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| | Bob Smith: Research (Site not responding. Last check: 2007-09-17) |
 | | Yellowstone's climactic eruptions expelled ash flows with volumes of: 1) 2,500 km³ with 2.0 Ma Huckleberry Ridge tuff, 2) 280 km³ in the 1.2 Ma Mesa Falls tuff, and 3) 1,000 km³ with the 0.6 Ma Lava Creek tuff (Christiansen, 1984). |
 | | The historical seismicity of Yellowstone is marked by the large 1959, Hebgen Lake, Montana, Ms = 7.5 event located on the northwest margin of the caldera, its extensive aftershock sequence, and by extensive earthquake swarms within the Yellowstone caldera. |
 | | Notably the trend of this swarm projected northwest and was orthogonal to the caldera boundary, suggesting the possibility of a radial fracture extending from the caldera and a possible scenario for either a propagating fracture extending from the Hebgen Lake fault toward the caldera or as magma filled fracture extending radially outward from the caldera. |
| www.mines.utah.edu /~rbsmith/RESEARCH/YellowstoneHotspot.html (3739 words) |
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