Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 14 September 1973:
Vol. 181. no. 4104, pp. 1040 - 1042
DOI: 10.1126/science.181.4104.1040

Articles

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".





To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)