1:24,000 Geologic Maps
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Vendor: Utah Geological SurveyBy: J. M. Hayden and E. G. SableThis color map covers the Virgin quadrangle. Information in this publication includes: a description of geologic units, a correlation of geologic units, a lithologic column, and two cross-sections.Other Information: Published: 2008Plates: 2 pl.Scale: 1:24,000Location: Washington CountyMedia Type:...
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Vendor: Utah Geological SurveyBy: T. J. Felger, D. L. Clark, and M. D. Hylland The Skinner Peaks quadrangle is located along the Basin and Range ? Colorado Plateau transition in central Utah. Key aspects of the quadrangle includes its location along the Levan segment of the active...
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Vendor: Utah Geological SurveyBy: J. M. Hayden The Washington Dome quadrangle in southwest Utah is in the transition zone between the Basin and Range Province to the west and the Colorado Plateau to the east. The quadrangle straddles two structural blocks separated by the Washington normal fault,...
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Vendor: Utah Geological SurveyBy: D. W. Moore, L. D. Nealey, P. D. Rowley, S. C. Hatfield, D. J. Maxwell, E. Mitchell This map is intended to update the preliminary geologic map of the same area, at the same scale. Updating required new fieldwork by P.D. Rowley and...
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Vendor: Utah Geological SurveyBy: M. P. Weiss and D. A. Sprinkel The Manti quadrangle lies in a region of structural transition between the extended lithosphere of the Basin and Range Province and the moderately deformed Colorado Plateau. In Late Cretaceous time this region was the leading edge...
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Vendor: Utah Geological SurveyBy: M. P. Weiss, J. G. McDermott, D. A. Sprinkel, R. L. Banks, and R. F. Biek The Chriss Canyon quadrangle lies in a region of structural transition between the extended lithosphere of the Basin and Range Province and the moderately deformed Colorado Plateau....
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Vendor: Utah Geological SurveyBy: H. H. Doelling and M. L. Ross The Big Bend quadrangle is named for a deeply incised meander bend in the Colorado River in southern Grand County, Utah. It is part of Utah's scenic Red-Rock country and includes the world-famous Delicate Arch and...
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Vendor: Utah Geological SurveyBy: H. H. Doelling The Dewey quadrangle is located on the northeast edge of the salt anticline region of the Paradox basin in east-central Utah. Exposed consolidated formations range in age from Permian to Cretaceous. In ascending order, these units include the Permian Cutler...
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Vendor: Utah Geological SurveyBy: G. C. Willis, H. H. Doelling, and M. L. Ross The Agate 7.5' quadrangle is located on the northwestern flank of the Uncompahgre Plateau and the southeastern edge of the Uinta Basin in eastern Utah. Proterozoic gneiss, amphibolite, and granitoids are exposed near...
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Vendor: Utah Geological SurveyBy: D. Sack The Swasey Peak NW quadrangle is located in east-central Tule Valley, about 45 miles west of Delta, Utah. It covers portions of the Tule Valley basin floor, the adjacent piedmonts of both the House Range and the Coyote Knolls, and a...
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Vendor: Utah Geological SurveyBy: D. Sack The Coyote Knolls quadrangle is located in west -central Tule Valley, about 50 miles west of Delta, Utah. It covers portions of the Tule Valley basin floor, the adjacent piedmonts of the Coyote Knolls and Confusion Range, and most of the...
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Vendor: Utah Geological SurveyBy: D. M. Miller and A. P. Lush The Pilot Peak quadrangle straddles the Utah-Nevada border in northwestern Utah and northeastern Nevada, and includes much of the highest part of the central Pilot Range. Flanking the range are piedmonts; on the west side is...
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Vendor: Utah Geological SurveyBy: G. C. Willis The Harley Dome quadrangle is located on the southern flank of the Uinta Basin in eastern Utah. The oldest exposed formation is the Cretaceous Aptian to Albian Cedar Mountain Formation. It is overlain by the Cenomanian Dakota Sandstone, which is...
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Vendor: Utah Geological SurveyBy: M. E. Jensen The Bear River City 7.5-minute quadrangle is located in northern Utah on the eastern margin of the Great Basin. Most of the quadrangle is covered by unconsolidated lacustrine and alluvial deposits that are Quaternary in age. Bedrock is only exposed...
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Vendor: Utah Geological SurveyBy: G. C. Willis The Redmond Canyon quadrangle is in the transition zone between the Colorado Plateau and the Basin and Range physiographic provinces, and includes parts of the Valley Mountains and the adjacent Sevier Valley. Small knolls, known locally as the Redmond Hills...
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Vendor: Utah Geological SurveyBy: W. L. Auby The Levan quadrangle is located along the northwestern part of the Gunnison Plateau. Rocks mapped range from Jurassic marine sediments to Quaternary surficial deposits. The Jurassic Arapien Shale is the most extensive unit mapped and, despite its name, is composed...
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Vendor: Utah Geological SurveyBy: D. L. Clark The quadrangle area lies along the eastern margin of the Basin and Range physiographic province and encompasses portions of the West Hills, and Juab and Sage Valleys. In the quadrangle, the West Hills consist of three distinct physiographic segments: 1)...
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Vendor: Utah Geological SurveyBy: D. M. Miller The Lucin 4 NW 7.5-minute quadrangle lies in northwestern Utah and includes part of the northern Silver Island Mountains and the adjacent Great Salt Lake Desert. A thick sequence of miogeoclinal Paleozoic rocks, ranging from Cambrian to Permian in age,...
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Vendor: Utah Geological SurveyBy: G. W. Weir and L. S. Beard The Tenmile Flat quadrangle, south-central Garfield County, lies in the Kaiparowits Plateau-Teasdale anticline section of the Colorado Plateau physiographic province. Mesas in the southwest corner of the quadrangle are spurs from the Kaiparowits Plateau. Extensive flats...
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Vendor: Utah Geological SurveyBy: G. W. Weir and L. S. Beard The Red Breaks quadrangle, south-central Garfield County, lies in the Circle Cliffs-Teasdale section of the Colorado Plateau physiographic province. A chief feature of the quadrangle is a large dissected mesa, Red Breaks, in the southwestern part...
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