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Random pictures

Süphan Dağ volcano

lava dome, strato volcano, pyroclatsic flows 4158 m
Turkey, 38.93°N / 42.83°E
Current status: dormant (1 out of 5) | Reports
Süphan Dağ volcano books
Typical eruption style: explosive
Süphan Dağ volcano eruptions: 10.000 years ago
TimeMag. / DepthDistanceLocation
Wed, 21 Feb
Wed, 21 Feb 19:20 UTCM 2.0 / 7.3 km40 kmMOLLAKASIM-(VAN)
Mon, 19 Feb
Mon, 19 Feb 16:40 UTCM 1.6 / 8.8 km40 kmVAN GOLU
Fri, 16 Feb
Fri, 16 Feb 19:44 UTCM 1.9 / 2.1 km30 kmADILCEVAZ (BITLIS)
Tue, 13 Feb
Tue, 13 Feb 05:33 UTCM 1.0 / 20.5 km35 kmVAN GOLU
Sun, 11 Feb
Sun, 11 Feb 00:16 UTCM 1.0 / 5 km13 kmCIMENLI-PATNOS (AGRI)
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The huge lava dome and strato-volcano is situated north of the famous lake Van.

Background:

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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