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Ivao volcan

cinder cones 1426 m / 4,678 ft
Urup Island, Iles Kuriles, 45.77°N / 149.68°E
Condition actuelle: normal / en sommeil (1 sur 5) | Reports
Ivao livres
Style éruptif tipique: strombolian
Eruptions du volcan Ivao: unknown No recent earthquakes
HeureMag. / DepthDistanceLocation
Ivao volcano is a group of several cinder cones on Urup Island, Kurile Islands. The cones are aligned NW-SE along the Krishtofovich Ridge of SW Urup Island.
The Ivao group itself consists of 3 young cones that are less than 10,000 years old. Ivao cone at the NW end is the highest of the group and the highest peak on Urup Island.
Lake Ivao has formed as a result of damming of a valley by the SE-most cone. Krutaya Mountain is the elongated central cone. It is the vent of the most recent eruption which erupted a viscous lava flow to the east.
(Source: GVP / Smithsonian volcano information)


Derniers images satellite


See also: Sentinel hub | Landsat 8

Ivao volcan

cinder cones 1426 m / 4,678 ft
Urup Island, Iles Kuriles, 45.77°N / 149.68°E
Condition actuelle: normal / en sommeil (1 sur 5) | Reports
Ivao livres
Style éruptif tipique: strombolian
Eruptions du volcan Ivao: unknown No recent earthquakes
HeureMag. / DepthDistanceLocation
Ivao volcano is a group of several cinder cones on Urup Island, Kurile Islands. The cones are aligned NW-SE along the Krishtofovich Ridge of SW Urup Island.
The Ivao group itself consists of 3 young cones that are less than 10,000 years old. Ivao cone at the NW end is the highest of the group and the highest peak on Urup Island.
Lake Ivao has formed as a result of damming of a valley by the SE-most cone. Krutaya Mountain is the elongated central cone. It is the vent of the most recent eruption which erupted a viscous lava flow to the east.
(Source: GVP / Smithsonian volcano information)


Derniers images satellite


See also: Sentinel hub | Landsat 8

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