[en] The Salt Lake City quadrangle in northeastern Utah contains portions of the Uinta Uplift, Uinta and Green River Basins, the Sevier Overthrust Belt, and the Basin-Range Province. Tertiary sediments dominate in the basins, Quaternary surface deposits and Precambrian sedimentary rocks are prevalent in the Uinta Uplift. Portions of the Uinta Uplift, and most of the Wasatch Mountains contain exposures of a tightly folded sequence of Mesozoic and Paleozoic Rocks. Laramide thrust faults and younger normal faults have contributed significantly to the recent topography of the area. Magnetic data apparently show dominantly deep sources, except in the Wasatch/Western Uinta area, where Tertiary intrusive bodies are exposed. The Salt Lake City quadrangle has apparently been relatively unproductive in terms of uranium mining. No claims were found by examination of known literature sources. A total of 199 anomalies are valid according to the criteria set forth in Volume I. The anomalies are scattered throughout the quadrangle. Other than a single anomaly of 46.8 ppM eU over an old AEC dump, none have peak count rates over 7.1 ppM eU