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New evidence for extraordinarily rapid change of the geomagnetic field
during a reversal R. S. Coe*, M. Prévot† & P. Camps†
*Earth
Sciences Department, University of California, Santa Cruz, California 95064,
USA
†Laboratoire de Géophysique et
Tectonique, Université de Montpellier 2, URA CNRS 1760, 34095
Montpellier Cédex 05, France
Palaeomagnetic results from lava flows recording a geomagnetic polarity
reversal at Steens Mountain, Oregon suggest the occurrence of brief episodes of
astonishingly rapid field change of six degrees per day. The evidence is large,
systematic variations in the direction of remanent magnetization as a function
of the temperature of thermal demagnetization and of vertical position within a
single flow, which are most simply explained by the hypothesis that the field
was changing direction as the flow cooled.
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