Gunung Suoh
Suoh
Kaldera · Indonesia · 1000 m

- Tipe
- Kaldera
- Negara
- Indonesia
- Wilayah
- Sunda-Banda Volcanic Regions / Sunda Volcanic Arc
- Ketinggian
- 1000 m
- Koordinat
- -5.250, 104.270
- Letusan terakhir
- 2024
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Cluster
- Batuan utama
- No Data (checked)
Ringkasan geologi
The 8 x 16 km Suoh (or Suwoh) depression appears to have a dominantly tectonic origin, but contains a smaller complex of overlapping calderas oriented NNE-SSW. Historically active maars and silicic domes lie along the margins of the depression, which falls along the Great Sumatran Fault that extends the length of the island. Numerous hot springs occur along faults within the depression, which contains the Pematang Bata fumarole field. Large phreatic explosions (0.2 km2 tephra) occurred at the time of a major tectonic earthquake in 1933. Very minor hydrothermal explosions produced two 5-m-wide craters at the time of a February 1994 earthquake.
Ringkasan Wikipedia
Ringkasan InggrisSuoh or Suwoh is an 8 × 16 km wide volcano-tectonic depression in the southern part of Sumatra, Indonesia. Historical maars and silicic lava domes are found along the Great Sumatran fault line. Phreatic eruptions have been recorded after both the major 1933 and 1994 Liwa earthquake. It is located within the West Lampung Regency, Lampung Province. The volcano erupted again in a similar fashion on 24 May 2024.
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Riwayat letusan
Garis waktu rinci
- 2024VEI 1Teramati2024-05-24 – 2024-05-24Nirwana Crater
- 1933VEI 4Teramati1933-07-10 – 1933-08-05Pematang Bata
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.