Ksudach
Stratovolcano · Russia · 1007m

- Type
- Stratovolcano
- Country
- Russia
- Region
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Elevation
- 1007m
- Coordinates
- 51.804, 157.529
- Last eruption
- 1907
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
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'.
From Wikipedia
Ksudach 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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Eruption history
Detailed timeline
- 1907VEI 5Observed1907-03-28 – OngoingStubel
- 1750VEI 4Geological estimate1750 – OngoingStubel
- 1000 (±50 yrs)VEI 4Geological estimate1000 – OngoingStubel
- 700VEI ?Geological estimate700 – Ongoing
- 350VEI 2Geological estimate350 – OngoingStubel
- 240 (±100 yrs)VEI 6Geological estimate240 – OngoingKsudach V caldera
- 200 BCEVEI 3Geological estimateBCE 200 – Ongoing
- 3000 BCEVEI 4Geological estimateBCE 3000 – Ongoing
- 4100 BCEVEI 3Geological estimateBCE 4100 – Ongoing
- 4550 BCEVEI 3Geological estimateBCE 4550 – Ongoing
- 4750 BCEVEI ?Geological estimateBCE 4750 – OngoingSW part of caldera IV (Paryashchiy Utes)
- 4900 BCEVEI 5Geological estimateBCE 4900 – OngoingKsudach IV caldera
- 5200 BCEVEI 5Geological estimateBCE 5200 – OngoingKsudach IV caldera
- 5600 BCEVEI ?Geological estimateBCE 5600 – Ongoing
- 7900 BCEVEI 5Geological estimateBCE 7900 – OngoingKsudach III caldera
External links
⚠ For reference only. Not for emergency response.