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Banda Sea

Coordinates:6°S127°E / 6°S 127°E /-6; 127
From Wikipedia, the free encyclopedia
Sea between Sulawesi and Maluku

Banda Sea
Run (left) and Nailaka (right), islands in the Banda Sea
Run (left) and Nailaka (right), islands in the Banda Sea
Location of the Banda Sea in Southeast Asia
Location of the Banda Sea in Southeast Asia
LocationSoutheast Asia
Coordinates6°S127°E / 6°S 127°E /-6; 127
TypeSea
Primary outflowsPacific Ocean,Timor Sea,Molucca Sea,Ceram Sea,Banda Arch
Basin countries
Max. length1,000 km (620 mi)
Max. width500 km (310 mi)
Surface area470,000 km2 (180,000 sq mi)[1]
Max. depth7,351 m (24,117 ft)
Location
Map
Interactive map of Banda Sea

TheBanda Sea (Indonesian:Laut Banda,Indonesian pronunciation:[ˌlaʊt̪̚ˈbanda];Portuguese:Mar de Banda;Tetum:Tasi Banda) is one of fourseas that surround theMaluku Islands ofIndonesia, connected to thePacific Ocean, but surrounded by hundreds of islands, includingTimor, as well as theHalmahera andCeram Seas. It is about 1,000 km (620 mi) east to west, and about 500 km (310 mi) north to south.[1]

Extent

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TheInternational Hydrographic Organization (IHO) defines the Banda Sea as being one of the waters of theEast Indian Archipelago. The IHO defines its limits as follows:[2]

On the North The Southern limits of theMolukka Sea [sic] and the Western and Southern limits of theCeram Sea.

On the East. From Tg Borang, the Northern point of Noehoe Tjoet [Kai Besar], through this island to its Southern point, thence a line to the Northeast point of Fordata, through this island and across to the Northeast point of Larat,Tanimbar Islands (7°06′S131°55′E / 7.100°S 131.917°E /-7.100; 131.917), down the East coast of Jamdena [Yamdena] Island to its Southern point, thence through Anggarmasa to the North point of Selaroe and through this island to Tg Aro Oesoe its Southern point (8°21′S130°45′E / 8.350°S 130.750°E /-8.350; 130.750).

On the South. A line from Tanjong Aro Oesoe, through Sermata to Tanjong Njadora the Southeast point of Lakov [Lakor,sic] (8°16′S128°14′E / 8.267°S 128.233°E /-8.267; 128.233) along the South coasts ofLakov [Lakor], Moa and Leti Islands to Tanjong Toet Pateh, the West point of Leti, thence a line to Tanjong Sewirawa the Eastern extremity ofTimor and along the North coast as far aslongitude 125° East.

On the West. From a point on the North coast of Timor in 125° East up this meridian toAlor Island, thence round the East point and along the North coasts of the Alor,Pantar,Lomblen andAdoenara Islands and thence across the Northern end of Flores Strait to Tanjong Serbete the Eastern extreme ofFlores, thence a line from its Northern point (8°04′S122°52′E / 8.067°S 122.867°E /-8.067; 122.867) to Kalaotoa Island (7°24′S121°52′E / 7.400°S 121.867°E /-7.400; 121.867) and through the chain of islands lying between it and the South point ofPulo Salayar, through this island and across the Strait to Tanjong Lassa,Celebes (5°37′S120°28′E / 5.617°S 120.467°E /-5.617; 120.467), thence along the Southern limit of theGulf of Boni and up the East coast of Celebes to Tanjong Botok (1°04′S123°19′E / 1.067°S 123.317°E /-1.067; 123.317).

Banda Sea in the center ofMaluku Islands

Geography

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Islands bordering the Banda Sea includeSulawesi to the west,Buru,Ambon,Seram to the north, theAru Islands,Tanimbar Islands, andKai Islands to the east, and theBarat Daya Islands andTimor to the south. Although the borders of the sea are hazardous tonavigation, with many small rocky islands, the middle of the sea is relatively open. Island groups within the sea include theBanda Islands. Some islands in the Banda Sea are active volcanoes including Gunung Api and Manuk in the Banda Islands.

Geology

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Plate tectonic activities in Banda Sea

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Map of theBanda Sea plate

The Banda arc is famous for its 180° curvature and is, in Timor, generally agreed to be the product of a collision between a volcanic arc and the Australian continental margin.[3][4] The Banda Sea occupies the main portion of theBanda Sea plate. The southern margin of the sea consists ofisland arcs abovesubduction zones. To the east of theSunda Trench is theTimor Trough which lies south ofTimor, the Tanimbar Trough south of theTanimbar Islands and theAru Trough east of theAru Islands. These trenches are the subduction zone of theIndo-Australian plate beneath the Banda Sea plate, where the Indo-Australian plate moves northwards. Fore-arc sediments progressively carried northwards by the Indo-Australian plate have been folded and faulted forming Timor Island. To the northeast liesSeram Island which overlies the subduction of theBird's Head plate ofWest Papua.[5] The deepest point of the sea,Weber Deep, is an exposed oceanic fault and the world's deepestforearc basin, with depth more than 7.2 kilometres (4.5 miles).[6][7]

Earthquakes

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TheUSSGeorge Washington crossing the Banda Sea

Earthquakes are very frequent in the area, due to the confluence of three tectonic plates – Eurasian, Pacific and Indo-Australian plates.

