The 1 Alpine-Federal geothermal test, at an elevation of 8,556 feet in eastern Arizona, was drilled by the Arizona Department of Commerce and U.S. Department of Energy to obtain information about the hot-dry-rock potential of Precambrian rocks in the Alpine-Nutrioso area, a region of extensive basaltic volcanism in southern Apache County. The hole reached total depth of 4,505 feet in August 1993. Temperature measurements were taken through October 1993 when final temperature, gamma ray, and neutron logs were run. The Alpine-Federal hole is located just east of U.S. Highway 180/191 (old 180/666) at the divide between Alpine and Nutrioso, in sec. 23, T. 6 N., R. 30 E., in the Apache-Sitgreaves National Forest (Fig. 1). The town of Alpine is about 6 miles south of the wellsite and the Arizona-New Mexico state line is about 6 miles east. The basaltic Springerville volcanic field is just north of the wellsite (Crumpler, L.S., Aubele, J.C., and Condit, C.D., 1994). Although volcanic rocks of middle Miocene to Oligocene age (Reynolds, 1988) are widespread in the region, erosion has removed them from the main valleys between Alpine and Nutrioso. As a result, the 1 Alpine-Federal was spudded in sedimentary strata of Oligocene to Eocene age (Reynolds, 1988). These sedimentary strata are exposed in road cuts along the highway and consist of light-colored, fine-grained clastics with minor conglomerates. The White Mountains, formed of volcanic rocks, are to the west, Escudilla Mountain (capped by volcanic rocks) is north, the Datil volcanic field is east in west-central New Mexico, and the Mogollon Rim (also capped by volcanic rocks) is to the south. ( 17 pages) previously published in 1994, revised June, 2009