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Bulletin of the Seismological Society of America; January 1961; v. 51; no. 1; p. 13-16
© 1961 Seismological Society of America
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A note on the amplitude-period relationship of earth noise in the one to eight second range

T. HATHERTON

GEOPHYSICS DIVISION, D.S.I.R.,, WELLINGTON, New Zealand

Abstract

Maximum values of surface particle displacement due to microseisms recorded at an Antarctic seismological station (Scott Base) are compared with the displacements obtained by Romney at Harvard and Pinewoods. The relation of the displacement to the fourth power of the period obtained by Romney is confirmed by the Antarctic data.






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