Pierre shale.

The Raton basin in New Mexico contains up to 4700 ft of marine shale and subordinate sandstone, limestone, coal, and terrestrial shale of Cretaceous age. However, brittle carbonate- and silica-rich interbeds in the shale intervals are capable, under the proper conditions, of providing highly productive fracture reservoirs containing …

Pierre shale. Things To Know About Pierre shale.

Conformably overlies Pierre shale (Upper Cretaceous); unconformably? underlies Laramie formation (Upper Cretaceous). Outcrops as northerly striking very narrow band from southern to northern borders of quad. In northern part of quad unit is composed entirely of sandstone, about 60 ft thick; near Golden it is composed of 8 ft of sandstone at ...Divided into a lower 2,300 ft thick shale sequence that has a few lenticular sandstones, the Cow Creek member (460 ft thick), shale (350 ft thick), and Espy tongue (250 ft thick). ... Is equivalent to the Gammon Ferruginous and Mitten Members of Pierre Shale on east side of basin. The Ardmore extends eastward where it is assigned as a bed at or ...Siliceous Pierre: shale ; Mineralogical composition. Dominant clay mineral assemblage of ferruginous, siliceous and aluminous minerals ; Maximum dimensions of the ...Dark-gray shale; marine offshore sediment; as thick as 700 metres (2,300 feet). State: North Dakota: Name: Pierre Formation: Geologic age: Upper Cretaceous: Lithologic constituents: Major Sedimentary > Clastic > Mudstone > Shale (Bed) marine offshore sediment. References: NGMDB product:

We were investigating a report of a mosasaur eroding out of the Weskan member of the Pierre Shale, immediately above the much better known Sharon Springs member. Hardly any people work on collecting fossils out of the Weskan, so we were excited for this opportunity in virtually unexplored country. The critter, RMDRC 14-015, got the …A polycotylid about 3m in length. also present in the Pierre Shale Formation: Brimosaurus: B. grandis: Kansas: Fort Hays Limestone: A nomen dubium. Styxosaurus: S. snowii: Smoky Hill Chalk: 85-81.5 Ma ago: A large elasmosaurid about 12m in length, also present in the Pierre Shale Formation Elasmosaurus "E." sternbergi

Paleontology Educational Resources Cooperstown Pierre Shale Site Cooperstown Pierre Shale Site Mosasaurs, Sharks, and Other Marine Creatures from the Cooperstown Pierre Shale Site by John W. Hoganson, Michael Hanson, Dennis L. Halvorson, and Verla Halvorson Figure 1 - Mike Hanson and Dennis Halvorson at the Cooperstown Site.Mosasaurs, Sharks, and Other marine Creatures from the Cooperstown Pierre Shale Site Hoganson, J.W. , 2005. Skeleton of the Oligocene (30 million-year-old) horse, Mesohippus , is a featured exhibit at the new ND Cowboy Hall of Fame in Medora.

A wavelet at a given distance away from a source is visibly smoother and of longer duration than is a wavelet closer to the source. For example, in the Pierre Shale in Colorado, a tenfold loss of amplitude occurs between 10 Hz and 70 Hz, and frequencies above 100 Hz are lost substantially. Many rocks are less attenuating than the Pierre Shale.The Pierre shale sample was extracted from blocks obtained from a Colorado quarry (Cerasi et al., 2017), and further cored to make cylindrical plugs from which fragments were detached and stored in air at room temperature. The sample was glued onto a pin and mounted on a goniometer head with its bedding-plane normal essentially co-aligned with ...Upper Cretaceous Mowry Shale. Bentonite includes any natural material dominantly com-posed of clay minerals in the smectite group. Swelling bentonite contains a high concentration of sodium ions and will substan-tially increase in volume when it is wetted with water. The bentonite in Wyoming likely originated from intense,Numerical modeling of a long-term in situ chemical osmosis experiment in the Pierre Shale, South Dakota. AM Garavito, H Kooi, CE Neuzil. Advances in Water Resources 29 (3), 481-492, 2006. 63: 2006: The system can't perform the operation now. Try again later. Articles 1-20. Show more.The Pierre Shale is a geologic formation or series in the Upper Cretaceous which occurs east of the Rocky Mountains in the Great Plains, from Pembina Valley in Canada [2] to New Mexico . The Pierre Shale was described by Meek and Hayden in 1862 in the Proceedings of the Academy of Sciences (Philadelphia).

Mancos and Pierre Shale. As the sea level rose, it flooded most of the state, depositing the Mancos Shale in the west and the Pierre Shale in central and eastern Colorado. These layers have produced an incredible menagerie of fossils, including coiled, squid-like ammonites, oysters, snails, rare and delicate pterosaur bones, enormous teeth …

The marine Pierre shale, of Late Cretaceous age, on the northern and western flanks of the Black Hills, consists of dark gray shale with some sandy shale and sandstone, and many beds of bentonite. It ranges in thickness from 2,000 to 2,700 feet.

