Anomalous delays of teleseismic P waves in Yellowstone National Park
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Abstract
TELESEISMIC P waves recorded by a short-period seismic network, comprising 12 stations, in Yellowstone National Park, show anomalous delays of 1–2 s in their travel times in the central region of the park relative to the surrounding area. To explain this phenomenon, I propose that a substantial body of low velocity material is present beneath the park, with horizontal dimensions of several tens of kilometres; it may be the magma chamber associated with the volcanism of Yellowstone (ref. 1, and G. P. Eaton et al., unpublished).
Study Area
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Anomalous delays of teleseismic P waves in Yellowstone National Park |
Series title | Nature |
DOI | 10.1038/253425a0 |
Volume | 253 |
Issue | 5491 |
Year Published | 1975 |
Language | English |
Publisher | Nature |
Description | 3 p. |
First page | 425 |
Last page | 427 |
Country | United States |
State | Wyoming |
Other Geospatial | Yellowstone National Park |
Google Analytic Metrics | Metrics page |