Ambrym volcano

shield volcano 1334 m (4,377 ft)
Vanuatu, -16.25°S / 168.12°E
Current status: normal or dormant (1 out of 5)
Last update: 27 Aug 2020
The crater of Benbow (Ambrym)
The crater of Benbow (Ambrym)

Ambrym is a large basaltic volcano with a 12-km-wide caldera. It is not only one of the most active volcanoes of Vanuatu, but in the world. Its most active craters often contain small lava lakes.

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Typical eruption style: Effusive, formation of lava lakes
Ambrym volcano eruptions: 1774, 1820(?), 1863, 1870(?), 1871, 1883, 1884, 1886, 1888, 1894, 1898, 1908, 1909(?), 1910, 1912, 1913, 1915, 1929, 1935, 1937, 1938, 1942, 1950, 1952, 1953, 1954, 1955, 1957, 1958, 1960, 1961, 1963, 1964, 1967, 1971, 1972, 1973, 1977 (2x), 1979 (2x), 1980, 1981, 1983, 1984, 1986, 1988, 1989, 1990, 1994, 1996, 2006, 2008, 2009 -ongoing

Latest nearby earthquakes

TimeMag. / DepthDistance/Location
Sun, 20 Jun 2021 (GMT) (1 earthquake)
21 Jun 3:46 am (GMT +11) (20 Jun 2021 16:46:57 GMT)
4.3

251 km
48 km (30 mi)
Coral Sea, 21 km southeast of Pentecost Island, Penama Province, Vanuatu

Background

Ambrym is a large basaltic volcano with a 12-km-wide caldera. It is not only one of the most active volcanoes of Vanuatu, but also in the world.
Ambrym's caldera is a wide, impressive moon-like landscape containing an ash plain, cut by innumerable erosion gullies and containing several active craters and recent lava flows.
The caldera is believed to have formed during a major plinian eruption with dacitic pyroclastic flows about 1900 years ago. Activity after the caldera formation was concentrated around two vents that have become large complex craters called Marum and Benbow. Often, both Marum and Benbow (as well as other craters) contain small lava lakes, which occasionally erupt lava flows onto the caldera floor, or even exit the caldera through erosion gaps.
The post-caldera eruptions have also formed a series of scoria cones and maars along a fissure system oriented ENE-WSW. Eruptions have apparently occurred almost yearly during historical time from cones within the caldera or from flank vents. However, from 1850 to 1950, reporting was mostly limited to extra-caldera eruptions that would have affected local populations.
Occasionally, explosive eruptions occur from the craters, mostly because of water-magma interaction. Such eruptions produce tall clouds of ash, and can cause serious health problems in the local population because the ash contaminates ground water.

Ambrym Photos

An usually clear view of the interior of Benbow's crater in the evening. (Photo: Tom Pfeiffer)
An usually clear view of the interior of Benbow's crater in the evening. (Photo: Tom Pfeiffer)
Highly fluid lava bursts from the vent of Benbow, Ambrym volcano, Vanuatu (Photo: Tom Pfeiffer)
Highly fluid lava bursts from the vent of Benbow, Ambrym volcano, Vanuatu (Photo: Tom Pfeiffer)
The south (l) and north (r) pit craters containing little lava lakes. Strong spattering from the south pit. (Photo: Tom Pfeiffer)
The south (l) and north (r) pit craters containing little lava lakes. Strong spattering from the south pit. (Photo: Tom Pfeiffer)
The deep second crater of Benbow (Photo: Yashmin Chebli)
The deep second crater of Benbow (Photo: Yashmin Chebli)
 



Ambrym volcano tours:
The Volcanoes of Ambrym - the Grand Traverse (11-day volcano expedition to Ambrym - individual departures & group tours)
Volcanoes and Cultures - Adventures in the South Sea (15-day volcano and photo expedition to Ambrym and Yasur volcanoes, Vanuatu)

See also: Sentinel hub | Landsat 8
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Map of the Ambrym caldera

map of Ambrym caldera
A sketch map of the vast caldera of Ambrym showing the location of its multiple vents. Taken from Stromboli Online.
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