코스타리카 · 성층화산
Platanar
- 화산 유형
- 성층화산
- 해발
- 2267m
- 마지막 분화
- 미확인

- 화산 유형
- 성층화산
- 국가
- 코스타리카
- 지역
- 중앙아메리카·카리브해 / Central America Volcanic Arc
- 해발
- 2267m
- 좌표
- 10.300, -84.366
- 마지막 분화
- 미확인
- 판구조 환경
- 섭입대 / 대륙 지각 (> 25 km)
- 화산 지형
- 복성화산체
- 주요 암석
- 안산암 / 현무암질 안산암
지질학적 요약
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 요약
영어 요약Platanar 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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