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Etrusk volcan

Stratovolcano 3100 m / 10171 ft
Turkey, 39.03°N / 43.66°E
Condition actuelle: (probablement) éteint (0 sur 5) | Reports
Etrusk livres
Style éruptif tipique: unspecified
Eruptions du volcan Etrusk: None during the past 10,000 years
Less than few million years ago (Pleistocene)
HeureMag. / DepthDistanceLocation
Thu, 4 Jun 2020 (UTC)
Thu, 4 Jun 07:15 UTCM 3.0 / 5 km21 kmErmisler-(van) (Turkey)
Tue, 2 Jun 2020 (UTC)
Tue, 2 Jun 08:13 UTCM 2.9 / 10 km20 kmEastern Turkey
Sun, 31 May 2020 (UTC)
Sun, 31 May 11:39 UTCM 3.3 / 5 km29 kmDegirmenozu-(van) (Turkey)
Sat, 30 May 2020 (UTC)
Sat, 30 May 05:14 UTCM 2.0 / 5 km27 kmDerebey-(van) (Turkey)
Tue, 26 May 2020 (UTC)
Tue, 26 May 22:41 UTCM 2.3 / 5 km26 kmBagdasan-(van) (Turkey)
Voir tous

Introduction:

As described by Oyan et al. (2010), the Pliocene Etrüsk volcano is one of the major volcanic centers of eastern Anatolia, just NE of Lake Van. There is a ~5-km-wide horseshoe-shaped caldera near the center of the volcano, with the Pleistocene Karniyak scoria cone about 11 km away on the SW flank near the lake. K-Ar age determinations by Oyan et al (2010) indicate that the main volcanic edifice of Etrusk was formed between 4.3 and 3.9 Ma, ending with caldera collapse. Between ~1 and 0.43 Ma, basalts erupted from the SW flank, predominantly from a ~N-S extending fissure, as well as from Karniyarik hill and a maar-shaped volcanic center (Düzgeyikçukuru). Lebedev et al. (2009) noted that the youngest dated trachybasalt from Karniyarek was 0.36 +/- 0.06 Ma.
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Source: Smithsonian / GVP volcano information

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See also: Sentinel hub | Landsat 8
 

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