Geophysicists suggest that large chunks of an ancient tectonic plate known as the Farallon Plate are still present under parts of central California and Mexico. The Isabella anomaly, IA, is at the same depth as other fragments of the Farallon plate under Oregon and Washington (Forsyth lab / Brown University) Around 100 million years ago, the Farallon oceanic plate lay between the converging Pacific and North American plates, which eventually came...
