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Random pictures
The crater of Benbow in the Ambrym caldera
The crater of Benbow in the Ambrym caldera

Latest news from Ambrym:

Lava fountain from Benbow's lava lake (image: Yashmin Chebli / VolcanoDiscovery)
Tuesday, Oct 23, 2018
A small group on our latest Vanuatu Volcano Expedition observed 3 active lava lakes in Ambrym volcano. Expedition leader volcanologist Yashmin Chebli reported from their visit during the first week of Oct 2018 (link to pictures): ... [more]
The active lava lake in Benbow's crater on Ambrym volcano in July 2018 (image: Yashmin Chebli / VolcanoDiscovery)
Monday, Aug 06, 2018
The activity of Ambrym volcano remains intense with three active lava lakes in Benbow, Marum and Niri Membelsu craters. Our expedition leader Yashmin Chebli was on the volcano last week and reports: ... [more]
 

Ambrym volcano

shield volcano 1334 m (4,377 ft)
Vanuatu, -16.25°S / 168.12°E
Current status: erupting (4 out of 5)
Ambrym webcams / live data | Reports
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Last update: 23 Oct 2018 (active lava lakes in Benbow, Marum and Niri Membelsu craters)
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 -ongoingThe crater of Benbow (Ambrym)
TimeMag. / DepthDistanceLocation
Mon, 29 Oct
Mon, 29 Oct 07:41 UTCM 5.0 / 183 km19 km VANUATU
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.

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:




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

Latest satellite images

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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