The Sunda Trench, earlier known as, and sometimes still indicated as the Java Trench, is located in the northeastern Indian Ocean, with a length of 2,600 kilometres (8,500,000 ft). The maximum depth of 7,725 metres (25,344 ft) (at 10°19'S, 109°58'E, about 320 km south of Yogyakarta), is the deepest point in the Indian Ocean. The trench stretches from the Lesser Sunda Islands past Java, around the southern coast of Sumatra on to the Andaman islands, and forms the boundary between Indo-Australian Plate and Eurasian plate (more specificly, Sunda Plate). The trench is considered to be part of the Pacific Ring of Fire as well as one of a ring of oceanic trenches around the northern edges of the Australian Plate.
There is scientific evidence that the recent earthquake activity in the area of the Java Trench could lead to further catastrophic shifting within a relatively short period of time, perhaps less than a decade. This threat has resulted in international agreements to establish a tsunami warning system in place along the Indian Ocean coast.
For about half its length, off of Sumatra, it is divided into two parallel troughs by an underwater ridge, and much of the trench is at least partially filled with sediments. Mappings after the 2004 Indian Ocean earthquake of the plate boundary showed resemblance to suspension bridge cables, with peaks and sags, indicative of asperity and locked faults, instead of the traditional wedge shape expected.
Some of the earliest exploration of the Trench occurred in the late 1950s when Robert Fisher, Research Geologist at the Scripps Institution of Oceanography, investigated the trench as part of a world wide scientific field exploration of the world's ocean floor and sub-oceanic crustal-structure. Bomb-sounding, echo-train analysis and manometer were some of the techniques used to determine the depth of the trench. The research contributed to an understanding of the subduction characteristic of the Pacific margins.
Various agencies have explored the trench in the aftermath of the 2004 earthquake, and these explorations have revealed extensive changes in the ocean floor.
The subduction of the Indo-Australian Plate beneath a bloc of the Eurasian Plate is associated with numerous earthquakes. Several of these earthquakes are notable for their size, associated tsunamis, and/or the number of fatalities they caused.
- 1797 Sumatra earthquake: Magnitude ~8.4
- 1833 Sumatra earthquake
- 1861 Sumatra earthquake: Magnitude ~8.5
- 1935 Sumatra earthquake: Magnitude 7.7
- 2000 Sumatra earthquake: Magnitude 7.9
- 2002 Sumatra earthquake: A Magnitude 7.3 earthquake that occurred at the boundary between the rupture areas of the 2004 and 2005 earthquakes listed below.
- 2004 Indian Ocean earthquake and tsunami
- 2005 Sumatra earthquake: Magnitude 8.6
- September 2007 Sumatra earthquakes
- 2009 Sumatra earthquakes: Magnitude 7.9
- October 2010 Sumatra earthquake and tsunami
- 1917 Bali earthquake: Magnitude 8.6
- 1994 Java earthquake: Magnitude 7.8
- May 2006 Java earthquake: Despite a Magnitude of only 6.3, this earthquake caused 5,782 deaths.
- July 2006 Java earthquake: Magnitude 7.7
- 2009 West Java earthquake: Magnitude 7.0
- Banda Arc
- Islands of Indonesia
- Plate tectonic
- Sunda Arc
- Sunda Islands
- Oceanic trench
- Sunda Trench (4°30' S 11°10' S 100°00' E 119°00' Accredited by: SCGN (Apr. 1987) The trench was studied in some detail in 1920's-1930's by Dutch geodesist F.A. Vening Meinesz, who made classic pendulum gravity measurements in a Dutch submarine. Shown as Java Trench in ACUF (Advisory Committee on Undersea Features Gazetteer). see also: http://www.gebco.net/
- Asia primed for next big quake - earth - 19 March 2005 - New Scientist Environment
- IOC: Towards a Tsunami Warning System in the Indian Ocean
- Physorg:Folded sediment unusual in Sumatran Tsunami area
- "The underwater survey of the SUMATRA earthquake source area"
- Špičák, A., V. Hanuš, and J. Vaněk (2007), Earthquake occurrence along the Java trench in front of the onset of the Wadati-Benioff zone: Beginning of a new subduction cycle?, Tectonics, 26, TC1005