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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).
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).
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]
The western and southern borders of Sundaland are clearly marked by the deeper waters of the Sunda Trench – some of the deepest in the world – and the Indian Ocean. [4]
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).
Download scientific diagram | A regional map showing the Sunda trench, the Sumatran Fault System (SFS) and the Sagaing fault, which between them absorb the convergence of the India-Australia...
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.
