Barva Volcano
Barva
복합화산 · Costa Rica · 2906m

- 화산 유형
- 복합화산
- 국가
- Costa Rica
- 지역
- Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
- 해발
- 2906m
- 좌표
- 10.135, -84.100
- 마지막 분화
- -6050년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
One of three massive volcanoes close to the capital city of San José, Volcán Barva (Barba) is a complex volcano with multiple peaks and flank vents. Three peaks visible from the Central Valley give it the common local name of Las Tres Marías. The voluminous andesitic-to-dacitic Tiribí Tuff, exposed in the Central Valley, was erupted about 322,000 years ago. The summit area is dominated by a 2 x 3 km crater open to the ESE. One of the cones on the upper N flank contains a crater lake. Cones are also found on the S flanks, along with lava flows. The Los Angeles flow, one of the most recent, descends nearly to the city of Heredia. A large Plinian eruption occurred during the early Holocene. Eruptions were reported in 1760 or 1766, 1776? (also a mudflow), and 1867, but later visits to the summit did not provide evidence for recent activity.
Wikipedia 요약
영어 요약Barva Volcano is an andesitic stratovolcano complex in central Costa Rica, 22 kilometres (14 mi) north of San José, in Heredia Province. It is the highest point in Braulio Carrillo National Park at 9,534 feet (2,906 m). One source states that it is the largest volcano in Central America by area and volume, being about 40 kilometres (25 mi) in diameter.
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분화 이력
상세 타임라인
- 1867년VEI ?지질학적 추정1867-03 ~ 진행 중
- 기원전 6050년 (±2000년)VEI 4지질학적 추정BCE 6050 ~ 진행 중
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