1-20 OF 4449 RESULTS FOR

Southwest Wyoming

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1951
AAPG Bulletin (1951) 35 (5): 1106.
...W. W. Rubey Abstract The area of southwest Wyoming covered by the Field Conference lies west of the Rock Springs uplift, southwest of the Wind River range, north of the Uinta Mountains and south of the Gros Ventre range. It is underlain at the eastern edge, the Rock Springs uplift, by shelf...
Journal Article
Published: 01 July 2024
Rocky Mountain Geology (2024) 59 (1): 1–18.
...Steven G. Fryberger ABSTRACT Within the Greater Rocky Mountain Region, ventifacts have not been extensively studied, and little is known about various local relationships between rock type, wind regime, and associated ventifaction styles. The Killpecker Sand Dunes area of southwest Wyoming hosts...
FIGURES | View All (20)
Journal Article
Journal: Interpretation
Published: 23 October 2017
Interpretation (2017) 5 (4): SS43–SS58.
... on a natural carbon dioxide reservoir, the Madison Limestone on the Moxa Arch of Southwest Wyoming, which serves as a natural analog for geologic cosequestration of sulfur dioxide and carbon dioxide. Idealized Madison Limestone ( dolomite + calcite ± anhydrite + pyrite ) and Na - Cl - SO 4 2 − brine ( I = 0.5...
FIGURES | View All (7)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 2015
AAPG Bulletin (2015) 99 (5): 889–925.
...-gas accumulations during the last 35 yr comes from the deep eastern GGRB in southwest Wyoming, the focus of this paper. McPeek ( 1981 ) reported that Upper Cretaceous sandstones within the Lewis Shale and Mesaverde Group are overpressured below a subsurface depth of about −2000 to −5000 ft (−610 m...
FIGURES | View All (25)
Journal Article
Published: 01 January 2010
Rocky Mountain Geology (2010) 45 (2): 113–132.
... comprises the bulk of the subsurface Bighorn in southwest Wyoming. Mottled dolostone (light-colored patches with higher porosity and dark-colored patches with lower porosity) is very common and is presumably the result of preferential early dolomitization of bioturbation. Core study suggests...
FIGURES | View All (11)
Journal Article
Journal: GSA Bulletin
Published: 01 April 1995
GSA Bulletin (1995) 107 (4): 454–462.
...Peter G. DeCelles; Gautam Mitra Abstract Problems with applying critical taper models to ancient orogenic wedges are overcome in the Late Cretaceous–late Paleocene Sevier orogenic wedge in Utah and Wyoming by a symptomatic approach in which wedge behavior is inferred from the time-space...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1994
GSA Bulletin (1994) 106 (1): 32–56.
... faulting in the northeast Utah-southwest Wyoming part of the Sevier thrust belt. These data indicate a general eastward progression of deformation that was punctuated by local out-of-sequence and hinterlandward-verging events. Provenance data delimit a sequential restoration of a regional cross section...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1982
AAPG Bulletin (1982) 66 (10): 1698–1699.
...Henry W. Roehler ABSTRACT The Wilkins Peak Member, the saline unit of the Green River Formation in southwest Wyoming, is more than 985 ft (300 m) thick and contains more than 35 beds of trona or trona with halite. The trona and halite were deposited in the deepest part of the basin of Lake Gosiute...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 593–594.
Journal Article
Published: 01 April 1971
Rocky Mountain Geology (1971) 10 (1): 15–23.
Journal Article
Published: 01 September 1968
Journal of Sedimentary Research (1968) 38 (3): 948–949.
...G. B. Asquith Abstract Large, elongate (up to 3 mm) subhedral to euhedral crystals of kaolinite were discovered in the Upper Cretaceous Almond Formation near Rock Springs, Wyoming. The kaolinite is present as a 1-3 inch thick underclay in the lower, non-marine portion of the Almond Formation...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1942
AAPG Bulletin (1942) 26 (5): 900.
