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The Java Sea covers the southern section of the 1,790,000 km 2 (690,000 sq mi) Sunda Shelf. A shallow sea, it has a mean depth of 46 m (151 ft). It measures about 1,600 km (990 mi) east-west by 380 km (240 mi) north-south [4] and occupies a total surface area of 320,000 km 2 (120,000 sq mi).
The rise of sea level during a meltwater pulse 14,600 to 14,300 years Before Present was as much as 16 meters within 300 years. [6] Present sea levels submerge a number of Pleistocene paleo river systems that drained much of Sundaland during the last glacial maximum 18,000 to 20,000 years ago. [7] To the east of the Sunda Shelf is the Sahul Shelf.
The strait is notoriously difficult to navigate because of this shallowness, very strong tidal currents, sandbanks, and man-made obstructions such as oil platforms off the Java coast. [ 3 ] For centuries, the strait was an important shipping route, especially during the period when the Dutch East India Company used it as the gateway to the ...
The Sahul Shelf and the Sunda Shelf today. The area in between is called "Wallacea"Sundaland [1] (also called Sundaica or the Sundaic region) is a biogeographical region of Southeast Asia corresponding to a larger landmass that was exposed throughout the last 2.6 million years during periods when sea levels were lower.
It is 3,200 kilometres (2,000 mi) long with a maximum depth of 7,290 metres (23,920 feet). [2] Its maximum depth is the deepest point in the Indian Ocean . The trench stretches from the Lesser Sunda Islands past Java , around the southern coast of Sumatra to the Andaman Islands , and forms the boundary between the Indo-Australian plate and ...
Flores Sea. The seas that border the Flores Sea are the Bali Sea (to the west), the Java Sea (to the northwest), and the Banda Sea (to the east and northeast). The Indian Ocean and the Savu Sea lie to the south but are separated from the Flores Sea by various islands. Islands that border this sea are the Lesser Sunda Islands and Celebes (Sulawesi).
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Since it is relatively shallow, with the depth of 50 metres (160 ft) or less, the volume transported by the current is relatively small. [12] A 2007–2008 study by a group of Indonesian and Chinese researchers found that the transport volume averaged 500,000 m 3 /second (or 0.5 Sv) with a net southward direction (i.e. to the Java Sea). [13]