본문으로 건너뛰기

코스타리카 · 성층화산

Platanar

화산 유형
성층화산
해발
2267m
마지막 분화
미확인
Platanar
사진: Green Mostaza · CC BY 4.0 · Wikimedia Commons
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 요약

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.

Wikipedia · CC BY-SA · 전체 기사 보기 →

분화 이력

용어집

상세 타임라인

분화 기록이 없습니다.

주변 화산

외부 링크

⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.