All geologic conditions in the Dillon Quadrangle (Montana and Idaho) have been thoroughly examined, and, using National Uranium Resource Evaluation criteria, environments are favorable for uranium deposits along fractured zones of Precambrian Y metasediments, in the McGowan Creek Formation, and in some Tertiary sedimentary basins.A 9-m-wide quartz-bearing fractured zone in Precambrian Y quartzites near Gibbonsville contains 175 ppm uranium, probably derived from formerly overlying Challis Volcanics by supergene processes.The Mississippian McGowan Creek Formation consists of uraniferous, black, siliceous mudstone and chert. In the Melrose district it has been fractured by a low-angle fault, and uranium has been further concentrated by circulating ground water in the 2-to 6-m-thick brecciated zones that in outcrop contain 90 to 170 ppm uranium.The Wise River, northern Divide Creek, Jefferson River, Salmon River, Horse Prairie, Beaverhead River, and upper Ruby River Basins are considered favorable for uranium deposits in sandstone. Present are suitable uraniferous source rocks such as the Boulder batholith, rhyolitic flow breccia, laharic deposits, or strongly welded tuffs; permeable sediments, including most sandstones and conglomerates, providing they do not contain devitrified glass; suitable reductants such as lignite, pyrite, or low-Eh geothermal water; and uranium occurrences. 9 probably flowed out into the Horse Prairie, Grasshopper Creek, Jefferson River, and upper Ruby River Tertiary basins. Plutonic Rocks. Four major Laramide batholiths crop out within the Dillon Quadrangle. They are the Boulder batholith, the Idaho batholith, the Pioneer batholith, and the Tobacco Root batholith. All are dominantly quartz monzonitic composition and hypidiomorphic-granular texture. Minor Tertiary intrusions are present, mainly in Idaho.The southern part of the Boulder batholith lies within the quadrangle and consists mainly of quartz monzonite, but also contains gabbro, quartz diorite, granodiorite, granite, and the late-stage differentiates, alaskite, aplite, and pegmatite. The batholith dates 78 to 72 m.y., overlapping the age of the Elkhorn Mountain Volcanics (Robinson and others, 1968). The batholith intrudes pre-Belt gneisses, Belt Supergroup metasediments, Paleozoic-Mesozoic sediments, and Elkhorn Mountain Volcanics. Two radically different models have been proposed for the emplacement of the batholith.