File:Hornito (24150729389).jpg

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A hornito from the north flank of Puʻu ʻŌʻō, Kīlauea volcano in Hawaii.

Explanation from the U.S. Geological Survey: "A hornito is a small rootless spatter cone that forms on the surface of a basaltic lava flow (usually pahoehoe). A hornito develops when lava is forced up through an opening in the cooled surface of a flow and then accumulates around the opening. Typically, hornitos are steep sided and form conspicuous pinnacles or stacks. They are "rootless" because they are fed by lava from the underlying flow instead of from a deeper magma conduit. The hornito in this photo recently formed over the lava tube on the north flank of Puʻu ʻŌʻō, Kīlauea volcano in Hawaii at the spot of a breakout that occurred on November 25."
Date
Source Hornito
Author U.S. Geological Survey from Reston, VA, USA
Camera location19° 23′ 39.29″ N, 155° 06′ 19.16″ W Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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This image was originally posted to Flickr by U.S. Geological Survey at https://flickr.com/photos/27784370@N05/24150729389. It was reviewed on 8 February 2016 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0.

8 February 2016

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Date/TimeThumbnailDimensionsUserComment
current22:38, 8 February 2016Thumbnail for version as of 22:38, 8 February 20163,648 × 2,736 (4.18 MB)Rhododendrites (talk | contribs)Transferred from Flickr via Flickr2Commons

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