Jepang · Kaldera
Naruko
- Tipe
- Kaldera
- Ketinggian
- 470 m
- Letusan terakhir
- 837

- Tipe
- Kaldera
- Negara
- Jepang
- Wilayah
- Pasifik Barat Laut / Northeast Japan Volcanic Arc
- Ketinggian
- 470 m
- Koordinat
- 38.729, 140.734
- Letusan terakhir
- 837
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Gugusan gunung api
- Batuan utama
- Riolit
Ringkasan geologi
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.
Ringkasan Wikipedia
Ringkasan InggrisNaruko 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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Riwayat letusan
5 tercatatGlosariumGaris waktu rinci
- 837VEI 1Teramati837-05-27 – akhir tidak diketahui
- 800 SMVEI ?Perkiraan geologi800 SM – akhir tidak diketahui
- 1350 SM (±50 tahun)VEI ?Perkiraan geologi1350 SM – akhir tidak diketahui
- 1400 SMVEI ?Perkiraan geologi1400 SM – akhir tidak diketahui
- 4400 SMVEI ?Perkiraan geologi4400 SM – akhir tidak diketahui
Gunung api terdekat
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.