Red Eagle Formation
| Red Eagle Formation | |
|---|---|
| Stratigraphic range: Carboniferous-Permian boundary[1] | |
| Type | Formation |
| Unit of | Council Grove Group |
| Sub-units | In Kansas and Nebraska: *Howe Limestone *Bennett Shale *Glenrock Limestone |
| Lithology | |
| Primary | Limestone |
| Other | Shale |
| Location | |
| Coordinates | Lua error in Module:Coordinates at line 489: attempt to index field 'wikibase' (a nil value). |
| Region | Midcontinent (Oklahoma, Kansas, Nebraska) |
| Country | United States |
| Type section | |
| Named for | Red Eagle School, southwest of Foraker, Oklahoma[2] |
| Named by | K.C. Heald |
| Year defined | 1916 |
The Red Eagle Formation (or Red Eagle Limestone) is a geologic formation ranging from Oklahoma, through Kansas, into southeast Nebraska of the United States.[2] Its members define the Carboniferous-Permian boundary in Kansas.[1]
Lithology
[edit | edit source]In the Oklahoma type location, the Red Eagle is a single limestone unit, not further defined into members. However, from the far southeast Nebraska type section into northern Kansas, the Red Eagle Formation consists of three members, each with distinctive lithologies. In Nebraska and northern Kansas in particular, the formation stands out on riverside bluffs and road cuts as two blocky, light-colored limestones sandwiching a dark layer of shale.[2]
Howe Limestone
[edit | edit source]Named from exposures south of Howe, Nebraska, the Howe Limestone member is a grey limestone, 4-5 feet thick, that weathers to buff or slightly yellow. The limestone exhibits brachiopods, baculites, and larger bivalve mollusks.[3] The environment was an open, but very shallow sea with very little in the way of terrigenous sediments. As such, the topmost bed is particularly notable for algae beds and melon-sized stromatolites.
Bennett Shale
[edit | edit source]Named from exposures along the Little Nemaha River and its branches south of Bennet, Nebraska, the Bennett Shale member is a dark, carbonaceous shale, 2.5 to 15 feet thick.[4] This very dark shale shows contrasting light-colored, circular, thin-shelled Orbiculoidea, roughly 1cm (1/3") in diameter. However, south of Interstate 70 in Kansas, the member becomes increasing limestone to the point that within Oklahoma, the bed is completely limestone and the Red Eagle unit undivided by any significant shale bed.
The Bennett is the youngest Permian rock unit in Kansas.
Glenrock Limestone
[edit | edit source]Named from exposures high in valley sides just northwest of Glenrock, Nebraska, the Glenrock Limestone member is lighter grey.[5] It is a hard limestone; fresh fractures sparkle in full sunlight from tiny calcite crystals.
The Glenrock is the oldest Carboniferous rock unit in Kansas.
See also
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- List of fossiliferous stratigraphic units in Nebraska
- List of fossiliferous stratigraphic units in Kansas
- List of fossiliferous stratigraphic units in Oklahoma
- Paleontology in Nebraska
- Paleontology in Kansas
- Paleontology in Oklahoma
References
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Further reading
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- Permian Oklahoma
- Permian Kansas
- Carboniferous southern paleotropical deposits
- Cisuralian Series of North America
- Limestone formations of the United States
- Shale formations of the United States
- Geologic formations of Oklahoma
- Geologic formations of Kansas
- Geologic formations of Nebraska
- Oklahoma geologic formation stubs
- Kansas geologic formation stubs
- Permian stubs