아르메니아 · 화쇄구
Dar-Alages
Vaiyots-Sar
- 화산 유형
- 화쇄구
- 해발
- 2575m
- 마지막 분화
- -2000년

- 화산 유형
- 화쇄구
- 국가
- 아르메니아
- 지역
- 아라비아·중앙아시아 / Caucasus Volcanic Province
- 해발
- 2575m
- 좌표
- 39.797, 45.497
- 마지막 분화
- -2000년
- 판구조 환경
- 판 내부 / 대륙 지각 (> 25 km)
- 화산 지형
- 소규모 (현무암질)
- 주요 암석
- 안산암 / 현무암질 안산암
지질학적 요약
The Vaiyots-Sar pyroclastic cone is located in the southern Armenia province of Vayots Dzor in the western Vardenis Volcanic Highland south of Lake Sevan (Karakhanian et al., 2002); previous names such as Dar-Alages or Daly-Tapa are of Russian origin. Near the north end of the approximately 5 x 8 km flow field the 1.5-km-diameter cone rises about 300 m above the surrounding lavas, identified by Sviatlovsky (1959) as post-glacial. Oswald (1906) noted that steep escarpments of Nummulitic limestones were ~6 km NE of the cone across an lava-flow field. At the southern end of the flow field a fissure-fed lava flow several thousand years ago dammed the Arpah River near the town of Vyke and then flowed NW for 6 km; the flows overlie a late Pleistocene terrace and have little soil development (Karakhanian et al., 2002). The youthful-looking Smbatassar cinder cone, 17 km NW of Vaiyots-Sar, appears to be the source vent for Holocene lava flows that traveled 11 km N and 17 km S down two valleys (Karakhanian et al., 2002).
Wikipedia 요약
영어 요약Dar-Alages is a group of six cinder lava cones south of Lake Sevan in Armenia. Fissure eruptions from Vaiyots-Sar dammed the Arpa river at Vayk 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 Yeheghis river 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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분화 이력
2건 기록용어집상세 타임라인
- 753년VEI ?근거 미기재753 ~ 종료일 미상
- 기원전 2000년 (±1000년)VEI ?지질학적 추정기원전 2000 ~ 종료일 미상Vaiyots-Sar
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