Spatial Variability of the Depth to the Magma Reservoir Beneath the Yellowstone Caldera Inferred from Observations of Seiche Loading Induced Strain
Seiche waves in Yellowstone Lake at ~78, ~51, and ~25 minute periods and heights <10 cm can cause measurable strain (< 40 ns) as observed on borehole strainmeters both near (<300 m) and far (~20 km) from the lake. Observations of the correlation between the seiche waves and the associated s...
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| Format: | Others |
| Language: | en |
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LSU
2017
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| Online Access: | http://etd.lsu.edu/docs/available/etd-04022017-185535/ |