Strong velocity dispersion occurred in the range from 10 kHz to 1 MHz for Pierre shale, and 1 kHz to 1 MHz for Mancos shale. However, for both shales, resonance measurements were representative ...Shale is a sedimentary rock while slate is a metamorphic rock formed from shale. Slate is much more durable than shale due to the metamorphic process it undergoes. Slate and shale are similar in appearance. Visually, it can be hard to tell ...Lithological and paleontological studies of outcrops of Upper Cretaceous formations were conducted at 12 localities in eastern Wyoming, central Colorado, and northeastern New Mexico. The sequence extends upward from the top of the Mowry Shale, or age-equivalent rocks, through the Graneros Shale, Greenhorn Limestone, Carlile Shale, Niobrara Formation, Pierre Shale, and Fox Hills Sandstone, or age-ePaleontology Educational Resources Cooperstown Pierre Shale Site Cooperstown Pierre Shale Site Mosasaurs, Sharks, and Other Marine Creatures from the Cooperstown Pierre Shale Site by John W. Hoganson, Michael Hanson, Dennis L. Halvorson, and Verla Halvorson Figure 1 - Mike Hanson and Dennis Halvorson at the Cooperstown Site.Pierre Robin sequence (or syndrome) is a condition in which an infant has a smaller than normal lower jaw, a tongue that falls back in the throat, and difficulty breathing. It is present at birth. Pierre Robin sequence (or syndrome) is a co...Carpenter, K. (2008). Vertebrate biostratigraphy of the Smoky Hill Chalk (Niobrara Formation) and the Sharon Springs Member (Pierre Shale). In High-Resolution Approaches in Stratigraphic Paleontology (pp. 421-437). Springer Netherlands. Eaton, G. F. (1910). Osteology of Pteranodon. Connecticut Academy of Arts and Sciences, Memoirs.A left side view of the skull of a large Mosasaurus missouriensis in the KU Museum of Natural History. In this section, I have placed pictures of some of the remaining genera of mosasaurs. Mosasaurus occurs later in the deposition of the Pierre Shale (early Campanian time). It was a very large mosasaur, reaching lengths of greater than 12 meters.

The Pierre Shale is a dark gray clayey to silty mudstone that is exposed in large parts of the Northern Great Plains (Gill and Cobban 1966).It is time equivalent to the Bearpaw Shale in northern and western Montana, Alberta, Saskatchewan, and possibly Manitoba (depending on reference, e.g., Bamburak and Nicolas 2009).It is Campanian to Maastrichtian in age.This paper describes the cranial morphology of two undescribed specimens of the polycotylid plesiosaur Dolichorhynchops bonneri from the Pierre Shale of South Dakota. Based on the axial osteology of the juvenile specimen (UNSM 55810), it was most likely a neonate at the time of death. The juvenile material exhibits well-defined suture lines in its …ABSTRACT: Everhart, M. J. and J. Bussen. 2001.First report of the mosasaur, Plioplatecarpus cf. primaevus, from the Pierre Shale (Campanian) of western Kansas.Kansas Academy of Science, Transactions 20(Abstracts): 28-29. The fragmentary skull, vertebrae, and ribs of a plioplatecarpine mosasaur were collected from the Pierre Shale in Logan County, KS, in 1995. Stratigraphically, the remains ...The 1-3-m-thick Crow Creek Member is a unique marlstone with rip-up clasts and a basal coarse layer in the Upper Cretaceous Pierre Shale in South Dakota and Nebraska. Although the Member has been thought to represent a marine transgression along the eastern margin of the Western Interior Seaway, the presence of impact ejecta from the Manson ...Although the isolated, round teeth had been found in many marine deposits around the world, the first Globidens to be described (G. alabamaensis, Gilmore, 1912) was found in the Mooreville Chalk of Alabama.Another species, Globidens dakotensis (Russell, 1975), was discovered in the Pierre Shale of South Dakota. A third, and very complete Globidens skeleton (including stomach contents) was ...The most diverse assemblage of fossils ever found in the Pierre Shale in North Dakota is located in Griggs County about 8 miles southeast of Cooperstown. The most well-known is the mosasaur that was found on this site and now resides in the North Dakota Heritage Center in Bismarck. There are more links to additional information on the ...The Pierre shale formation is a subdivisio of thne Montana group and is Upper-Cretaceous in age. The Pierre shale has 4 . been subdivided into various members. With few exceptions the members of the Pierre shale, with respect to geographic location, are as follows: KANSAS SOUTH WYOMING NORTH COLORADO DAKOTA DAKOTA (Pueblo area)

The Pierre Shale was originally named by Meek and Hayden (1861) based on outcrops along the Missouri River near Fort Pierre, South Dakota. The unit cov-ers much of South Dakota west of the Missouri River, excluding the Badlands, the Black Hills, and northwestern South Dakota (Gries and Martin, 1985). A reference section for the Pierre Shale in ...

