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  2. Java Sea - Wikipedia

    en.wikipedia.org/wiki/Java_Sea

    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).

  3. Sunda Strait - Wikipedia

    en.wikipedia.org/wiki/Sunda_Strait

    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 ...

  4. Sunda Shelf - Wikipedia

    en.wikipedia.org/wiki/Sunda_Shelf

    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.

  5. Sunda Trench - Wikipedia

    en.wikipedia.org/wiki/Sunda_Trench

    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 ...

  6. Under keel clearance - Wikipedia

    en.wikipedia.org/wiki/Under_keel_clearance

    In seafaring, under keel clearance (UKC) is the vertical distance between seabed and the keel or hull of a ship. [1] [2] [3] It is used to ensure sufficient navigable water is available for ships at sea.

  7. Bathymetry - Wikipedia

    en.wikipedia.org/wiki/Bathymetry

    Bathymetric charts showcase depth using a series of lines and points at equal intervals, called depth contours or isobaths (a type of contour line). A closed shape with increasingly smaller shapes inside of it can indicate an ocean trench or a seamount, or underwater mountain, depending on whether the depths increase or decrease going inward.

  8. AOL Mail

    mail.aol.com/d?reason=invalid_cred

    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

  9. Borders of the oceans - Wikipedia

    en.wikipedia.org/wiki/Borders_of_the_oceans

    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 ...