 | |
| Geography | |
|---|---|
| Location | Indonesia |
| Coordinates | 7°09′04″S 110°08′25″E / 7.1510°S 110.1403°E |
| Major islands | Sumatra, Java, Nusa Tenggara |
| Additional information | |
| Tectonic - Indo-Australian Plate and Eurasia Plate
Major Volcanoes - Merapi, Krakatoa, Mount Sinabung, Semeru | |
The Sunda Arc is a volcanic arc that produced the volcanoes that form the topographic spine of the islands of Sumatra, Nusa Tenggara, Java, the Sunda Strait, and the Lesser Sunda Islands. The Sunda Arc begins at Sumatra and ends at Flores, and is adjacent to the Banda Arc.[1] The Sunda Arc is formed via the subduction of the Indo-Australian Plate beneath the Sunda and Burma plates at a velocity of 63–70 mm/year.[2]
- ^ Pacey, Adam; Macpherson, Colin G.; McCaffrey, Ken J. W. (2013-05-01). "Linear volcanic segments in the central Sunda Arc, Indonesia, identified using Hough Transform analysis: Implications for arc lithosphere control upon volcano distribution". Earth and Planetary Science Letters. 369–370: 24–33. Bibcode:2013E&PSL.369...24P. doi:10.1016/j.epsl.2013.02.040. ISSN 0012-821X.
- ^ Simons, W. J. F.; Socquet, A.; Vigny, C.; Ambrosius, B. a. C.; Abu, S. Haji; Promthong, Chaiwat; Subarya, C.; Sarsito, D. A.; Matheussen, S.; Morgan, P.; Spakman, W. (2007). "A decade of GPS in Southeast Asia: Resolving Sundaland motion and boundaries". Journal of Geophysical Research: Solid Earth. 112 (B6): B06420. Bibcode:2007JGRB..112.6420S. doi:10.1029/2005JB003868. ISSN 2156-2202.