
 GEOLEX
Summary of Citation: Montana
Publication:
Eldridge, G.H., 1888, On some stratigraphical and structural
features of the country about Denver, Colorado: Colorado
Scientific Society Proceedings, v. 3, pt. 1, p. 86-118
Usage in Publication: Montana group*
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Overview
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Denver basin
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Summary: Name Montana group will be used for the Fort Pierre and Fox Hills, and the Fox Hills will include both the Fort Pierre and the Fox Hills as Meek and Hayden defined them in a forthcoming in American Journal of Science (footnote on p. 93-94). Called a "member of the Cretaceous."
Summary of Citation: Montana
Publication:
Stebinger, E., 1914, The Montana group of northwestern Montana:
U.S. Geological Survey Professional Paper, 90, p. 62-68
Usage in Publication: Montana group*
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Sweetgrass arch
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Summary: In northwest MT in and near the Blackfoot Indian Reservation, Glacier Co on the Sweetgrass arch, the formations in the Montana group are very different from those on the Missouri and Musselshell Rivers in the central part of the state. A section in valley of Two Medicine River from its mouth in T31N, R5W to a point 3 mi above T31N, R9W studied. Section starts above Colorado shale. Montana group above the Colorado is divided into (ascending): Virgelle sandstone (first used), Two Medicine formation (first used), Bearpaw shale, and Horsethief sandstone (newly assigned to Montana group). Cross section shows relations of the sequence in Two Medicine River valley with units between southern Alberta and the Black Hills. Virgelle is equivalent to the lower Eagle of central MT. Two Medicine tongues into the Claggett and Judith River of central MT. Horsethief is equivalent to Lennep of central MT. Overlain by rocks of continental origin designated "St. Mary River beds of Dawson." Late Cretaceous age inferred.
Summary of Citation: Montana
Publication:
Bowen, C.F., 1915, The stratigraphy of the Montana group, with
special reference to the position and age of the Judith River
formation in north-central Montana: U.S. Geological Survey
Professional Paper, 90, p. 95-153
Usage in Publication: Montana group*
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Revised
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Central Montana uplift
Sweetgrass arch
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Summary: Revised in that the lower massive persistent sandstone member of the Eagle sandstone, basal formation of the Montana group, is named Virgelle sandstone member. Overlies Colorado shale. Underlies Lance formation. Divided into the (ascending): Eagle sandstone, Claggett formation, Judith River formation, and Bearpaw shale. Geologic map of area from Judith on the Missouri River in Fergus Co south to Musselshell in Musselshell Co, MT on the Central Montana uplift. Virgelle member named for locality on the Missouri River, Chouteau Co, MT on the Sweetgrass arch. Late Cretaceous age.
Summary of Citation: Montana
Publication:
Darton, N.H., 1919, Description of the Newell quadrangle, South
Dakota: U.S. Geological Survey Geologic Atlas of the United
States, Newell folio, no. 209, 7 p.
Usage in Publication: Montana group*
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Areal limits
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Williston basin
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Summary: Name extended to Black Hills region, Butte and Meade Cos, SD in Williston basin, to include Pierre shale and overlying Fox Hills sandstone. Underlain by Niobrara formation; overlain by Lance formation. Late Cretaceous in age.
Summary of Citation: Montana
Publication:
Schultz, A.R., 1920, Oil possibilities in and around Baxter
basin, in the Rock Springs uplift, Sweetwater County, Wyoming:
U.S. Geological Survey Bulletin, 702, 107 p.
Usage in Publication: Montana group*
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Revised
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Greater Green River basin
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Summary: Revised in that Montana group divided into (ascending): the Baxter shale (new), Blair formation (new), Mesaverde formation, and Lewis shale in Sweetwater Co, WY in the Greater Green River basin. Ranges from 3,500 to 6,300 ft thick in report area. Geologic map. Stratigraphic charts. Only Blair and Baxter described. Of Late Cretaceous age.
