Ambrym

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Ambrym
Ambrym volcano.jpg
Ash plume from Ambrym Volcano, October 4, 2004
Elevation 1,334 m (4,377 ft)[1]
Location
Location Vanuatu
Coordinates 16°15′S 168°7′E / 16.25°S 168.117°E / -16.25; 168.117Coordinates: 16°15′S 168°7′E / 16.25°S 168.117°E / -16.25; 168.117[1]
Geology
Type Pyroclastic shield[1]
Volcanic arc New Hebrides arc[1]
Last eruption 2011 (ongoing)[1]

Ambrym is a volcanic island in the archipelago of Vanuatu (formerly known as the New Hebrides). It is well known for its highly active volcanic activity that includes lava lake formation.

Contents

Etymology

Ambrym (aka Ambrin[2]) was so named by Captain Cook, who anchored off there in 1774. It means "here are yams" ("ham rim" in the Ranon language).[3]

Geography

Located near the center of the long Vanuatuan archipelago, Ambryn is roughly triangular in shape, about 50 km (31 mi) wide.[4] With 677.7 square kilometres (261.7 sq mi) of surface area, it is the fifth largest island in the country.

The summit at the center of the island is dominated by a desert-like caldera, which covers an area of 100 square kilometres (39 sq mi).[1]

With the exception of human settlements, the rest of the island is covered by thick jungle.[4]

Volcanology

Boiling lava in Marum crater, Ambrym, in a photo taken 24 September 2009.

Ambrym is a large basaltic volcano with a 12-km-wide caldera, and one of the most active volcanoes of the New Hebrides volcanic arc.

The caldera is the result of a huge plinian explosion, which took place around 50 AD. Its explosive force is rated 6, the second highest in the Smithsonian Institution's Volcanic Explosivity Index ranks of the largest volcanic explosions in recent geological history.[5]

The massive, 1900-year-old, 12 kilometres (7.5 mi) × 8 kilometres (5.0 mi) caldera is the site of two active volcanic cones, Benbow and Marum (also spelled Maroum).[1]

While at higher elevations cinder cones predominate, the western tip of the island is characterized by a series of basaltic tuff rings, of which the largest is about 1 kilometre (0.62 mi) in diameter. These were produced by phreatic eruptions when magma contacted the water table and water-saturated sediments along the coast.[6]

Several times per century, Ambrym volcano had destructive eruptions.

Mt Benbow last erupted in 1913, causing the evacuation of the population to Mele, near Port Vila on Efate.

Demographics

With the neighbour island of Malakula and a few smaller islands, Ambrym forms Malampa Province. Its largest settlement is the village of Eas. The population of 8,000 inhabitants [7] lives mainly off coconut plantations.

Languages

An Ambrym woodcarver, circa 1925

Like many islands in Vanuatu, Ambrym has its own Austronesian languages. In the north is the North Ambrym language, in the southeast is the Southeast Ambrym language, in the south Dakaka language, in the west Lonwolwol language, and in the southwest Port-Vato language. These are all spoken by a few hundred to a few thousand speakers each.

The kinship system used by natives of Ambrym can be modeled by a non-commutative group.[8]

Nearby small islands to the south

  • Paama with villages of Liro and Loulep
  • Lopevi with villages of Holen and Halos (now abandoned)

Towns and villages

  • Fali - Craig Cove - Baiap - Sesivi - Emiotungan - Polibetakever - Lolibulo - Linboul - Liro - Loulep - Olal - Ranuetlam - Ranon - Port Vato - Lalinda - Toak - Fanla

Tourism

Tourists are attracted by Ambrym's unique features: the active volcanoes, the tropical vegetation, and the customs of the local villagers. They stay in traditional style bungalows, as there are no hotels on the island.[3]

References

External links



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