Mount Iwate
Iwatesan
Vulcano complesso · Japan · 2038 m

- Tipo
- Vulcano complesso
- Paese
- Japan
- Regione
- Pacifico nord-occidentale / Northeast Japan Volcanic Arc
- Altitudine
- 2038 m
- Coordinate
- 39.853, 141.001
- Ultima eruzione
- 1919
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Basalt / Picro-Basalt
Sintesi geologica
Viewed from the east, Iwatesan volcano has a symmetrical profile that invites comparison with Fuji, but on the west an older cone is visible containing an oval-shaped, 1.8 x 3 km caldera. After the growth of Nishi-Iwate volcano beginning about 700,000 years ago, activity migrated eastward to form Higashi-Iwate volcano. Iwate has collapsed seven times during the past 230,000 years, most recently between 739 and 1615 CE. The dominantly basaltic summit cone of Higashi-Iwate volcano, Yakushidake, is truncated by a 500-m-wide crater. It rises well above and buries the eastern rim of the caldera, which is breached by a narrow gorge on the NW. A central cone containing a 500-m-wide crater partially filled by a lake is located in the center of the oval-shaped caldera. A young lava flow from Yakushidake descended into the caldera, and a fresh-looking lava flow from the 1732 eruption traveled down the NE flank.
Storia delle eruzioni
Cronologia dettagliata
- 1934VEI ?Stima geologica1934-07-16 – 1935-07-02
- 1919VEI 1Osservata1919-07-15 – 1919-07-15W side of Onigajo caldera (O-jigokudani)
- 1732VEI 2Osservata1732-01-22 – 1732-10NE flank of Yakushi-dake
- 1689VEI 2Stima geologica1689-06-22 – In corso
- 1687VEI 2Stima geologica1687-04-14 – 1687-07
- 1686VEI 3Osservata1686-03-26 – 1686-03-27
- 1450 (±100 anni)VEI ?Stima geologica1450 – In corsoNishi-Iwate and Higashi-Iwate
- 1300 (±50 anni)VEI 3Stima geologica1300 – In corsoHigashi-Iwate (Myoko-dake)
- 150VEI ?Stima geologica150 – In corsoHigashi-Iwate
- 350 a.C.VEI ?Stima geologicaBCE 350 – In corsoHigashi-Iwate
- 450 a.C.VEI ?Stima geologicaBCE 450 – In corsoNishi-Iwate (O-jigokudani area)
- 1150 a.C.VEI ?Stima geologicaBCE 1150 – In corsoNishi-Iwate
- 1250 a.C.VEI 3Stima geologicaBCE 1250 – In corsoHigashi-Iwate
- 1500 a.C. (±300 anni)VEI ?Stima geologicaBCE 1500 – In corsoHigashi-Iwate
- 1650 a.C.VEI ?Stima geologicaBCE 1650 – In corsoNishi-Iwate (O-jigokudani area)
- 2000 a.C.VEI ?Stima geologicaBCE 2000 – In corsoNishi-yama
- 2050 a.C. (±200 anni)VEI ?Stima geologicaBCE 2050 – In corsoHigashi-Iwate
- 2700 a.C. (±200 anni)VEI ?Stima geologicaBCE 2700 – In corsoHigashi-Iwate
- 2950 a.C. (±50 anni)VEI ?Stima geologicaBCE 2950 – In corsoNishi-Iwate
- 3050 a.C.VEI ?Stima geologicaBCE 3050 – In corsoHigashi-Iwate
- 3250 a.C. (±500 anni)VEI 0Stima geologicaBCE 3250 – In corso
- 3750 a.C. (±100 anni)VEI ?Stima geologicaBCE 3750 – In corsoHigashi-Iwate
- 4350 a.C. (±500 anni)VEI ?Stima geologicaBCE 4350 – In corsoHigashi-Iwate
- 4450 a.C. (±500 anni)VEI 0Stima geologicaBCE 4450 – In corsoHigashi-Iwate
- 4850 a.C. (±50 anni)VEI ?Stima geologicaBCE 4850 – In corsoNishi-Iwate
- 4900 a.C. (±100 anni)VEI ?Stima geologicaBCE 4900 – In corsoHigashi-Iwate
- 5650 a.C. (±50 anni)VEI ?Stima geologicaBCE 5650 – In corsoNishi-Iwate
- 6300 a.C. (±100 anni)VEI ?Stima geologicaBCE 6300 – In corsoNishi-Iwate
- 6450 a.C. (±1600 anni)VEI ?Stima geologicaBCE 6450 – In corso
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.