BeschreibungVaiyots-Sar volcano lies just north of the major Areni-Zanghezour Fault, near the town of Vaik, and produced a fissure-fed lava flow several thousand years ago that dammed the Arpah River and flowed to the west for 6 km. The flows overlie a late Pleistocene terrace and have little soil development.
The youthful-looking Smbatassar cinder cone is located 17 km to the NW and produced lava flows that traveled 11 and 17 km north and south, respectively.
Oswald (1906) noted that steep escarpments of Nummulitic limestones faced the “Dalykh-tapa” volcano, about 6 km NE across an extensive lava-flow field.
Siehe auch: Sentinel hub | Landsat 8 | NASA FIRMS