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Additional evidence relating to "A worldwide storm of microseisms with periods of about 27 seconds"

LAMONT GEOLOGICAL OBSERVATORY OF COLUMBIA UNIVERSITY, PALISADES, NEW YORK

Abstract

The hypothesis that the worldwide storm of ultralong period microseisms in early June 1961 was caused by ocean swell of the same periods striking the coast of the Gulf of Guinea is supported by mariners' observations of unusual swell and its effects at the places and times predicted by the hypothesis.

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