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Global Volcanism Program | Image GVP-03078

This blocky lava flow in the McKenzie Pass area of the central Oregon Cascades originated from Yapoah scoria cone on the north flank of North Sister about 2,600-2,900 years ago. The flow traveled 5 km to the north before being deflected by lava flows from the Belknap and Little Belknap shield volcanoes and then flowed an additional 8 km to the NE. Photo by Lee Siebert, 1972 (Smithsonian Institution).

This blocky lava flow in the McKenzie Pass area of the central Oregon Cascades originated from Yapoah scoria cone on the north flank of North Sister about 2,600-2,900 years ago. The flow traveled 5 km to the north before being deflected by lava flows from the Belknap and Little Belknap shield volcanoes and then flowed an additional 8 km to the NE.

Photo by Lee Siebert, 1972 (Smithsonian Institution).

Creative Commons Icon This image is made available under the Public Domain Dedication CC0 license, but proper attribution is appreciated.

Keywords: lava flow | scoria cone


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