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Fishing is an important economic activity in the Java Sea. Over 3,000 species of marine life are found in the area. A number of national parks exist in the area such as Karimunjawa. The Thousand Islands are located north of the national capital Jakarta, and are the city's only regency. The area around the Java Sea is also a popular tourist ...
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 ...
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 ...
Only at the Permian-Triassic boundary ~250 million years ago was the long-term mean sea level lower than today. Long term changes in the mean sea level are the result of changes in the oceanic crust, with a downward trend expected to continue in the very long term. [14] During the glacial-interglacial cycles over the past few million years, the ...
The Eastern limits of the Philippine Sea [P 1] and Japan Sea [P 2] and the Southeastern limit of the Sea of Okhotsk. [P 3] On the North. The Southern limits of the Bering Sea [P 4] and the Gulf of Alaska. [P 5] On the East. The Western limit of Coastal waters of Southeast Alaska and Br. Columbia, [P 6] and the Southern limit of the Gulf of ...
The territorial waters of Indonesia are defined according to the principles set out in Article 46 of the United Nations Convention on the Law of the Sea. Their boundary consists of straight lines ("baselines") linking 195 coordinate points located at the outer edge of the archipelago ("basepoints").
Sea currents in the strait have a very complex configuration, largely dependent on monsoon seasons: during the northwesterly winds, the northern vector predominates, while in the south-east it is the southern one. The maximum speed – up to 13 km / h – flows reach the northern, most narrow part of the strait.