コスタリカ · 成層火山
プラタナル火山
Platanar
- タイプ
- 成層火山
- 標高
- 2267m
- 最終噴火
- 不明

- タイプ
- 成層火山
- 国
- コスタリカ
- 地域
- 中央アメリカ・カリブ海 / Central America Volcanic Arc
- 標高
- 2267m
- 座標
- 10.300, -84.366
- 最終噴火
- 不明
- テクトニクス環境
- 沈み込み帯 / 大陸地殻 (> 25 km)
- 火山地形
- 複成火山
- 主要岩石
- 安山岩 / 玄武岩質安山岩
地質学的概要
The Platanar volcanic center is the NW-most volcano in the Cordillera Central of Costa Rica. The massive complex covers about 900 km2 and is dominated by two largely Pleistocene stratovolcanoes, Platanar and Porvenir. These volcanoes were constructed within the Pleistocene Chocosuela caldera, which may have formed during a major slope failure. The Cerro Platanar volcano (known locally as Volcán Congo) on the N side of the complex has prehistorical lava flows on its W flanks and is the youngest volcanic center. The highest peak is Porvenir, whose summit crater lies 3 km S of Platanar. A thin layer of phreatic ash suggested that an eruption from Platanar occurred within the past few thousand years (Stine and Banks, 1991). The Aguas Zarcas group of nine basaltic cinder cones, located on the N flank of the Platanar-Porvenir complex to as low as 160 m altitude is, in part, Holocene in age.
Wikipedia の要約
英語版の要約Platanar Volcano is a dormant stratovolcano located in the Cordillera Central mountain range. It is located within Juan Castro Blanco National Park. In 1968, 2,500 hectares on Cerro Platanar were converted into a national forest.
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