Energy & Resource Development of Continental Margins by Teh Fu Yen, D. Walsh, Don Walsh

By Teh Fu Yen, D. Walsh, Don Walsh

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Subsequently, 18 expensive tests have been drilled without finding com­ mercial accumulations and nearly half of the tracts that were leased have now been dropped. Similar, but not as costly, examples are in the Gulf of Alaska and the southern California borderland. A review of the latter area shows that since 1971, there have been several published estimates of undiscovered resources for the offshore area of southern California. These estimates have been widely divergent, but an accurate comparison cannot be made because of the different methods of reporting.

M. (1966), The Denver area earthquakes and the Rocky Mountain disposal well. The Mountain Geologist, _3 (1), p. 23-26. 12. J. and R. Berry (1973), Environmental hazards of the Santa Barbara Channel: Oil and gas seeps and Holocene faulting, in. Geology, Seismicity, and Environmental Impact. Assoc. Eng. Geologists, Spec. Pub. 13. , Jr. (1975), San Simeon-Hosgri fault system, coastal California: Economic and environmental implications. Science, 190, 1291. 14. V. , M. N. Feather (1963), Experimental deformation of sedimentary rocks under confining pressure: pore-pressure tests.

Nuclear power generation withdrawal and consumption requirements are derived essent­ ially for cooling needs, Nuclear plant water consumption factors vary with the type of plant and cooling processes used. 8 gallons per kilowatt hour is needed. The mining and processing of the raw fuel - uranium ore - also requires the use of some water. Our vast requirements for electrical power depend totally on the availability of cooling water from our lakes, rivers, and coastal zones. Indeed, if one excludes hydropower, which is thermally non-polluting, the purpose of all energy sources (fossil fuel, geothermal, or nuclear) is to create a high temperature, Tj_.

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