Abstract
Although hypocenters of earthquakes on the island of Hawaii are now routinely assigned to within 5km, depth was a poorly determined parameter until the early 1960's. However, the 1950-1960 period was very active both in volcanic eruptions and large earthquakes. Source depths for the 12 largest Hawaiian earthquakes (magnitude 6 or greater) since 1940 are estimated from the ratios of body and surface wave amplitudes recorded at Pasadena, California. In general, large earthquakes near the volcanic flanks and fault systems are shallow (= or < 20km). Two earthquakes of magnitude 6 occurred under the volcanoes Mauna Loa (in 1950) and Kilauea (in 1951); they preceded major eruptions by 3 days and 14 months, respectively, and had the largest depth estimates at 40-55km and 35-50km. -from Authors
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CITATION STYLE
Eissler, H. K., & Kanamori, H. (1986). Depth estimates of large earthquakes on the island of Hawaii since 1940. Journal of Geophysical Research, 91(B2), 2063–2076. https://doi.org/10.1029/JB091iB02p02063
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