Mount Elbrus
Elbrus
Stratovolcano · Russia · 5642m

- Type
- Stratovolcano
- Country
- Russia
- Region
- Arabia-Central Asia Volcanic Regions / Caucasus Volcanic Province
- Elevation
- 5642m
- Coordinates
- 43.351, 42.442
- Last eruption
- 50
- Tectonic setting
- Intraplate / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Dacite
Geological summary
Elbrus, the highest peak of the Caucasus Mountains of SW Russia, is a large glaciated stratovolcano. The summit area has two distinct peaks about 1 km apart, with a 250-m-wide crater on the eastern cone, separated by a low saddle from the western peak. Eruptive products cover 260 km2; its longest lava flow traveled 24 km down the NNE flank. Vlodavetz (in Blumenthal et al., 1964, CAVW) hypothesized that the most recent lava flows were 2,000-3,000 years old based on morphological appearance. Gushchenko (1979) noted explosive activity and a lava flow across a glacial moraine, and dated it at around 2,000 years ago. Weak solfataric activity has been reported near the summit, and hot springs are present on the flanks.
From Wikipedia
Mount Elbrus is the highest mountain in Russia and Europe. It is a dormant stratovolcano rising 5,642 m (18,510 ft) above sea level, and is the highest volcano in Eurasia, as well as the tenth-most prominent peak in the world. It is situated in the southern Russian republic of Kabardino-Balkaria in the western extension of Ciscaucasia, and is the highest peak of the Caucasus Mountains.
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Eruption history
Detailed timeline
- 50 (±50 yrs)VEI ?Geological estimate50 – Ongoing
External links
⚠ For reference only. Not for emergency response.