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The Banda Sea in the south of the Molucca archipelago includes a small group of islands. Three major tectonic plates beneath the sea, Eurasian, Pacific and Indo-Australian plates, have been converging since the Mesozoic epoch.[21] Volcanoes in the Banda Sea are mainly islands, but some are submarine volcanoes. | Name | Shape | Elevation | Last eruption (VEI) | Geolocation | | (m) | (ft) | | Emperor of China | submarine | -2,850 | -9,350 | unknown | 6.62° S 124.22° E | | Nieuwerkerk | submarine | -2,285 | -7,500 | unknown | 6.60° S 124.675° E | | Gunungapi Wetar | stratovolcano | 282 | 925 | 1699 (3) | 6.642° S 126.65° E | | Wurlali | stratovolcano | 868 | 2,850 | 3 June 1892 (2) | 7.125° S 128.675° E | | Teon | stratovolcano | 655 | 2,150 | 3 June 1904 (2) | 6.92° S 129.125° E | | Nila | stratovolcano | 781 | 2,500 | 7 May 1968 (1) | 6.73° S 129.50° E | | Serua | stratovolcano | 641 | 2,100 | 18 September 1921 (2) | 6.30° S 130.00° E | | Manuk | stratovolcano | 282 | 925 | unknown | 5.53° S 130.292° E | | Banda Api | caldera | 640 | 2,100 | 9 May 1988 (3) | 4.525° S 129.871° E |
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