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Ararat volcano

stratovolcano 5165 m
Turkey, 39.7°N / 44.3°E
Current status: dormant (1 out of 5)
Ararat webcams / live data
Ararat volcano books
Typical eruption style: explosive
Ararat volcano eruptions: 1840 AD
TimeMag. / DepthDistanceLocation
Tue, 2 Jan
Tue, 2 Jan 02:25 UTCM 2.9 / 5 km26 kmTURKIYE-IRAN SINIR BOLGESI
Wed, 20 Dec
Wed, 20 Dec 12:20 UTCM 2.2 / 21.9 km25 kmSAGDIC-DOGUBAYAZIT (AGRI)
Sun, 17 Dec
Sun, 17 Dec 04:55 UTCM 2.1 / 5.6 km43 kmTURKIYE-IRAN SINIR BOLGESI
Thu, 7 Dec
Thu, 7 Dec 13:22 UTCM 2.6 / 2 km40 km TURKEY-IRAN BORDER REGION
Fri, 1 Dec
Fri, 1 Dec 07:25 UTCM 1.9 / 5 km35 kmASAGICIFTLIK-ARALIK (IGDIR)
View all recent quakes
The 5165-m-high, double-peaked stratovolcano Mount Ararat, also known as Agri Dagi, is Turkey's highest, largest volume, and easternmost volcano.

Background:

Glacier-clad Ararat, along with its twin volcano, 3925-m-high Kucuk Ararat (or Lesser Ararat), covers an area of 1000 sq km at the eastern end of a SSW-ESE line of volcanoes extending from Nemrut Dagi. Construction of the Greater and Lesser Ararat volcanoes was followed by a period of extensive flank eruptions, many erupted along N-S-trending fissures. The initial stage of flank eruptions produced a cluster of cinder cones and dacitic-rhyolitic lava domes surrounding Greater Ararat and a series of pyroclastic cones and domes on the western flank of Lesser Ararat. Late-stage activity formed large pyroclastic cones lower on the flanks of the two volcanoes. Ararat appears to have been active during the 3rd millennium BC; pyroclastic-flow deposits overlie early Bronze Age artifacts and human remains. Karakhanian et al. (2002) reported historical evidence for a phreatic eruption and pyroclastic flow at the time of a July 1840 earthquake and landslide.

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