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Wildcatite, CaFe 3+ Te 6+ O 5 (OH), the second new tellurate mineral from the Detroit district, Juab County, Utah
Exomorphism of jacobsite precipitates in bixbyite single crystals from the Thomas Range in Utah
Adanite, a new lead-tellurite-sulfate mineral from the North Star mine, Tintic, Utah, and Tombstone, Arizona, USA
Andymcdonaldite (Fe 3+ 2 Te 6+ O 6 ), a new ferric iron tellurate with inverse trirutile structure from the Detroit district, Juab County, Utah
Origin of the fluorine- and beryllium-rich rhyolites of the Spor Mountain Formation, Western Utah
Dagenaisite, A New Zinc Tellurate From the Gold Chain Mine, Tintic, Utah, U.S.A.
Uranium-bearing opals: Products of U-mobilization, diffusion, and transformation processes
New Mineral Names
Crustal structure and signatures of recent tectonism as influenced by ancient terranes in the western United States
REEF RECOVERY FOLLOWING THE FRASNIAN–FAMENNIAN (LATE DEVONIAN) MASS EXTINCTION: EVIDENCE FROM THE DUGWAY RANGE, WEST-CENTRAL UTAH
New mineral names
THE OD (ORDER–DISORDER) STRUCTURE OF HOLFERTITE, A HYDRATED URANYL TITANATE MINERAL FROM SEARLE CANYON, THOMAS RANGE, UTAH, USA
Identification of mixite minerals — an SEM and Raman spectroscopic analysis
Abstract Donald R. Currey spent over two decades researching and exploring relics of ancient Lake Bonneville in the eastern Great Basin. Shoreline and deepwater deposits of Lake Bonneville document coastal processes, lake chemistry, and environmental change during the late Pleistocene and Holocene. This field guide summarizes findings at many of the classic localities researched by Currey and colleagues that contributed to the current understanding of this impressive pluvial lake and its interglacial successor, Great Salt Lake. Subjects include coastal processes at Antelope Island and the Stockton Bar; lake history, chemistry and environmental change at Stansbury Island, the Public Shooting Grounds and Hansel Valley; deltaic depositional processes at Big Cottonwood Canyon, American Fork Canyon and Brigham City; and the relative chronology of glacial and lacustrine deposition at Little Cottonwood Canyon and Bells Canyon.