Many deflation basins have formed on the Pierre Shale surface to the east of the Colorado Front Range from Denver to Fort Collins. Other pans occur in association with Late Pleistocene desiccation of large pluvial lakes, which was accompanied by deflation in many regions. This led to the migration of dune fields into areas adjacent to the ...The aquifer overlies relatively impermeable claystones of the White River Group, the Cretaceous Pierre Shale, or the shaly chalk and limestone of the Cretaceous Niobrara Formation. The base of the aquifer and the water table generally slope west to east and saturated thickness varies from 0 to greater than 160 m (Fig. 5 ).The Sharon Springs member of the Pierre shale of Cretaceous age, a hard black organic-rich shale similar to the Chattanooga shale, is radioactive throughout central and western South Dakota, most of Nebraska, northern Kansas, and northeastern Colorado. In the Missouri River valley, thin beds of the shale contain as much as 0.01 percent uranium.Assigned as a member of Pierre Shale in eastern ND in Williston basin. No type locality designated. Named Odanah Beds in Manitoba and treated as a member of Riding Mountain Formation. In Pembina Mountain area of northeastern ND, the soft DeGrey Member of Pierre is overlain conformably by hard, light-gray siliceous shale that contains ...The accuracy of the numerical solution is verified against an analytical solution in a homogeneous medium. An example shows that the proposed wave equation describes the constant-Q attenuation and velocity dispersion behaviour observed in Pierre Shale. Finally, we consider a plane-layer model and the Marmousi model to show how the new ...Mowry Shale. According to Keefer and Johnson (1997), the Mowry Shale in the Wind River Basin is characterized by two distinct units (fig. 5). The lower part consists of 50 to 150 ft of soft fissile clay-rich shale that has been referred to as the Shell Creek Shale in the adjacent Bighorn and Powder River Basins (Eicher, 1962;Se-rich soils in eastern Montana, western North Dakota, much of South Dakota, Wyoming, Colorado, and Utah, are underlain by a mixture of rock types, but shale is abundant in these areas. Particularly high concentrations of Se occur in soils overlying the Northern Rolling Pierre Shale Plains (USDA, 2006) in central South Dakota.

Report (volume). of the Pierre Area South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 307 Geology of the Pierre Area South...South Dakota By DWIGHT R.

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FIGURE 34. Hoploscaphites criptonodosus (Riccardi, 1983), macroconch. A–D. USNM 713617, USGS loc. 12757, Baculites grandis Zone, Pierre Shale, Weston County ...All of the specimens in this study originate from the Pierre Shale (Campanian-Maastrichtian; Bamburak and Nicolas, 2009).The formation is approximately 340 m thick and is subdivided into five members: Gammon Ferruginous, Pembina, Millwood, Odanah, and Coulter members (Bamburak and Nicolas, 2010).The vertebrate fossils, including the hesperornithiforms in this study, came from the first three ...And, finally, Tylosaurus neumilleri and Tylosaurus pembinensis were described from the middle Campanian of the Pierre Shale of South Dakota and Manitoba, respectively (Nicholls 1988;Martin 2007 ...Archelon is an extinct marine turtle from the Late Cretaceous, and is the largest sea turtle ever to have been documented, with the biggest specimen measuring 460 cm (15 ft) from head to tail, 400 cm (13 ft) from flipper to flipper, and 2,200 kg (4,900 lb) in weight. It is known only from the Dakota Pierre Shale and has one species, A. ischyros.The Pierre Shale is a geologic formation or series in the Upper Cretaceous which occurs east of the Rocky Mountains from North Dakota to New Mexico. The Pierre Shale was described by Meek and Hayden in 1862 in the Proceedings of the Academy of Sciences (Philadelphia). They described it as a dark-gray shale, fossiliferous, with veins and seams of gypsum, and concretions of iron oxide. The ...Archelon (from Greek αρχελών meaning ruler turtle) is a genus of extinct sea turtle, the largest that has ever been documented, and the second largest chelonian after Stupendemys. The first specimen of Archelon (YPM 3000) was collected from the Pierre Shale of South Dakota by Dr. G.R. Wieland in 1895 and described by him the following year (Wieland, 1896). The largest Archelon fossil ...Studies of laboratory-treated Na +-smectite and Pierre Shale and natural thermo-mature gas shale indicate that, large quantities of silica are released during clay mineral transformation to form quartz cement (within a closed shale system).Two types of quartz cement are recorded in lab treated samples; granular silica, formed with all lab treated samples (Na +-smectite and Pierre Shale) at ...The contact of the Niobrara Formation and Sharon Springs Member of the Pierre Shale is geochemically defined by a synchronous decrease in Si, K, Al, Ti, Zr, Cr, and Nb and increase in Sr and Ca concentrations in the Smoky Hill Member. Elemental changes at formation boundaries can be attributed to differing mineralogical composition across the ...Cold methane seep deposits in the Pierre Shale of South Dakota and Wyoming. Photos by S.M. Klofak and M.P. Garb. A) View of seep deposits in the background, AMNH loc. 3494, Baculites scotti -Didymoceras nebrascense zones, Pierre Shale, Weston County, Wyoming. The seep deposits appear as small mounds called "Tepee Buttes".3. Orientation of the Pierre Shale along the Front Range -Beds have a nearly vertical alignment where uplifted along the Front Range. -This creates a 1.5-3.2 km wide band along the Front Range. -A dip angle of 30° or greater leads to the particular case of heaving bedrock Many beds intersect the ground surface each with different swell potentials.—Chevron Corporation's CFO Pierre Breber said in a statement ... Finance - Chevron Chevron announces buy of Hess for $53 billion in new oil megadeal days after Exxon …

