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and continued down the valley for 6 km. These lava flows are considered
Holocene in age given the lack of a soil cover and their placement above a Pleistocene river terrace. Smbatassar cinder cones likewise generated two lava flows of 11 and 17 km length that overlie Pleistocene
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Karakhanian, A.; Djrbashian, R.; Trifonov, V.; Philip, H.; Arakelian, S.; Avagian, A. (2002). "Holocene-historical volcanism and active faults as natural risk factors for
Armenia and adjacent countries".
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terraces, thus also dating to the
Holocene. Legends of the destruction of the towns Yegheghis and Moz in 735 AD may be linked to activity in these volcanoes.
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462:location article is a
165:2000 BCE ± 1000 years
112:39.58167°N 45.67861°E
518:Mountains of Armenia
513:Volcanoes of Armenia
352:Mountains of Armenia
83:Volcanoes in Armenia
296:2002JVGR..113..319K
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231:. VolcanoDiscovery
117:39.58167; 45.67861
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264:. Retrieved
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233:. Retrieved
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225:"Dar-Alages"
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90:Coordinates
24:Vaiyots-Sar
507:Categories
392:Dar-Alages
211:References
196:Arpa river
188:Lake Sevan
184:lava cones
180:Դարալագյազ
172:Dar-Alages
103:45°40′43″E
100:39°34′54″N
49:Dar-Alages
19:Dar-Alages
402:Kaputjugh
397:Gutanasar
312:0377-0273
229:Volcanoes
186:south of
128:Geography
68:Elevation
422:Niphates
387:Azhdahak
362:Achkasar
176:Armenian
460:Armenia
412:Khustup
377:Aramazd
372:Aragats
292:Bibcode
235:July 9,
192:Armenia
143:Geology
137:Armenia
133:Country
78:Listing
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266:9 July
458:This
427:Porak
464:stub
308:ISSN
268:2015
237:2015
200:Vayk
367:Ara
300:doi
288:113
198:at
190:in
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
