Abstract
A detailed seismological study of the mantle beneath the Bowie hotspot, west of Canada, reveals a zone of low seismic velocities. The anomaly, probed at a depth of ∼700 km, adds a delay of 0.15 s to the travel times of seismic waves traversing a region ∼150 km in diameter, located ∼150 km away from the vertical projection of the Bowie seamount. This observation suggests that a mantle plume is present in the lower mantle beneath Bowie, with the amplitude of the anomaly implying a temperature contrast of about ∼300 K.
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Nataf, HC., VanDecar, J. Seismological detection of a mantle plume?. Nature 364, 115–120 (1993). https://doi.org/10.1038/364115a0
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DOI: https://doi.org/10.1038/364115a0
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