A monogenetic volcanic field is a type of volcanic field consisting of 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. The small monogenetic volcanoes of these fields are the most common subaerial volcanic landform.
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| - Monogenetischer Vulkan (de)
- Champ volcanique monogénique (fr)
- 단성 화산 (ko)
- Monogenetic volcanic field (en)
- Monogenetische vulkaan (nl)
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| - Ein monogenetischer Vulkan entsteht, im Gegensatz zum polygenetischen Vulkan, durch nur eine Eruption oder eine auch mehrere Jahre andauernde Eruptionsphase. Viele Schlackenkegel, Tuffringe und Maare zählen zu diesem Typ. Diese Vulkane sind oft zu hunderten in sogenannten monogenetischen Vulkanfeldern versammelt. Ein anschauliches Beispiel ist der Schlackenkegel Paricutín in Mexiko, dessen Aufbauphase neun Jahre dauerte. (de)
- Un champ volcanique monogénique est un champ volcanique de fissures volcaniques isolées ; les champs volcaniques monogéniques sont considérés comme un type de volcan. Ils n'apparaissent que là où les réserves de magma du volcan sont très réduites. Aucune de ces fentes ne sont cependant assez proches les unes des autres, ou assez larges pour pouvoir former un volcan. (fr)
- 단성 화산(單成火山)은 화산의 일종으로, 단 한번만의 분화로 만들어지는 화산을 말한다. 대표적인 예는 아이슬란드의 라키 산, 대한민국 제주특별자치도의송악산 등이 있는데, 라키 산은 한 번 분화한 이후에 몇차례 분화를 또 했는데, 대표적으로 934년, 1783년의 분화가 유명하다. 이렇게 단성 화산은 한 번 분화하면 식어버리므로 휴화산 상태라고 할 수 있지만, 그렇다고 모두 휴화산인건 아니다. (ko)
- Een monogenetische vulkaan is een vulkaan die, in tegenstelling tot polygenetische vulkanen, slechts één keer uitbarst en daarna nooit meer actief wordt. De meeste monogenetische vulkanen zijn askegels, zoals de bekendste voorbeelden hieronder. (nl)
- A monogenetic volcanic field is a type of volcanic field consisting of 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. The small monogenetic volcanoes of these fields are the most common subaerial volcanic landform. (en)
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| - Ein monogenetischer Vulkan entsteht, im Gegensatz zum polygenetischen Vulkan, durch nur eine Eruption oder eine auch mehrere Jahre andauernde Eruptionsphase. Viele Schlackenkegel, Tuffringe und Maare zählen zu diesem Typ. Diese Vulkane sind oft zu hunderten in sogenannten monogenetischen Vulkanfeldern versammelt. Ein anschauliches Beispiel ist der Schlackenkegel Paricutín in Mexiko, dessen Aufbauphase neun Jahre dauerte. (de)
- Un champ volcanique monogénique est un champ volcanique de fissures volcaniques isolées ; les champs volcaniques monogéniques sont considérés comme un type de volcan. Ils n'apparaissent que là où les réserves de magma du volcan sont très réduites. Aucune de ces fentes ne sont cependant assez proches les unes des autres, ou assez larges pour pouvoir former un volcan. (fr)
- A monogenetic volcanic field is a type of volcanic field consisting of 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. The small monogenetic volcanoes of these fields are the most common subaerial volcanic landform. 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 exceptionally large. 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. The magma supplying such fields is thought to have rapidly ascended from its source region, with only short resident times (decades or less) in shallow magma chambers. (en)
- 단성 화산(單成火山)은 화산의 일종으로, 단 한번만의 분화로 만들어지는 화산을 말한다. 대표적인 예는 아이슬란드의 라키 산, 대한민국 제주특별자치도의송악산 등이 있는데, 라키 산은 한 번 분화한 이후에 몇차례 분화를 또 했는데, 대표적으로 934년, 1783년의 분화가 유명하다. 이렇게 단성 화산은 한 번 분화하면 식어버리므로 휴화산 상태라고 할 수 있지만, 그렇다고 모두 휴화산인건 아니다. (ko)
- Een monogenetische vulkaan is een vulkaan die, in tegenstelling tot polygenetische vulkanen, slechts één keer uitbarst en daarna nooit meer actief wordt. De meeste monogenetische vulkanen zijn askegels, zoals de bekendste voorbeelden hieronder. (nl)
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