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Göllü Dağ vulkaan

stratovulkaan 2143 m
Turkey, 38.26°N / 34.55°E
Current status: normal or dormant (1 out of 5) | Reports
Göllü Dağ vulkaan boeken
Typical eruption style: explosive
Göllü Dağ vulkaanuitbarstingen: none in historic times
TijdMag. / DiepteAfstandLocatie
Tue, 16 Apr 2019
Tue, 16 Apr 06:50 UTCM 1.240 kmOzyurt-(nigde) (Turkey)
Fri, 12 Apr 2019
Fri, 12 Apr 08:59 UTCM 1.440 kmOzyurt-(nigde) (Turkey)
Thu, 11 Apr 2019
Thu, 11 Apr 09:08 UTCM 1.8 / 5 km29 kmKucukkoy-(nigde) (Turkey)
Thu, 4 Apr 2019
Thu, 4 Apr 09:36 UTCM 1.238 kmGumusler-(nigde) (Turkey)
Tue, 19 Mar 2019
Tue, 19 Mar 14:08 UTCM 1.539 kmOzyurt-(nigde) (Turkey)
Bekijk alle recente aardbevingen
Göllü Dağ, a 2143-m-high rhyolitic-to-rhyodacitic lava dome complex in central Anatolia, lies between the Hasan Dağ and Acigöl-Nevsehir volcanic complexes.

Background:

The volcano was active between 1.33 to 0.84 million years ago (Bigazzi et al., 1995). A large number of cinder cones are located adjacent to Göllü Dağ along a along N-S-trending fissures north of the lava dome complex and south of the Erdas Dağ massif. Lava domes and cinder cones overlie the buried silicic Derinkuyu caldera complex of Tertiary age. The hydrothermal alteration and hot springs are present in the Sahin Kalesi resurgent dome complex west of Göllü Dağ and on the southern flank of the Erdas Dağ massif north of Göllü Dağ.


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