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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
Thu, 18 May
Thu, 18 May 01:29 UTCM 2.0 / 24.7 km19 kmDEMIRTEPE-DOGUBAYAZIT (AGRI)
Wed, 17 May
Wed, 17 May 06:42 UTCM 2.6 / 5 km20 kmTOPCATAN-DOGUBAYAZIT (AGRI)
Sat, 13 May
Sat, 13 May 00:04 UTCM 1.9 / 5.4 km30 kmIGDIR
Fri, 28 Apr
Fri, 28 Apr 08:56 UTCM 2.1 / 5.9 km47 kmBAYRAKTUTAN-(IGDIR)
Thu, 13 Apr
Thu, 13 Apr 16:34 UTCM 2.6 / 1 km22 kmEASTERN TURKEY
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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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