels attempting either passage. In spite of the strength of the
currents the Sunda Strait is steadily being diminished in width, and the
process if continued must result in a restoration of that junction of
Sumatra and Java which according to some authorities formerly
existed.[2]
In general terms Java may be described as one of the breakwater islands
of the Indian Ocean--part of the mountainous rim (continuous more or
less completely with Sumatra) of the partially submerged plateau which
lies between the ocean on the S. and the Chinese Sea on the N., and has
the massive island of Borneo as its chief subaerial portion. While the
waves and currents of the ocean sweep away most of the products of
denudation along the south coast or throw a small percentage back in the
shape of sandy downs, the Java Sea on the north--not more than 50
fathoms deep--allows them to settle and to form sometimes with
extraordinary rapidity broad alluvial tracts.[3]
Public-domain text, read in full here on John Shaqi.
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