The Edge Experiment and the U.S. East Coast Magnetic Anomaly

The EDGE experiment offshore the U.S. east coast obtained near vertical incidence seismic reflection data, as well as wide angle seismic reflection and seismic refraction data. These results are combined with magnetic total intensity data in order to establish the origin for the East Coast Magnetic Anomaly (ECMA) and to hypothesize about geological events taking place at the time that opening was initiated in the North Atlantic.