Chugwater Formation

Chugwater Formation (Group)
Chugwater Formation (Group)
Stratigraphic range: Triassic
	Outcrop of Chugwater Group near Thermopolis, Wyoming
Type	sedimentary
Underlies	Nugget Sandstone, Morrison Formation
Overlies	Dinwoody Formation, Goose Egg Formation
Lithology
Primary	sandstone
Other	shale, gypsum, limestone
Location
Extent	Wyoming, Colorado, Montana
Type section
Named for	Chugwater, Wyoming
Named by	N. H. Darton, 1904

The Chugwater Formation is a mapped bedrock unit consisting primarily of red

formation in Colorado and Montana, but as a Group (set of formations), the Chugwater Group, in Wyoming. Despite its presence below the highly studied Morrison Formation

, the Chugwater receives little attention.

Description

The most noticeable feature on a large scale is the brick-red color, caused by

oxidation of iron minerals in the rock. This color is periodically interrupted by streaks and spots of reduced iron, a light bluish-gray shade. Near the top of the formation is a thick layer of gypsum of very high quality. The whole rock is interrupted by gypsum veins

as well as having a disrupted texture because of the precipitation of gypsum crystals after deposition of the rock.

The Chugwater consists mainly of

crossbedding. Examples of infilled mudcracks

of irregular shape, are common.

The main constituent of the Chugwater is

Feldspars are also present, though in lesser amounts, as are hematite and gypsum. Small flecks of a dark, opaque mineral have been tentatively identified as biotite. The minerals are cemented by a non-carbonate matrix

, probably siliceous.

The Chugwater is a prime example of red beds, commonly deposited during the Permian and Triassic periods.

Stratigraphy

The Chugwater Group

Green River Basin, Laramie Basin

.

For example, in the Wind River and Greater Green River basins, the formations (in ascending stratigraphic order) are: Red Peak Formation, Crow Mountain Formation, Jelm Formation, and Popo Agie Formation.^[3] However, in the Powder River Basin, the formations are: Red Peak Formation, Alcova Limestone, Crow Mountain Sandstone, unnamed red beds, and Popo Agie Formation.^[4]

Age

Relative age dating of the Chugwater places it in the Triassic Period.

References

^ Darton, N.H., 1904, Comparison of the stratigraphy of the Black Hills, Bighorn Mountains, and Rocky Mountain Front Range: Geological Society of America Bulletin, v. 15, p. 379-448. abstract
^ Pipiringos, G.N., 1968, Correlation and nomenclature of some Triassic and Jurassic rocks in south-central Wyoming, IN Shorter contributions to general geology, 1967: U.S. Geological Survey Professional Paper, 594-D, p. D1-D26. link to report
^ High, L.R., Jr., and Picard, M.D., 1969, Stratigraphic relations within upper Chugwater Group (Triassic), Wyoming: American Association of Petroleum Geologists Bulletin, v. 53, no. 5, p. 1091-1104. abstract
^ Cavaroc, V.V., and Flores, R.M., 1991, Red beds of the Triassic Chugwater Group, southwestern Powder River basin, Wyoming, IN Evolution of sedimentary basins; Powder River basin: U.S. Geological Survey Bulletin, 1917-E, p. E1-E17. link to report

[1] Darton, N.H., 1904, Comparison of the stratigraphy of the Black Hills, Bighorn Mountains, and Rocky Mountain Front Range: Geological Society of America Bulletin, v. 15, p. 379-448. abstract

[2] Pipiringos, G.N., 1968, Correlation and nomenclature of some Triassic and Jurassic rocks in south-central Wyoming, IN Shorter contributions to general geology, 1967: U.S. Geological Survey Professional Paper, 594-D, p. D1-D26. link to report

[3] High, L.R., Jr., and Picard, M.D., 1969, Stratigraphic relations within upper Chugwater Group (Triassic), Wyoming: American Association of Petroleum Geologists Bulletin, v. 53, no. 5, p. 1091-1104. abstract

[4] Cavaroc, V.V., and Flores, R.M., 1991, Red beds of the Triassic Chugwater Group, southwestern Powder River basin, Wyoming, IN Evolution of sedimentary basins; Powder River basin: U.S. Geological Survey Bulletin, 1917-E, p. E1-E17. link to report

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