IntroductionVents near Pisgah crater were the source of mostly pahoehoe lava flows that traveled 8 km SE to Lavic Lake, and in a narrow lobe as far as 18 km west of the vent. Paleomagnetic, argon-argon, and cosmogenic helium dated locate it at about 25,000 years before present. Another very youthful looking, but undated cinder cone and lava field of the Lavic Lake volcanic field is located in the Sunshine Peak area of the Lava Beds Mountains, south of the better known Pisgah Crater.
Source: GVP Lavic Lake information
See also: Sentinel hub | Landsat 8