Coordinates: 19°45′00″S 175°04′30″W / 19.75000°S 175.07500°W / -19.75000; -175.07500
From Wikipedia, the free encyclopedia
Tofua Island (lower left) and neighbouring Kao Island, Tonga, Pacific Ocean
Highest point
Elevation515 m (1,690 ft)
Prominence515 m (1,690 ft)
ListingList of volcanoes in Tonga
Coordinates19°45′00″S 175°04′30″W / 19.75000°S 175.07500°W / -19.75000; -175.07500
Tofua is located in Tonga
Tonga Islands, Tonga
Mountain typeVolcanic caldera
Last eruption2022 (Ongoing)[1]
Tofua caldera

Tofua is a volcanic island in Tonga. Located in the Haʻapai island group, it is a steep-sided composite cone with a summit caldera. It is part of the highly active Kermadec-Tonga subduction zone and its associated volcanic arc, which extends from New Zealand north-northeast to Fiji, and is formed by the subduction of the Pacific Plate under the Indo-Australian Plate.[2] It lies about 100 km (62 mi) above a very active seismic zone.[3] It is connected to the nearby island of Kao by a submarine ridge.[4]

The island is a national park.

Geography and geology[edit]

The island is oval, measuring approximately 80 square kilometers.[4] Its sides rise steeply to the rim of the caldera, which is partially filled by a volcanic crater lake with a depth of 500 m (1,600 ft).[5] The caldera was formed by a major eruption around 1,000 years BP, which left deposits up to 0.5 metres (1 ft 8 in) thick on islands over 40 kilometres (25 mi) away.[6]

Tofua's pre-caldera activity is recorded by a sequence of pyroclastic deposits and lavas constituting the older cone, followed on the northern part of the island by froth lavas or welded and unwelded ignimbrite. Following the caldera collapse, lavas were erupted from the northern part of the island and the caldera-rim fissure zone, scoria and lavas from the caldera-wall fissure zones, pyroclastics and lavas from intracaldera cones, and recent pyroclastic fall deposits on the outer cone. Eruptive products are mainly basaltic andesites and andesites, plus occasional dacite flows within the older cone. A postcaldera cone with fumarolic activity (Lofia) is in the northern part of the caldera[5]

Most historical eruptions have been small explosions from Lofia cone along the northern caldera rim. The eruptions of 1958–59 caused most of the islanders to evacuate for a year or more.


In 1774 Captain Cook sailed between Tofua and Kao, but did not land.[7] He observed smoke rising from the island, and that "[the] brow of the Hill had been consumed by fire".[7]

The Mutiny on the Bounty took place on 28 April 1789, about 30 nautical miles (56 km; 35 mi) from Tofua. After being cast off the ship, Captain William Bligh navigated the overcrowded 23-foot (7.0 m) open launch on an epic 41-day voyage first to Tofua and then to the Dutch East Indies port of Kupang on Timor equipped with a quadrant, a pocket watch, sextant and a compass. The mutineers refused them charts so Bligh had to navigate to Timor from memory.[8] He recorded the distance as 3,618 nautical miles (6,701 km; 4,164 mi). He passed through the difficult Torres Strait along the way and reached Kupang on June 14.[8] The only casualty on this voyage was a crewman named John Norton who was stoned to death by the natives of Tofua, the first island they tried to land on.[9]

At Tofua (Bligh spelled it Tofoa), Bligh and eighteen loyalists sought refuge in a cave to augment their meager provisions. In the March 1968 issue of the National Geographic Magazine, Luis Marden claimed to have found this cave and the grave of John Norton.[10] Both findings were later disproved by Bengt Danielsson (who had been a member of the 1947 Kon-Tiki expedition) in the June 1985 issue of the Pacific Islands Monthly. Danielsson identified Bligh's cave as lying on the sheltered northwest coast, where Bligh identified it; Marden's cave lies on the exposed southeast coast. Additionally, Danielsson thought it highly unlikely that the Tofuans would have allotted any grave site to Norton, or that the grave, if allotted, would have been preserved for two centuries.[11]

In May 1943, a lifeboat containing 23 survivors from the Liberty ship SS Phoebe A. Hearst, which sank after being torpedoed by the Japanese submarine I19 on 30 April 1943, landed. The crew survived on shellfish and coconuts until spotted by a Lockheed Hudson patrol aircraft of the Royal New Zealand Air Force and were picked up the following day by the US Navy YMS-1-class minesweeper YMS-89 and taken to Tongatapu.[12]

