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- Q900734 subject Q6274804.
- Q900734 subject Q8639116.
- Q900734 abstract "A monogenetic volcanic field is a group of small monogenetic volcanoes, each of which erupts only once, as opposed to polygenetic volcanoes, which erupt repeatedly over a period of time. Many monogenetic volcanoes are cinder cones, often with lava flows, such as Parícutin in the Michoacán-Guanajuato volcanic field, which erupted from 1943 to 1952. Some monogenetic volcanoes are small lava shields, such as Rangitoto Island in the Auckland volcanic field. Other monogenetic volcanoes are tuff rings or maars. A monogenetic field typically contains between ten and a hundred volcanoes. The Michoacán-Guanajuato field in Mexico contains more than a thousand volcanoes and is much larger than usual.Monogenetic fields occur only where the magma supply to the volcano is low or where vents are not close enough or large enough to develop plumbing systems for continuous feeding of magma. Monogenetic volcanic fields can provide snapshots of the underlying region beneath the surface, and may be useful in studying the generation of magma and the composition of the mantle since the single eruption produced would match that of the chamber from which it erupted.Examples of monogenetic volcanic fields:Auckland volcanic field, underlying much of the city of Auckland, New ZealandWells Gray-Clearwater volcanic field, east-central British Columbia, CanadaHonolulu Volcanic Series, Hawaii, United StatesBoring Lava Field, in and near Portland, Oregon, United StatesMichoacán-Guanajuato volcanic field (includes El Jorullo and Parícutin), Michoacán, MexicoVulkan Eifel, GermanyChaîne des Puys, FranceCarrán-Los Venados, ChileNorth and north-eastern area of Gran Canaria, Canary Islands, SpainSouthern Volcanic Zone of Tenerife, Canary Islands, Spain↑".
- Q900734 wikiPageWikiLink Q1068630.
- Q900734 wikiPageWikiLink Q142.
- Q900734 wikiPageWikiLink Q1422715.
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- Q900734 wikiPageWikiLink Q183.
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- Q900734 wikiPageWikiLink Q231620.
- Q900734 wikiPageWikiLink Q29.
- Q900734 wikiPageWikiLink Q2940365.
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- Q900734 wikiPageWikiLink Q298.
- Q900734 wikiPageWikiLink Q30.
- Q900734 wikiPageWikiLink Q3242376.
- Q900734 wikiPageWikiLink Q37100.
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- Q900734 wikiPageWikiLink Q5813.
- Q900734 wikiPageWikiLink Q5896719.
- Q900734 wikiPageWikiLink Q6106.
- Q900734 wikiPageWikiLink Q6274804.
- Q900734 wikiPageWikiLink Q664.
- Q900734 wikiPageWikiLink Q666046.
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- Q900734 wikiPageWikiLink Q782.
- Q900734 wikiPageWikiLink Q79861.
- Q900734 wikiPageWikiLink Q8072.
- Q900734 wikiPageWikiLink Q8639116.
- Q900734 wikiPageWikiLink Q96.
- Q900734 comment "A monogenetic volcanic field is a group of small monogenetic volcanoes, each of which erupts only once, as opposed to polygenetic volcanoes, which erupt repeatedly over a period of time. Many monogenetic volcanoes are cinder cones, often with lava flows, such as Parícutin in the Michoacán-Guanajuato volcanic field, which erupted from 1943 to 1952. Some monogenetic volcanoes are small lava shields, such as Rangitoto Island in the Auckland volcanic field.".
- Q900734 label "Monogenetic volcanic field".