Summary of Citation: Montana
Publication:
Lavington, C.S., 1933, Montana group in eastern Colorado: American
Association of Petroleum Geologists Bulletin, v. 17, no. 4,
p. 397-410
Usage in Publication: Montana group
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Las Vegas-Raton basin
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Summary: Divided into Pierre shale (base) and Fox Hills sandstone (top). Is 4,300 to 6,000+ ft thick. Contact between Pierre and Fox Hills is gradational. Pierre divided into 5 zones (ascending): barren zone, rusty zone, tepee zone, cone-in-cone zone, and transition zone. Cross sections. Barren zone includes a 20 ft thick sandstone called Apache sandstone member (first used); the new member attributed to an unpublished report by H. W. C. Prommel. Report area concerned with Denver and Las Vegas-Raton basins. Of Late Cretaceous age.
Summary of Citation: Montana
Publication:
Viele, G.W. and Harris, F.G., III, 1965, Montana Group stratigraphy,
Lewis and Clark County, Montana: American Association of
Petroleum Geologists Bulletin, v. 49, no. 4, p. 379-417
Usage in Publication: Montana Group
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Revised
Overview
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Montana folded belt province
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Summary: Typically consists of (ascending) Telegraph Creek Formation, Virgelle Sandstone, Two Medicine Formation, Bearpaw Shale, Horsethief Formation, St. Mary River Formation, and Willow Creek Formation; totaling about 5,000 ft in thickness in the Disturbed belt of northern Lewis and Clark Co, MT in Montana folded belt province. Revised along western margin of Disturbed belt in that the Big Skunk Formation (new), comprised of 2,100 ft of volcanic-rich, arkosic sedimentary rock, occupies the upper two-thirds of the Two Medicine stratigraphic interval. Age is Late Cretaceous.
Summary of Citation: Montana
Publication:
Gill, J.R. and Cobban, W.A., 1973, Stratigraphy and geologic
history of Montana Group and equivalent rocks, Montana,
Wyoming, and North and South Dakota: U.S. Geological Survey
Professional Paper, 776, 37 p.
Usage in Publication: Montana Group*
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Montana folded belt province
Central Montana uplift
Williston basin
Powder River basin
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Summary: Revised to include Hell Creek Formation as uppermost unit because of its lithogenetic similarities to underlying Cretaceous units; Miner Creek and St. Mary River Formations, Hell Creek equivalents, are not included within Montana. Telegraph Creek Formation considered basal part of Montana. Study area is within central MT in Lewis and Clark and Meagher Cos (Montana folded belt province), Wheatland, Golden Valley, and Fergus Cos (Central Montana uplift), Garfield Co (Williston basin), and Bighorn Co (Powder River basin). West-east cross section A-A' across central MT from Dearborn River to Porcupine dome (a distance of 300 mi) shows Montana Group to consist of (ascending) Telegraph Creek Formation, Virgelle Sandstone, and Two Medicine Formation, in Dearborn River area; Telegraph Creek, Virgelle Sandstone Member of Eagle Sandstone, main body of Eagle, Judith River Formation, Claggett Shale, Parkman Sandstone, Bearpaw Shale, Horsethief Sandstone, Lennep Sandstone, and Hell Creek Formation, in Bruno siding area; Gammon Shale, Claggett, Parkman, Bearpaw, Fox Hills Sandstone, and Hell Creek, in Porcupine dome area. Ammonite zones on cross sections. Cross section B-B' shows rocks equivalent to Montana Group in WY; section C-C' correlates Montana Group rocks in MT with equivalent rocks in WY. Table of stratigraphic nomenclature for MT and WY (fig. 12). Age is latest Santonian to late Maestrichtian (Late Cretaceous).
Summary of Citation: Montana
Publication:
Ruppel, E.T., O'Neill, J.M. and Lopez, D.A., 1993, Geologic map
of the Dillon 1 degrees x 2 degrees quadrangle, Montana: U.S.
Geological Survey Miscellaneous Investigations Series Map,
I-1803-H, 1 sheet, scale 1:250,000
Usage in Publication: Montana Group
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Not used
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Summary: Rocks formerly assigned to the Montana Group in the Dillon area, southwest MT in the Montana folded belt province, are designated unnamed upper and lower parts of an unnamed sedimentary rock sequence of Early and Late Cretaceous age. These sedimentary rocks are younger than the Blackleaf Formation and older than the Beaverhead Group. Name Montana Group not used.
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