Naruko
Caldera · Japan · 470 m

- Tipo
- Caldera
- País
- Japan
- Región
- Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
- Altitud
- 470 m
- Coordenadas
- 38.729, 140.734
- Última erupción
- 837
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Cluster
- Roca principal
- Rhyolite
Resumen geológico
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.
Resumen de Wikipedia
Resumen en inglésNaruko 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.
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Historial de erupciones
Línea de tiempo detallada
- 837VEI 1Observado837-05-27 – En curso
- 800 a. C.VEI ?Estimación geológicaBCE 800 – En curso
- 1350 a. C. (±50 años)VEI ?Estimación geológicaBCE 1350 – En curso
- 1400 a. C.VEI ?Estimación geológicaBCE 1400 – En curso
- 4400 a. C.VEI ?Estimación geológicaBCE 4400 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.