Ksudach
Stratovolkan · Russia · 1007 m

- Tipe
- Stratovolkan
- Negara
- Russia
- Wilayah
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Ketinggian
- 1007 m
- Koordinat
- 51.804, 157.529
- Letusan terakhir
- 1907
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Caldera
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
Ksudach is unique among Kamchatka volcanoes in its morphology and geologic history. It is a large, low-angle stratovolcano, constructed of alternating basaltic-andesitic lavas and dacitic pyroclastics, and is truncated by an intricate complex of five calderas. An array of post-caldera structures is truncated by later calderas, the last three of which formed during the Holocene, about 7,900 and 5,000 BCE and about 240 CE. The latter eruption was the second largest in Kamchatka during the Holocene, and produced about 20 km3 of rhyodacitic airfall tephra and 3-4 km3 of pyroclastic flows. The eastern part of the caldera complex contains two lakes, the northern of which forms an embayment in Shtyubel' (Stubel) Crater, a low-angle cone that began forming about 1,600 years ago in the youngest caldera. The only historical eruption, in 1907, originated from Shtyubel'.
Ringkasan Wikipedia
Ringkasan InggrisKsudach is a stratovolcano in southern Kamchatka, Russia. The last eruption of Ksudach was in March 1907, on or around 28 March, which was one of the largest ever recorded in Kamchatka with a Volcanic Explosivity Index of 5. The summit area comprises overlapping calderas. Two lakes, Bolshoe and Kraternoe, are located within calderas at the summit of Ksudach. These lakes, along with hot springs and the surrounding wilderness, make the Ksudach Volcano region a popular trekking destination. In the event of renewed volcanic activity, its remote location minimizes its potential hazard to humans.
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Riwayat letusan
Garis waktu rinci
- 1907VEI 5Teramati1907-03-28 – BerlangsungStubel
- 1750VEI 4Perkiraan geologi1750 – BerlangsungStubel
- 1000 (±50 tahun)VEI 4Perkiraan geologi1000 – BerlangsungStubel
- 700VEI ?Perkiraan geologi700 – Berlangsung
- 350VEI 2Perkiraan geologi350 – BerlangsungStubel
- 240 (±100 tahun)VEI 6Perkiraan geologi240 – BerlangsungKsudach V caldera
- 200 SMVEI 3Perkiraan geologiBCE 200 – Berlangsung
- 3000 SMVEI 4Perkiraan geologiBCE 3000 – Berlangsung
- 4100 SMVEI 3Perkiraan geologiBCE 4100 – Berlangsung
- 4550 SMVEI 3Perkiraan geologiBCE 4550 – Berlangsung
- 4750 SMVEI ?Perkiraan geologiBCE 4750 – BerlangsungSW part of caldera IV (Paryashchiy Utes)
- 4900 SMVEI 5Perkiraan geologiBCE 4900 – BerlangsungKsudach IV caldera
- 5200 SMVEI 5Perkiraan geologiBCE 5200 – BerlangsungKsudach IV caldera
- 5600 SMVEI ?Perkiraan geologiBCE 5600 – Berlangsung
- 7900 SMVEI 5Perkiraan geologiBCE 7900 – BerlangsungKsudach III caldera
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.