Magnetic Polarity of Pillow Basalts from Reykjanes Ridge
Jelle De Boer 1,
Jean-Guy Schilling 1, and
Dale C. Krause 1
1 Graduate School of Oceanography, University of Rhode Island, Kingston
A first attempt to measure directly the magnetic polarity of submarine basalts dredged from the Reykjanes Ridge indicates that the first two magnetic anomalies over the ridge resulted from a reversal of the earth's magnetic field. Volcanic criteria were used to determine the orientation the samples had before they were dredged from the sea floor.