Palaeomagnetic results from lava flows recording a geomagnetic polarit
y reversal at Steens Mountain, Oregon suggest the occurrence of brief
episodes of astonishingly rapid field change of six degrees per day. T
he evidence is large, systematic variations in the direction of remane
nt magnetization as a function of the temperature of thermal demagneti
zation and of vertical position within a single flow, which are most s
imply explained by the hypothesis that the field was changing directio
n as the flow cooled.