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![]() Photograph by David R. Sherrod, May 1979 Tephra deposits consisting primarily of pumice lapilli erupted at Newberry volcano about 1,300 years ago from the Big Obsidian Flow vent. This trench is located on the east flank of Newberry on the Sand Hill lava flow, 3.2 km from the vent. |
The most recent eruption about 1,300 years ago began with a series of explosive events in the summit caldera that formed layers of tephra downwind. Large blocks of pumice and dense lava fragments as large as 1 meter in diameter were deposited within the caldera. At this site on the east flank of the volcano, the explosive activity resulted in pumice deposits mostly less than 3 m thick! Ash from these eruptions have been traced as far east as Idaho. See figure 3 of the Newberry report for illustration of activity. |
![]() Photograph by Norman S. MacLeod, May 1979 Ash-cloud deposit from a pyroclastic flow that was erupted in Newberry's caldera about 1,300 years ago from the Big Obsidian Flow vent. This site is located near the Big Obsidian Flow parking lot, only a few meters from the edge of the Big Obsidian Flow. |
As the intensity of the explosive activity increased, pyroclastic flows swept from the vent inside Newberry caldera and rushed into Paulina Lake, probably causing secondary explosions from the lake. Just beyond the margin of these pyroclastic-flow deposits, a layer of gray ash shown here atop older brown-colored volcanic rocks is evidence of a fast-moving ash cloud that raced ahead of the pyroclastic flow. See figure 3 of the Newberry report for illustration of activity. |
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URL of this document: http://volcanoes.usgs.gov/About/Highlights/NewberryHaz/NewbDetails.html