2 edition of Lithology of the Sundance formation, Dubois area, Fremont County, Wyoming found in the catalog.
Lithology of the Sundance formation, Dubois area, Fremont County, Wyoming
James Albert Knupke
Written in English
|Statement||by James A. Knupke|
|The Physical Object|
|Pagination||41 leaves :|
|Number of Pages||41|
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Only Bold Mountain that USGS knows about it in Fremont County,WY at N,W. CAUTION:Collecting vertebrate material in the US requires landowner or. Riverton, Lander, Dubois, and Shoshoni are the primary towns in Fremont County.
Worland is the major community in Washakie County. Regionally, the planning area lies within the Missouri River drainage system and covers an area of approximat square miles of federal, state, and privately owned land in central and northwestern Wyoming.
The Morrison Formation is a distinctive sequence of Upper Jurassic sedimentary rock found in the western United States which has been the most fertile source of dinosaur fossils in North is composed of mudstone, sandstone, siltstone, and limestone and is light gray, greenish gray, or red.
Most of the fossils occur in the green siltstone beds and lower sandstones, relics of the Country: United States. Water is arguably the state’s most valuable resource because water is the main constituent of all organic life. It accounts for percent by weight of living g is located over the continental divide and therefore is the headwaters region for four major river basins in the west: 1) Missouri-Mississippi, 2) Green-Colorado, 3) Snake-Columbia, and 4) Great Salt Lake.
Formation. The lithology at the site consists of a of Megalneusaurus rex was relocated in the Gas Hills area of eastern Fremont County, WY and plesiosaurs of the Sundance Formation of. Geology and ground-water resources of the Rawlins area, Carbon County, Wyoming USGS Publications Warehouse.
Berry, Delmar W. The Rawlins area in west-central Carbon County, south-central Wyoming includes approximately square miles of plains and valleys grading into relatively rugged uplifts. The climate is characterized by low precipitation, rapid evaporation, and.
Chugwater Formation or Group (Lower Triassic-Upper Triassic) at surface, covers area. Chugwater Formation (North Dubois area Northeast Wyoming) - Red siltstone and shale. Alcova Limestone Member in upper middle part in north Wyoming. Thin gypsum partings near base in north and northeast Wyoming.
Given that the Rock Point Member is thickest in the southern Four Corners region and that the Chinle Formation is beveled to successively older units to the west by the J-0 unconformity, it seems likely that the Rock Point 32 A WYOMING: COLOR, DO AI SOUTH'CENTRAL WYOMING I F,~ONT RANGE SUNDANCE FORMATION " Jurossic Rocks 60 0 I0 In central Wyoming, the unconformity at the base of the Sundance cuts out successively older strata in the Gypsum Spring Formation from west to east (Love, Tourtelot, and others, ).
The "Upper Sundance" is The unconformity at the base of the Sundance For- of Late Jurassic age and correlates with the Stump Sandmation has been discussed. This banner text can have markup. web; books; video; audio; software; images; Toggle navigation.
Sundance Formation (1) Nugget Fremont County Wyoming (13) Hot Springs County Wyoming (1) Lincoln County Wyoming Dean DuBois of EnCana Oil and Gas (U.S.A.) Inc. reviewed and revised some of the data.
Mineral Occurrence and Development Report, Lander Field Office Planning Area, April - Free ebook download as PDF File .pdf), Text File .txt) or read book online for free. The Mineral Occurrence and Development Potential Report has been prepared to support the process of amending the Resource Management Plan for the Bureau of Land Management Lander Field Office, Wyoming.
Uranium in the Mayoworth area, Johnson County, Wyoming - a preliminary report. USGS Publications Warehouse. Love, J.D. The uranium mineral, metatyuyamunite, occurs in the basal limestone of the Sundance formation of late Jurassic age along the east flank of the Bighorn Mountains, about 2 miles southwest of the abandoned Mayoworth.
Fremont County Colorado (3) Front Range Albany County Wyoming (1) Laramie Basin (1) Wind River Range (1) Sundance Formation (1) Triassic Upper Triassic Chinle Formation.
12 Gros Ventre Wilderness Study Area, Wyoming (or) anhydrite) is invariably present, most of it in one basal bed ft ( m) thick. The formation is pres ent in broad exposures along the northeastern edge of the study area and in a few small outcrops on the southern and southwestern flanks of the Gros Ventre Range.
Sundance Formation NCUR® Logo Information Appreciation for the La Crosse Area has been present from the days of our earliest inhabitants. When the giant glaciers of the Ice Age retreated north, they left the La Crosse area virtually untouched. In the 17th century, European settlers made their way through the rugged limestone formations and the narrow.
Wyoming is a state in the mountain region of the Western United States. The state is the 10th largest by area, the least populous, and the second most sparsely populated state in the country.
Wyoming is bordered on the north by Montana, on the east by South Dakota and Nebraska, on the south by Colorado, on the southwest by Utah, and on the west by Idaho and Montana.
Andersson, K.A., Early lithification of limestones in the Redwater Shale Member of the Sundance Formation (Jurassic) of southeastern Wyoming. Contributions to Geology, University of Wyoming André, M.
and Lamy, E., Crustacés xylophages et lithophages. Bulletin de l’Institut océanographique de Monaco During my freshman year at the University of Wyoming I met Dr.
(Dave) Love who was later the central figure in John McPhee's book "Rising from the Plains". When I was looking for a summer job Dave hired me as a field assistant for a USGS camp in the Powder River Basin of Wyoming where Dave's expertise and interpretation had discovered.
the Michigan City area, Nelson County, North Dakota: N. Oak. State Water Conserv. The areal extent and lithology of the formation are discussed. The oil and gas potential of the Winnipegosis reefs is mentioned. Clabaugh, S. Fremont F.,Southwestern North Dakota clay.
Sundance Formation Green shale and thin-bedded sand- stone. Gypsum Springs White massive gypsum with some Formation interbedded red shale and siltstone.
Red shale, siltstone and fine. PERMO-TRIASSIC Spearfish Formation grained sandstone; gypsum beds near bottom. PERMIAN. Minnekahta Gray to purple t laminated, coarsely The Oklahoma Geology Camp is located in a gap in the nearer tree-covered hogback in the upper right. The southeast-dipping Dakota Group forms a prominent hogback and overlies the slope-forming Morrison Formation and underlies a thick section of Cretaceous shales and limestones.
This area (Grape Creek) is the students’ first major mapping project.Stratigraphy and paleontology of the Cloverly Formation (Lower Cretaceous) of the Bighorn Basin area, Wyoming and Montana.
Peabody Museum Nat. History Bull. 35, 1– Tumanova, T. ().