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Bulletin of the Seismological Society of America; January 1935; v. 25; no. 1; p. 62-80
© 1935 Seismological Society of America
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The first preliminary waves of the Nevada earthquake of December 20, 1932*

PERRY BYERLY

Abstract

The P travel-time curve of the Nevada earthquake is presented. It is drawn as a series of straight lines. It is near {Delta} = 28° that the data outline most clearly the sudden change in slope of the curve, but definite evidence of overlapping of the branches is lacking. At {Delta} = 67° (approximately) the curve branches into two parts as did the curve of the Texas earthquake. Between 4° and 12° three parallel P curves are drawn. The suggested explanation of them is that they are due to transformations of an original P or S at boundaries near the focus. This would indicate a depth of focus of about fifteen kilometers.

The nature of the first motion at the various stations shows a complex distribution which does not lead to a simple explanation of the forces acting at the focus.

A long-period component of P waves is observed, and it is concluded that it is present from very near the beginning of the record, although often masked by shorter-period motion. It begins in opposite phase to the shorter-period motion accompanying it.

Footnotes

* [Received for publication June 4, 1934.]




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