Ecology

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The Banda Sea is amarine ecoregion, as defined by theWorld Wildlife Fund. It is part of theCoral Triangle region, which has the greatest diversity of coral reef species in the broaderIndo-Pacific.[8]

The Banda Sea, together with the adjacentFlores Sea, forms theBanda-Flores Sea marine ecoregion, included in the Global 200 list of ecoregions identified by the WWF as priorities for conservation.[9]

The islands surrounding the Banda Sea are part ofWallacea, a biogeographical region that contains the islands lying between Asia and Australia which haven't been joined to either continent. The islands of Wallacea are home to a mix of plant and animal species from both tropicalAsia (theIndomalayan realm) and theAustralasian realm which includes Australia and New Guinea.

The islands are divided among severalterrestrial ecoregions. The northern islands ofSulawesi,Buru, andSeram constitute separatetropical moist forest ecoregions. The islands south of the Banda Sea are among the driest in Indonesia, and are home totropical dry forests. TheTimor and Wetar deciduous forests ecoregion includes Timor and Wetar. The Lesser Sunda Islands fromAlor throughFlores andSumbawa toLombok constitute theLesser Sundas deciduous forests ecoregion.[10]

The Tanimbar Islands, Kai Islands, and Barat Daya Islands (except for Wetar) in the southeastern Banda Sea form theBanda Sea Islands moist deciduous forestsecoregion. These islands are covered in mostly-intact rain forest, and home to a number ofendemic plants and animals including twenty-one bird species, a very high number for this small ecoregion. There are only twenty-two native mammals on these islands, including the raredusky pademelon(Thylogale brunii) andIndonesian tomb bat (Taphozous achates), and the endangeredendemicKei myotis bat(Myotis stalkeri). The birdlife is threatened by egg collectors and even more by cats and rodents that have been introduced to the islands.Yamdena in the Tanimbar Islands is an example of a large and fairly unspoilt habitat and is a protected area.[11] The base for visiting these islands is by plane or ship fromAmbon Island to the north. The Banda and Kai Islands, although remote, are visited by tourists for snorkelling and for their unspoilt beaches. Various cetacean species have been recorded including either or bothblue andpygmy blue whales[12][13][14] andOmura's whales.[15]

References

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  1. ^ab"Banda Sea".World Atlas. Retrieved18 November 2025.
  2. ^"Limits of Oceans and Seas, 3rd edition"(PDF). International Hydrographic Organization. 1953. Archived fromthe original(PDF) on 8 October 2011. Retrieved28 December 2020.
  3. ^Carter, D. J.; Audley-Charles, M. G.; Barber, A. J. (1976)."Stratigraphical analysis of island arc—continental margin collision in eastern Indonesia".Journal of the Geological Society.132 (2):179–198.doi:10.1144/gsjgs.132.2.0179.
  4. ^Hamilton, W. (1979). Tectonics of the Indonesian Region (Report). United States Geological Survey Professional Papers. Vol. 1078. United States Government Printing Office.doi:10.3133/pp1078.
  5. ^"Chapter II (Geology of Timor-Leste)".Atlas of mineral resources of the ESCAP region Volume 17 Geology and Mineral Resources of Timor-Leste(PDF). United Nations Economic and Social Commission for Asia and the Pacific. 24 December 2003. Archived fromthe original(PDF) on 20 May 2005.
  6. ^"Discovery of biggest exposed fault on Earth solves mystery of how abyss formed".New Atlas. 29 November 2016. Retrieved25 August 2019.
  7. ^"World's Largest Exposed Fault Covers Area Twice The Size of Belgium".IFLScience. 30 November 2016. Retrieved25 August 2019.
  8. ^Spalding, Mark D.; Fox, Helen E.; Allen, Gerald R.; et al. (2007)."Marine Ecoregions of the World: A Bioregionalization of Coastal and Shelf Areas".BioScience.57 (7):573–583.doi:10.1641/B570707.
  9. ^Olson, D. M., Dinerstein, E. 2002. The Global 200: Priority ecoregions for global conservation.Annals of the Missouri Botanical Garden 89(2):199-224,[1]Archived 2016-05-13 at theWayback Machine.
  10. ^Wikramanayake, Eric; Dinerstein, Eric; Loucks, Colby J.; et al. (1 December 2001),Terrestrial Ecoregions of the Indo-Pacific: a Conservation Assessment, Washington, DC: Island Press,ISBN 978-1559639231
  11. ^"Banda Sea Islands moist deciduous forests".Terrestrial Ecoregions. World Wildlife Fund.
  12. ^Wildiaries.BLUE WHALES OF THE BANDA SEA & FORGOTTEN ISLANDSArchived 24 September 2017 at theWayback Machine. Retrieved on 24 September 2017
  13. ^Edwards J..An Indo-Pacific Bottlenose Dolphin bow riding on the wake of a gigantic Blue Whale.Archived 24 September 2017 at theWayback Machine.Getty Images. Retrieved on 24 September 2017
  14. ^Sarah. 2015.Sailing Through the Banda Sea. Small Girl Big Travels: Field Notes. Retrieved on 24 September 2017
  15. ^Ogata J. M.. 2017.Ambon – Banda Islands – Raja AmpatArchived 2 April 2019 at theWayback Machine. Mermaid Liveaboards. Retrieved on 24 September 2017

Further reading

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  • Ponder, H. W. (1944)In Javanese waters; some sidelights on a few of the countless lovely, little known islands scattered over the Banda sea & some glimpses of their strange & stormy history London, Seeley, Service & Co. ltd.
  • Patrick D. Nunn (1994)Oceanic Islands Oxford, Great Britain, Blackwell
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