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Udina

Estratovolcán · Russia · 2886 m

The Udina volcanic massif consists of two cones constructed along a WNW-ESE line at the south end of the Klyuchevskaya volcanic group, and SE of Tolbachik. The western cone is Bolshaya Udina, seen here from the south, and has a lava dome on the SW flank. The smaller Malaya Udina is out of view to the right.
The Udina volcanic massif consists of two cones constructed along a WNW-ESE line at the south end of the Klyuchevskaya volcanic group, and SE of Tolbachik. The western cone is Bolshaya Udina, seen here from the south, and has a lava dome on the SW flank. The smaller Malaya Udina is out of view to the right. · Foto: Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
Tipo
Estratovolcán
País
Russia
Región
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitud
2886 m
Coordenadas
55.758, 160.527
Última erupción
Desconocido
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

The Udina volcanic massif consists of two conical stratovolcanoes constructed along a WNW-ESE line at the south end of the Kliuchevskaya volcanic group, SE of Tolbachik volcano. The andesitic western volcano, Bolshaya Udina, has a prominent lava dome on its SW flank. The basaltic Malaya Udina rises above a low saddle at the eastern end of the complex; small lava domes also occur on its flanks.

Resumen de Wikipedia

Udina es un macizo volcánico situado en el centro de la península de Kamchatka, en la Federación de Rusia. Comprende dos estratovolcanes cónicos: el Bolshaya Udina y el Málaya Udina.

Wikipedia · CC BY-SA · Leer artículo completo

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⚠ Solo como referencia. No apto para respuesta ante emergencias.