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Medicine Bow Peak

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Journal Article
Published: 01 April 1962
Rocky Mountain Geology (1962) 1 (1): 48.
Journal Article
Published: 01 April 1962
Rocky Mountain Geology (1962) 1 (1): 21–29.
... and are characterized by pronounced "knob-and-kettle" topography and tills rich in crystalline constituents. More recent deposits at the base of Medicine Bow Peak, W. of the source of Libby Creek, have been considered by some workers as recent moraines, but are more likely protalus ramparts overlying latest Pinedale...
Journal Article
Published: 01 January 1998
Rocky Mountain Geology (1998) 33 (2): 259–277.
... Madre, MB = Medicine Bow Mountains, LM = Laramie Mountains, RH = Richeau Hills, LPSZ = Laramie Peak shear zone † z = zircon, s = sphene, a = apatite, b = baddeleyite, h = hornblende § (1) Premo and Van Schmus, 1989 ; (2) Snyder et al., 1995 ; (3) Cox et al., 1995 ; (4) Loucks et al., 1988...
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Journal Article
Published: 01 September 1926
American Mineralogist (1926) 11 (9): 239–246.
...Arthur L. Crawford Abstract The purpose of this article is to place on record an American occurrence of oligoclase crystals of pendine 1 habit, an unusually rare form of a common mineral. They occur at Gold Hill, Wyoming, on the west flank of Medicine Bow Mountains or Snowy Range, about three miles...
Journal Article
Published: 01 January 2000
Rocky Mountain Geology (2000) 35 (1): 71–90.
... the Archean Wyoming province and Proterozoic Colorado province. The time of emplacement of the Horse Creek anorthosite complex coincides with late stages of the Medicine Bow orogeny, in which Proterozoic island arcs collided with the Wyoming province. The Horse Creek anorthosite complex was emplaced in a zone...
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Journal Article
Published: 01 January 2011
Rocky Mountain Geology (2011) 46 (2): 111–135.
... in the Medicine Bow Mountains of southeastern Wyoming. These shear zones are generally interpreted as a mid-crustal thrust system rotated to its present-day subvertical orientation during late-stage, orogen-scale folding. However, the map geometry, presence of large domains of S tectonites, and vertical mineral...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.245.01.05
EISBN: 9781862394933
... of these features. Abstract The Laramie Peak shear system (LPSS) is a 10 km-thick zone of heterogeneous general shear (non-coaxial) that records significant tectonic regeneration of middle-lower crustal rocks of the Archean Wyoming province. The shear system is related to the 1.78–1.74 Ga Medicine Bow...
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Journal Article
Published: 01 March 1989
Bulletin of Canadian Petroleum Geology (1989) 37 (1): 98–112.
...Rory C. Hankel; Graham R. Davies; H. Roy Krouse ABSTRACT The Upper Cretaceous (Santonian) Medicine Hat Formation in the eastern section of the Medicine Hat Field of southeastern Alberta overlies the Colorado Shale and is overlain by the First White Specks Shale. In the project area, the Medicine...
Journal Article
Published: 01 January 2000
Rocky Mountain Geology (2000) 35 (2): 163–204.
... occurs in the Hanna Basin in carbonaceous to lignitic strata, representing fluvial and paludal episodes bounded by incursions of epicontinental seas. Amber occurs, in decreasing age, in the Upper Cretaceous Allen Ridge, Medicine Bow, and Ferris formations (parts of the last straddle the Cretaceous...
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Journal Article
Published: 01 September 1997
Bulletin of Canadian Petroleum Geology (1997) 45 (3): 356–376.
... producing and non producing zones (Plates 1 and 2). Pore throat size distribution curves generally have broad peaks (or poor pore throat sorting) which coincide with the different pore types identified in these fine grained sediments. Mean pore throat radius (R50) was measured at 0.10 pm for the Medicine...
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1989
AAPG Bulletin (1989) 73 (11): 1361–1382.
...James M. Wood; John C. Hopkins ABSTRACT Over 50% of the established oil reserves (1.325 million m 3 ) of the Little Bow field in southern Alberta are stratigraphically trapped within upper Mannville G, U, and W pools. These pools are hosted by three parallel, elongate sandstone bodies within...
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Journal Article
Published: 01 January 2014
Rocky Mountain Geology (2014) 49 (1): 61–74.
... with the potential for inflow over a low ridge physically separating the lake from the nearby Medicine Bow River. No outflow channel is present. The basal age of the lake is ∼6000 cal yr BP ( Brunelle et al., 2013 ). Precipitation is low (∼25 cm/yr), but evenly distributed through the year, with a slight peak in May...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1965
AAPG Bulletin (1965) 49 (4): 379–417.
... the Telegraph Creek, Virgelle, Two Medicine, Bearpaw, Horsethief, St. Mary River, and Willow Creek Formations, aggregating about 5,000 feet in thickness. The basal formations of the Montana Group, the Telegraph Creek and Virgelle, are regressive shallow-marine and lagoonal feldspathic sandstones and shales...
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