In 2008–2009, the Swiss adventurer Xavier Rosset spent 10 months alone on the island. Having a camera, he turned his survivalist endeavor into a documentary called 300 Days Alone.[13][14]

The oral tradition of Kao and Tofua[edit]

E. W. Gifford, recording Tongan myths and tales in the 1920s, documented this explanation for Tofua's caldera and the creation of Kao Island to the north:

Three deities from Samoa, Tuvuvata, Sisi, and Faingaa, conspired to steal Tofua. So they came and tore up the high mountain by its very roots and its place was taken by a large lake. This enraged the Tongan gods very much and one of them, Tafakula, essayed to stop the thieves. He stood on the island of Luahako and bent over so as to show his anus. It shone so brilliantly that the Samoan deities were struck with fear, thinking that the sun was rising and that their dastardly works was about to be revealed. Hence, they dropped the mountain and fled to Samoa. The mountain became the island of Kao.[15]


The island is the largest area of undisturbed Tongan tropical moist forests in Tonga, and was designated a national park in 2001.[16] It has been designated an Important Bird Area by BirdLife International.[17] Birds include the Many-colored fruit dove, Crimson-crowned fruit dove, Blue-crowned lorikeet, Polynesian wattled honeyeater, Polynesian triller, Fiji shrikebill, and Polynesian starling.[18]

See also[edit]


  1. ^ "Tofua: Eruptive History". Global Volcanism Program. Smithsonian Institution. Retrieved 21 February 2022.
  2. ^ Caulfield, J. T.; Turner, S. P.; Smith, I. E. M.; Cooper, L. B.; Jenner, G. A. (2012). "Magma Evolution in the Primitive, Intra-oceanic Tonga Arc: Petrogenesis of Basaltic Andesites at Tofua Volcano". Journal of Petrology. 53 (6): 1197–1230. doi:10.1093/petrology/egs013. Retrieved 22 January 2022.
  3. ^ Ewart, A.; Bryan, W.B.; and Gill, J.B. "Mineralogy and Geochemistry of the Younger Volcanic Islands of Tonga, S.W. Pacific." Journal of Petrology. 14:3 (1973). doi:10.1093/petrology/14.3.429
  4. ^ a b Bauer, Glenn R. (1970). "The Geology of Tofua Island, Tonga" (PDF). Pacific Science. 24 (3): 333–350. Archived from the original (PDF) on 22 January 2022. Retrieved 22 January 2022.
  5. ^ a b "Tofua". Global Volcanism Program. Smithsonian Institution.
  6. ^ Caulfield, J. T.; Cronin, S. J.; Turner, S. P.; Cooper, L. B. (2011). "Mafic Plinian volcanism and ignimbrite emplacement at Tofua volcano, Tonga". Bulletin of Volcanology. 73 (9): 1259–1277. Bibcode:2011BVol...73.1259C. doi:10.1007/s00445-011-0477-9. S2CID 140540145.
  7. ^ a b "The Friendly Isles". Captain Cook Society. Retrieved 22 January 2022.
  8. ^ a b "A Voyage to the South Sea". Retrieved 2020-05-07.
  9. ^ "Pitcairn Islands Study Center". Retrieved 2020-05-07.
  10. ^ danielramirez (2016-05-30). National Geographic 1968.
  11. ^ "Vol. 56, No. 6 (Jun. 1, 1985)". Retrieved 2020-05-07.
  12. ^ Cressman, Robert J. (2016). The Official Chronology of the U.S. Navy in World War II. Annapolis: Naval Institute Press. ISBN 978-1-68247-154-8. OCLC 1030816142.
  13. ^ "Xavier Rosset: 300 days alone on an island". TEDxGeneva (in French). Retrieved 2020-05-07.
  14. ^ "Swiss alone on remote Tongan island attracting a lot of interest". RNZ. 10 November 2008. Retrieved 22 January 2022.
  15. ^ Edward Winslow Gifford (1924), Tongan myths and tales, Honolulu: Bernice P. Bishop Museum Bulletin, No. 8
  16. ^ "Tofua Island". Digital Observatory for Protected Areas (DOPA) Explorer. Retrieved 22 January 2022.
  17. ^ "Tofua and Kao". BirdLife International. Retrieved 22 January 2022.
  18. ^ "Tofua and Kao: Details". BirdLife International. Retrieved 22 January 2022.

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