Nisyros
Stratovolkan · Greece · 698 m

- Tipe
- Stratovolkan
- Negara
- Greece
- Wilayah
- European Volcanic Regions / Hellenic Volcanic Arc
- Ketinggian
- 698 m
- Koordinat
- 36.589, 27.155
- Letusan terakhir
- 1888
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Dacite
Ringkasan geologi
The easternmost volcano of the Aegean arc forms the 9-km-wide island of Nisyros, which is truncated by a 3-4 km wide caldera. The island was constructed during the past 150,000 years, with three cone-building stages including explosive and effusive andesitic eruptions and effusive and extrusive dacitic and rhyolitic activity. The age of the caldera is variously considered to be less than 24,000 years before present (BP) (Keller et al., 1990) and older than 44,000 years BP (Limburg and Varekamp, 1991). Five large post-caldera lava domes completely fill the western part of the caldera. The NE-most (Boriatiko) and SW-most (Karaviotis) lava domes and flows are significantly younger than the other domes. A sixth post-caldera dome, outside the SW caldera rim, produced lava flows that reached the coast. Historical phreatic eruptions occurred from craters within the caldera between 1422 and 1888. Intense hydrothermal activity continues in the form of many fumaroles on the caldera floor and hot springs along the coast.
Riwayat letusan
Garis waktu rinci
- 1888VEI 2Teramati1888-09-25 – BerlangsungPolyvotis Micros
- 1873VEI 2Teramati1873-06 – 1873-09-26Plegathon and Polyvotis
- 1871VEI 2Teramati1871 – BerlangsungPlegathon and Polyvotis
- 1422VEI 2Teramati1422 – Berlangsung
Tautan eksternal
- Belum ada di Wikipedia (Bahasa Indonesia). Anda dapat berkontribusi di Wikidata.
- 🔗 Halaman asli Smithsonian GVP
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