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  1. en.wikipedia.org › wiki › Sunda_PlateSunda plate - Wikipedia

    The Sunda plate includes the South China Sea, the Andaman Sea, southern parts of Vietnam, Myanmar, Laos and Thailand along with Malaysia, Singapore, Cambodia, southern Philippines, and the islands of Bali, Lombok, West Nusa Tenggara, Borneo, Sumatra, Java, and part of Sulawesi in Indonesia.

  2. en.wikipedia.org › wiki › Sunda_TrenchSunda Trench - Wikipedia

    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 Eurasian Plate (more specifically, Sunda Plate).

  3. 1 paź 2019 · The Java Trench, also known as the Sunda Trench, is located south and west of the islands of Java and Sumatra in the eastern Indian Ocean, and is in excess of 3200 km in length. The trench is formed as the Indo-Australian Plate subducts beneath the Eurasian Plate, at a rate of between 60 and 73 mm per year ( De Mets et al., 2010 ).

  4. en.wikipedia.org › wiki › Sunda_ShelfSunda Shelf - Wikipedia

    Sunda Shelf. Map of Sahul and Sunda. Geologically, the Sunda Shelf (/ ˈsʌndə / [1]) is a south-eastern extension of the continental shelf of Mainland Southeast Asia. Major landmasses on the shelf include Bali, Borneo, Java, Madura, and Sumatra, as well as their surrounding smaller islands. [2]

  5. 1 gru 2014 · Structural map of the major ridges and basins of South Sundaland from SE Borneo to Eastern Java and Flores basins. The region of East Java–Madura–Kanggean south of the Meratus Mountains and Bawean Arch (Figure 5, Figure 6), includes the Java basins and continental ridges (Ketapang High/North Madura ridge).

  6. 20 lut 2023 · Active subduction at the Sunda trench is the principal driver of ongoing India-Asia convergence and Indian indentation. Our models predict that lateral subduction zones lead to mountain growth like the Himalaya over tens of millions of years.

  7. 30 cze 2016 · Sundaland is a biogeographical region of Southeastern Asia that encompasses the Sunda shelf, the part of the Asian continental shelf that was exposed during the last glacial period of the Pleistocene, from approximately 110,000 to 12,000 years ago.

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