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Tana volcan

Stratovolcanoes 1170 m / 3,839 ft
United States, Aleutian Islands, 52.83°N / -169.77°W
Condition actuelle: normal / en sommeil (1 sur 5) | Reports
Tana livres
Style éruptif tipique: unspecified
Eruptions du volcan Tana: unknown, no recent eruptions No recent earthquakes
HeureMag. / DepthDistanceLocation

Introduction:

The Tana volcanic complex forming the eastern half of the dumbbell-shaped Chuginadak Island, opposite the dramatic conical Cleveland stratovolcano, is composed of two prominent E-W-trending volcanoes. The complex shows evidence of glacial erosion, but the observation on satellite imagery of highly irregular coastlines forming peninsulas west of Applegate Cove on the NW side of the complex and Concord Point on the south side imply lava flows of mid- to late-Holocene age (Nye 2007, pers. comm.). Prominent lava flow levees are visible near Concord Point, where a low-silica rhyolite sample was obtained. The undissected cone and youthful crater forming the western summit also imply a post-glacial age, and youthful cinder cones also lie east of the isthmus between Cleveland and Tana volcanoes.
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Smithsonian / GVP volcano information

Tana Photos:

Volcanic coast Los Hervideros, Montanas del fuego in background, Lanzarote Isl., Canaries (Photo: WNomad)
Volcanic coast Los Hervideros, Montanas del fuego in background, Lanzarote Isl., Canaries (Photo: WNomad)
 Lanzarote 2016 - Charco de los clicos Pt.1: An example of Hydrovolcanism - the crater of the volcano Montaña de Golfo (Photo: Ayasha27)
Lanzarote 2016 - Charco de los clicos Pt.1: An example of Hydrovolcanism - the crater of the volcano Montaña de Golfo (Photo: Ayasha27)



Derniers images satellite


See also: Sentinel hub | Landsat 8
 

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