Preliminary Atlas of Active Shallow Tectonic Deformation in the Puget Lowland, W
27,14 €
In 1985, when Gower and others summarized geological and geophysical evidence for the region's shallow faults, only one of these structures, the Saddle Mountain Fault Zone, had demonstrated earthquake activity during the Holocene, or past 10,000 years (Carson, 1973; Wilson and others, 1975, 1979).
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