Mota Lava
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Mota Lava or Motalava is an island of the Banks group, in the north of
Vanuatu Vanuatu ( or ; ), officially the Republic of Vanuatu (; ), is an island country in Melanesia located in the South Pacific Ocean. The archipelago, which is of volcanic origin, is east of northern Australia, northeast of New Caledonia, east o ...
. It forms a single coral system with the small island of Ra. The 2009 census figures give a population of 1,640 inhabitants (Mota Lava + Ra), which amounts to a population density of 67 people per km2.


Geography


Geography and geology

With an area of 24 km2 (9.3 sq mi), Mota Lava is the fourth largest island in the Banks Islands, after Gaua, Vanua Lava and Ureparapara. It is the highest () of the eastern chain of islands, as well as the largest. Ra, a small island of , is located off the southern coast of Mota Lava. It is attached to it by high corals that one can wade through at low tide. The climate on Mota Lava is humid tropical. The average annual rainfall exceeds 4000 mm. The island is subject to frequent earthquakes and cyclones. The island is served by Mota Lava Airport.


Geology

Mota Lava is composed of at least five
basalt Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial ...
ic
stratovolcano A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with ...
es. Two of the cones, Vetman and Tuntog, are well-preserved. Vetman is a pyroclastic cone in the centre of the island with a breached summit crater. At the southwest end of the island, Tuntog is a composite cone with a wide crater.
Geochemical Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the ...
analysis shows that the island's lava has a similar composition to that from nearby Mota and Ureparapara, as well as lava from the south of the country, but differs from material erupted in central Vanuatu. The latter region has been affected by the subduction of a submerged, extinct island arc complex called the D'Entrecasteaux Zone.


Name and language

In early 19th-century texts and maps, Mota Lava was called ''Saddle Island'', after the distinctive saddle-shaped profile it presents when seen from a boat offshore. The inhabitants of Mota Lava call the island Mwotlap, locally spelled ''M̄otlap'' (). The language spoken by the inhabitants of Motalava is also called Mwotlap. It is the most widely spoken language in the Banks Islands, with about 2,100 speakers. The recently extinct Volow language also used to be spoken on Mota Lava. An early attempt to transcribe the native name, both for the island and the language, yielded a form ''Motlav''. The name ''M̄ota Lava'' (or in simple spelling, ''Motalava'') caught on after it started being used by 19th-century missionaries to the island. They borrowed that name from the language spoken on neighbouring Mota. Both the Mota and Mwotlap names of the island descend from a protoform *''mʷota laβa'' in Proto-Torres-Banks, literally "large Mota". A process of vowel deletion, regular in Mwotlap, explains how * was shortened to .


History

Like the rest of Vanuatu, Motalava was first settled around the by Austronesian navigators belonging to the
Lapita culture The Lapita culture is the name given to a Neolithic Austronesian peoples, Austronesian people and their distinct material culture, who settled Island Melanesia via a seaborne migration at around 1600 to 500 BCE. The Lapita people are believed t ...
. Archaeologists have found ancient
obsidian Obsidian ( ) is a naturally occurring volcanic glass formed when lava extrusive rock, extruded from a volcano cools rapidly with minimal crystal growth. It is an igneous rock. Produced from felsic lava, obsidian is rich in the lighter element ...
in Mota Lava, Vanua Lava and Gaua, and Lapita pottery have been found in the island. The island was first sighted by Europeans during the Spanish expedition of
Pedro Fernández de Quirós Pedro is a masculine given name. Pedro is the Spanish, Portuguese, and Galician name for '' Peter''. Its French equivalent is Pierre while its English and Germanic form is Peter. The counterpart patronymic surname of the name Pedro, meani ...
, from 25 to 29 April 1606. The island’s name was then charted as ''Lágrimas de San Pedro'' (“St. Peter's Tears”, in Spanish).Kelly, Celsus, O.F.M. ''La Austrialia del Espíritu Santo. The Journal of Fray Martín de Munilla O.F.M. and other documents relating to the Voyage of Pedro Fernández de Quirós to the South Sea (1605-1606) and the Franciscan Missionary Plan (1617-1627)'' Cambridge, 1966, p.39, 62.


Notes and references


Notes


References

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External links


An introduction to the culture of Mota Lava and its surroundings
– featuring photos, maps, access to linguistic documents and traditional stories (site of the linguist Alexandre François) **
A Journey to Motalava
(''Promenade ethnolinguistique à Motalava'') {{Authority control Islands of Vanuatu Volcanoes of Vanuatu Torba Province Banks Islands