Gravitational Evidence for a Low-Density Mass beneath the Galápagos Islands
J. E. Case 1,
S. L. Ryland 2,
Tom Simkin 3, and
K. A. Howard 4
1 U.S. Geological Survey, P.O. Box 6732, Corpus Christi, Texas 78411
2 California Institute of Technology, Pasadena 91109
3 Smithsonian Institution, Washington, D.C. 20560
4 U.S. Geological Survey, Menlo Park, California 94025
A residual negative free-air and Bouguer anomaly of at least 80 milligals, superimposed on a broader high, occurs over the Galápagos Islands The axis of the anomaly trends roughly east and plunges eastward. Thus, a low-density mass in the crust or upper mantle must underlie the archipelago. This anomaly may be caused by thermal expansion over a crust-mantle " hot spot".