“…Goff and Lackner (1998) evaluated ultramafic bodies in the United States as sources of magnesium for CO, sequestration with an emphasis on two California sites: the Del Puerto ultramtilc mass and the Wilbur Springs serpentinite. The reactivity of various ultramafic rocks, as conducted in simple acid dissolution experiments, was compared by Goff et al (1997). Goff and Guthrie (1999) discussed the geology, tectonics, alteration hktory, present exploitation, and environmental situation of extensive ultramafic deposits in the Clear Lake region, California.…”