Is the upper member of Niobrara Formation above Fort Hays Limestone Member of Niobrara and beneath Pierre Shale. Divided in the Pueblo area, Pueblo Co, CO in Denver basin, into 7 units described in ascending order: 1) shale and limestone unit is a 20 ft thick gray calcareous shale separated into 18 layers by gray shaly limestone, has INOCERAMUS DEFORMIS, is of early and middle Coniacian age; 2 ...Pierre Shale--Upper unit. Ogallala Fm (Tertiary) at surface, covers 24 % of this area. Loose to well-cemented sand and gravel. Older gravels and alluviums (Quaternary) at surface, covers 10 % of this area. Includes Slocum, Verdos, Rocky Flats, and Nussbaum Alluviums in east, and Florida, Bridgetimber, and Bayfield Gravels in southwest.The Pierre shale sample was extracted from blocks obtained from a Colorado quarry (Cerasi et al., 2017), and further cored to make cylindrical plugs from which fragments were detached and stored in air at room temperature. The sample was glued onto a pin and mounted on a goniometer head with its bedding-plane normal essentially co-aligned with ...Instagram:https://instagram. greenbush commuter rail stationt by talbots jacketsautozonepartsku v texas Four case histories where important changes in pile capacity were observed with time are presented. Two show an increase of pile capacity for shaft bearing piles driven into deep sand deposits. The increase occurred over a period longer than needed for pore pressure dissipation. In one case, increases of 33 and 85% in pile capacity were measured 2 and …Dark-gray shale; marine offshore sediment; as thick as 700 metres (2,300 feet). State: North Dakota: Name: Pierre Formation: Geologic age: Upper Cretaceous: Lithologic constituents: Major Sedimentary > Clastic > Mudstone > Shale (Bed) marine offshore sediment. References: NGMDB product: hillel kubyu game channel tonight This is the Pierre Shale, which underlies much of the city of Colorado Springs and troubles engineering geologists with its expanding and contracting clay, which can crack foundations and heave roads. Two additional Cretaceous layers are on display along Popes Bluffs in Ute Valley Park. The Fox Hills Sandstone consists of beach sand resembling ...Claystone samples of the Denver and Pierre Shale Formations obtained near Denver, Colorado, USA were used in the study. A moist tamping system was used to obtain "identical" soil specimens. wyatt spirit golf Archelon (from Greek αρχελών meaning ruler turtle) is a genus of extinct sea turtle, the largest that has ever been documented, and the second largest chelonian after Stupendemys. The first specimen of Archelon (YPM 3000) was collected from the Pierre Shale of South Dakota by Dr. G.R. Wieland in 1895 and described by him the following year (Wieland, 1896). The largest Archelon fossil ...The lower Pierre Shale and the Niobrara Formation of the Powder River basin are examples of the “wide-shelf” configuration, in which subsidence is relatively slow, progradation is rapid, and sand is largely confined to the shelf. The regressive Lewis Shale of the Washakie and Red Desert basins illustrates the complex relations between a ...Ammonite Fossils - Collected from Wyoming and Montana region. This pair of polished ammonites was found in the Pierre Shale region, a geologic formation dating to the Late Cretaceous epoch (approximately 100 to 66 million years ago) which occurs east of the Rocky Mountains in the Great Plains states. Ammonites are a type of extinct marine ...