...W. T. Nightingale The development during the past few years of commercial volumes of petroleum and natural gas in the Wasatch formation of northwest Colorado and southwest Wyoming has aroused considerable geological comment. The Wasatch formation is of Eocene age and fluvio-terrestrial in origin...
Series: AAPG Special Publication
Published: 01 January 1935
DOI: 10.1306/SV7335C11
EISBN: 9781629812557
... Abstract The Hiawatha and West Hiawatha gas fields, located in Vermilion Creek basin and on the state line between southwest Wyoming and northwest Colorado, are of commercial importance as the field terminus of the gas pipe-line system supplying Salt Lake City and adjacent towns with natural...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1930
AAPG Bulletin (1930) 14 (8): 1013–1040.
...W. T. NIGHTINGALF ABSTRACT The Vermilion Creek gas area, located on both sides of the state line between southwest Wyoming and northwest Colorado, is now the field terminus of a 330-mile $20,000,000.00 gas line built in 1929 and supplying Salt Lake City, Utah, and adjacent towns with natural gas...
FIGURES | View All (5)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1930
AAPG Bulletin (1930) 14 (8): 1013–1040.
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1952
AAPG Bulletin (1952) 36 (10): 1962–2010.
...Donald Towse ABSTRACT The Upper Cretaceous Frontier formation is a conspicuous sandy unit in the predominantly fine-grained rocks of the Colorado group in Wyoming. The Frontier formation is an important oil-producing formation in Wyoming. The formation was studied in detail in the southwest Powder...
FIGURES | View All (18)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1995
AAPG Bulletin (1995) 79 (9): 1377–1394.
...Philipp C. Molzer; Eric A. Erslev ABSTRACT Understanding the diversity of structural trends in the Laramide foreland of the conterminous United States is important to understanding the location, geometry, and fracturing of hydrocarbon reservoirs. East-west basement-cored arches in central Wyoming...
FIGURES | View All (18)
Journal Article
Journal: GSA Bulletin
Published: 01 October 1938
GSA Bulletin (1938) 49 (10): 1515–1544.
.... The west flank of the syncline has moved relatively east‐ward onto the east flank. Along the thrusts at the surface there are drag blocks younger than either of the two formations in contact along the fault. University of Wyoming, Laramie, Wyo. 11 04 1938 © 1938 Geological Society...
Image
Sand roses for the Southwest Wyoming Regional Airport ~13 km (eight miles) east of Rock Springs—and ~40 km (25 miles) south of the study area at Killpecker dunes (data from Iowa Environmental Mesonet, 2020). A, The month of May 2016 showing strong northeast winds. B, The annual sand rose for the years 2009–2019. Sand roses express the relative power of the wind to move sand using the method of Fryberger and Dean (1979). The numbers in circles are directional groupings around a 360-degree scale based on the original data. The numbers stacked vertically represent vector unit (VU) totals (a comparative estimate of sand-moving wind energy) for each of the 16 compass directions evaluated by the sand roses.
Published: 01 July 2024
Figure 8. Sand roses for the Southwest Wyoming Regional Airport ~13 km (eight miles) east of Rock Springs—and ~40 km (25 miles) south of the study area at Killpecker dunes (data from Iowa Environmental Mesonet, 2020 ). A , The month of May 2016 showing strong northeast winds. B , The annual
Image
Regional tectonic map of northeast Utah and southwest Wyoming shows the approximate traces of the major thrusts in the area related to the Sevier fold and thrust belt and the generalized geologic units exposed in the area (modified from DeCelles, 1994; DeCelles and Cavazza, 1999; Weil et al., 2010). Red box shows area from which field samples were collected for this study.
Published: 16 December 2020
Figure 2. Regional tectonic map of northeast Utah and southwest Wyoming shows the approximate traces of the major thrusts in the area related to the Sevier fold and thrust belt and the generalized geologic units exposed in the area (modified from DeCelles, 1994 ; DeCelles and Cavazza, 1999