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Süphan Dağ volcan

lava dome, strato volcano, pyroclatsic flows 4158 m
Turkey, 38.93°N / 42.83°E
Condition actuelle: en sommeil (1 sur 5)
Style éruptif tipique: Explosive
Eruptions du volcan Süphan Dağ: 10.000 years ago
Derniers séismes proches:
TimeMag. / DepthDistanceLocation
Sat, 15 Jun
Sat, 15 Jun 01:44 UTCM 1.9 / 5 km43 km EASTERN TURKEY
Fri, 14 Jun
Fri, 14 Jun 22:28 UTCM 2 / 5 km37 km EASTERN TURKEY
Fri, 14 Jun 01:04 UTCM 1.6 / 22.1 km42 kmVAN GOLU
Thu, 13 Jun
Thu, 13 Jun 10:03 UTCM 2.2 / 18 km40 km EASTERN TURKEY
Tue, 11 Jun
Tue, 11 Jun 01:56 UTCM 2.6 / 5 km44 km EASTERN TURKEY
Voir tous
The huge lava dome and strato-volcano is situated north of the famous lake Van.

Introduction:

A glacial ice cap covers the top of the lava dome. It is the second highest volcano of Turkey. During construction of the volcano andesitic-dacitic lava flows alternated with fluid basaltic flows, followed by construction of a large lava dome over the central vent. The flanks of the volcano are dotted with numerous lava domes and pyroclastic cones erupted along radial and circumferential fissures, particularly on the northern, souther, and eastern sides. The 1.5-km-wide, low-rimmed Aygirgölü maar was erupted on the lower southern flank. During the latest stage of activity, voluminous basaltic lava flows traveled as far as 30 km from the summit. Potassium-Argon dates for Süphan Dağ range from 2 to about 0.1 million years, but the latest basaltic eruption occurred about 10,000 years ago (Yilmaz et al., 1998).


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