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Tendürek Dağ volcan

stratovolcan 3584 m
Turkey, 39.35°N / 43.87°E
Condition actuelle: en sommeil (1 sur 5)
Style éruptif tipique: Explosive
Eruptions du volcan Tendürek Dağ: 1855 AD
Derniers séismes proches:
TimeMag. / DepthDistanceLocation
Tue, 11 Jun
Tue, 11 Jun 20:57 UTCM 2.8 / 6 km24 km TURKEY-IRAN BORDER REGION
Tue, 4 Jun
Tue, 4 Jun 12:37 UTCM 2.7 / 5 km17 km TURKEY-IRAN BORDER REGION
Sat, 1 Jun
Sat, 1 Jun 16:03 UTCM 2.3 / 21 km17 km TURKEY-IRAN BORDER REGION
Fri, 24 May
Fri, 24 May 02:39 UTCM 1.7 / 4.1 km20 kmKILAVUZ-CALDIRAN (VAN)
Wed, 22 May
Wed, 22 May 08:32 UTCM 2.3 / 20 km13 km EASTERN TURKEY
Voir tous
Tendürek Dagi, also known as Tendürük Dagi, is an elongated shield volcano that rises 1800 m above the plain of Dogubayazit, near the Iranian border, south of Mount Ararat.

Introduction:

An E-W-trending summit ridge, developed north of an arcuate caldera structure exposed only on the southern side, contains two well-developed cones. The higher western cone is capped by a steep-walled crater with a trachytic spine at its eastern edge. The flatter eastern crater contains a warm lake. The shield volcano developed during a period when highly mobile lava flows from the western crater covered an area of 500 sq km. Following summit caldera formation, numberous flank eruptions took place from N-S-trending fissures, producing viscous trachytic lava domes and flows as well as fluid basaltic pahoehoe flows that extend 10-20 km to the north and south. The lastest activity formed two major basaltic lava flows from large cones on the NE and SE flanks. An eruption took place from a vent on the SE flank about 2500 years ago, and a gas-and-ash eruption took place in 1855.


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