Jepang · Stratovolkan
Gunung Haruna
Harunasan
- Tipe
- Stratovolkan
- Ketinggian
- 1449 m
- Letusan terakhir
- 550

- Tipe
- Stratovolkan
- Negara
- Jepang
- Wilayah
- Pasifik Barat Laut / Northeast Japan Volcanic Arc
- Ketinggian
- 1449 m
- Koordinat
- 36.477, 138.851
- Letusan terakhir
- 550
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Andesit / Andesit basaltik
Ringkasan geologi
Harunasan is truncated by a small summit caldera containing the symmetrical post-caldera pyroclastic cone of Haruna-Fuji. Harunasan formed prior to 300,000 years ago and had caldera-producing eruptions at about 200,000 and 40,000 years ago. Viscous lava flows and lava domes were subsequently extruded within and around the caldera, the western side of which is currently partially filled by Lake Haruna. The Futatsudake lava dome east of the caldera was the source of two large explosive eruptions during the 6th century CE.
Ringkasan Wikipedia
Ringkasan InggrisMount Haruna is a dormant stratovolcano in Gunma Prefecture, in the Kantō region of eastern Honshū, Japan.
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Riwayat letusan
3 tercatatGlosariumGaris waktu rinci
- 550 (±10 tahun)VEI 5Perkiraan geologi550-06-01 – akhir tidak diketahuiFutatsu-dake
- 520 (±10 tahun)VEI 4Perkiraan geologi520-06-01 – akhir tidak diketahuiFutatsu-dake
- 450 (±50 tahun)VEI 3Perkiraan geologi450 – akhir tidak diketahuiFutatsu-dake
Gunung api terdekat
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.