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나루코산

Naruko

칼데라 · Japan · 470m

Katanuma lake in the 5.5 x 7 km Narugo caldera is seen from its NW shore with Ogadake lava dome on the right-center horizon. It is the highest of a cluster of lava domes surrounding the lake at 470 m above sea level. Katanuma is one of the most acidic crater lakes in Japan, with a pH of 1.6, and sulfur is mined from sediments on the lake floor.
Katanuma lake in the 5.5 x 7 km Narugo caldera is seen from its NW shore with Ogadake lava dome on the right-center horizon. It is the highest of a cluster of lava domes surrounding the lake at 470 m above sea level. Katanuma is one of the most acidic crater lakes in Japan, with a pH of 1.6, and sulfur is mined from sediments on the lake floor. · 사진: Copyrighted photo by Jun'ichi Itoh (Japanese Quaternary Volcanoes database, RIODB, http://riodb02.ibase.aist.go.jp/strata/VOL_JP/EN/index.htm and Geol Surv Japan, AIST, http://www.gsj.jp/). · Wikimedia Commons
화산 유형
칼데라
국가
Japan
지역
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
해발
470m
좌표
38.729, 140.734
마지막 분화
837년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Cluster
주요 암석
Rhyolite
지질학적 요약

Naruko is a poorly defined, 5.5 x 7 km caldera NW of the city of Sendai. Formed during eruptions about 73,000 and 45,000 years ago, it contains a cluster of four dacitic lava domes of Holocene age surrounding the 400-m-wide lake-filled Katanuma crater. The highest of the low, but steep-sided lava domes, Ogadake, lies SE of the lake and reaches only 470 m above sea level. Ogadake and Kurumigadake domes are capped by conglomerates and mudstones uplifted during dome growth. The only recorded eruption in occurred in 837 CE. Water vapor and sulfur-dioxide gas emission occurs from Shurado crater on Toyagamori lava dome west of the lake and from the bottom of the crater lake, which is one of the most acidic in Japan, with a pH of 1.6. Solfataras are found on the western shore of Katanuma, and sulfur is mined from sediments on the lake floor.

Wikipedia 요약

영어 요약

Naruko is a stratovolcano located in Ōsaki, Miyagi Prefecture, Japan. The volcano consists of a 7 km wide caldera with several lava domes. The summit of the 470 m high Mt. Kurumigatake is one of the four lava domes located in the center of the caldera. The volcano is well known because of its relationship to the Naruko Hot Springs Villages. However, its lack of well-defined features makes it difficult to recognize for a casual observer. The Japan Metrological Agency considers Naruko to be an active volcano.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
4400 BCE~4206 BCE · 1건 · 최고 VEI ?1491 BCE~1297 BCE · 2건 · 최고 VEI ?909 BCE~715 BCE · 1건 · 최고 VEI ?643~837 · 1건 · 최고 VEI 14400 BCE3042 BCE1878 BCE521 BCE643

상세 타임라인

  1. 837년VEI 1관측 기록
    837-05-27 ~ 진행 중
  2. 기원전 800년VEI ?지질학적 추정
    BCE 800 ~ 진행 중
  3. 기원전 1350년 (±50년)VEI ?지질학적 추정
    BCE 1350 ~ 진행 중
  4. 기원전 1400년VEI ?지질학적 추정
    BCE 1400 ~ 진행 중
  5. 기원전 4400년VEI ?지질학적 추정
    BCE 4400 ~ 진행 중

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