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- W2592648802 abstract "Summary The Chelmsford earthquake of June 23, 1938, occurred at 03h 57m 56s.5 G.C.T. The epicentral determination made by the writer of this article is 71° 25′ W, 42° 37′ N. The distance-arcual intersection occurs at the southernmost tip of an ellipse of greatest intensity, and this may be due to the fact that all three stations employed in the determination were to the south and west of the area, or that structural conditions elongated the greatest intensity area. The major axis of the ellipse does coincide with the strike of the geologic structure in this area. The greatest intensity given by the writer is IV on the Rossi-Forel Scale." @default.
- W2592648802 created "2017-03-16" @default.
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- W2592648802 date "1940-04-01" @default.
- W2592648802 modified "2023-09-24" @default.
- W2592648802 title "The Chelmsford, Massachusetts, earthquake of June 23, 1938*" @default.
- W2592648802 cites W140873457 @default.
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- W2592648802 doi "https://doi.org/10.1785/bssa0300020099" @default.
- W2592648802 hasPublicationYear "1940" @default.
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