File:USGS Kīlauea multimediaFile-1931.jpeg

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Description

Kīlauea's 2018 lower Puna eruption.

At 10:30 HST, ground shaking from a preliminary magnitude-5.0 earthquake south of Pu‘u ‘Ō‘ō caused rockfalls and possibly additional collapse into the Pu‘u ‘Ō‘ō crater on Kīlauea Volcano's East Rift Zone. A short-lived plume of ash produced by this event lofted skyward and dissipated as it drifted southwest from Pu‘u ‘Ō‘ō. Downwind areas may have experienced a dusting of ash from this plume. At this time, the 10:30 earthquake has caused no other changes at Kīlauea Volcano. HVO will continue to closely watch monitoring data for any changes. This image was captured from an HVO overflight carrying HVO scientists to the East Rift Zone for field work today. USGS photo by Kevan Kamibayashi.

Date
Source https://volcanoes.usgs.gov/volcanoes/kilauea/multimedia_chronology.html
https://volcanoes.usgs.gov/observatories/hvo/multimedia_uploads/multimediaFile-1931.jpg
Author United States Geological Survey
Camera location19° 24′ 07.08″ N, 155° 09′ 01.08″ W  Heading=98.9761° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location19° 23′ 19.57″ N, 155° 06′ 21.83″ W Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

Licensing

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Public domain
This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.

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current04:17, 17 November 2018Thumbnail for version as of 04:17, 17 November 20184,032 × 3,024 (1.91 MB)Batholith (talk | contribs)== {{int:filedesc}} == {{Information |description= Kīlauea's 2018 lower Puna eruption. {{Quote box |At 10:30 HST, ground shaking from a preliminary magnitude-5.0 earthquake south of Pu‘u ‘Ō‘ō caused rockfalls and possibly additional collapse into the Pu‘u ‘Ō‘ō crater on Kīlauea Volcano's East Rift Zone. A short-lived plume of ash produced by this event lofted skyward and dissipated as it drifted southwest from Pu‘u ‘Ō‘ō. Downwind areas may hav...

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