Steven Dutch, Professor Emeritus, Natural and Applied Sciences, Universityof Wisconsin - Green Bay
Era | Formation | Picture | Notes | ||
Tertiary | Medicine Root Gravels | 0-2 m | |||
Sharps | 30 m | Forms the tips of the highest Badlands pinnacles | |||
Rockyford Ash | 2-4 m | A thin ledge-forming unit just below the tops of the pinnacles. | |||
Brule | 100 m | Makes up most of the Badlands cliffs. Often banded white and pink. | |||
Chadron | 15-20 m | From top to bottom: gray Chadron Formation, red Interior
Paleosol, yellow Yellow Mounds Paleosol, and yellow-gray Fox hillsFormation. The paleosols are not really a formation, but truncate a number of formations. |
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Interior Paleosol | 1-2 m | ||||
Chamberlain Pass | 0-4 m | ||||
Yellow Mounds Paleosol | 2-5 m | ||||
Upper Cretaceous | Fox hills | 6-60 m | |||
Pierre Shale | 200 m + | God must have been in a gray mood when he made this stuff and covered half of South Dakota with it. | |||
Upper Cretaceous | Niobrara Formation | 80 m | |||
Upper Cretaceous | Carlile Shale | 150 m | |||
Upper Cretaceous | Greenhorn Formation | Upper Limestone | 20 m | ||
Lower Shale | 60-80 m | ||||
Upper Cretaceous | Belle Fourche Shale | 100 m | |||
Lower Cretaceous | Mowry Shale | 40 m | |||
Lower Cretaceous | Newcastle Sandstone | 10 m | |||
Lower Cretaceous | Skull Creek Shale | 60-80 m | Dull gray shale with gypsum. Not the white nodular masses of the Spearfish but transparent blades, best seen by sun glint. | ||
Lower Cretaceous | Fall River Formation | 40 m | That's lignite at the bottom. | ||
Lower Cretaceous | Lakota Formation | 70-110 m | |||
Upper Jurassic | Morrison Formation | 0-30 m | The Western Interior Jurassic formation. | ||
Upper Jurassic | Unkpapa Sandstone | 15-40 m | Not typical Unkpapa but striking. This purple and yellow striped facies is found in a small area not publicly accessible. | ||
Upper Jurassic | Sundance Formation | 25 m | Consists of a variety of sandstone and limestone members. | ||
Unconformity | |||||
Permian | Spearfish Formation | The Spearfish and Opeche Formations are all but indistinguishable, except that the Spearfish has abundant gypsum. | |||
Permian | Minnekahta Limestone | Pink, fine-bedded | |||
Permian | Opeche Formation | The Opeche can be told from the very similar Spearfish Formation by its lack of gypsum. | |||
Pennsylvanian-Permian | Minnelusa Formation | Gray but stained orange by the overlying formations. | |||
Unconformity | |||||
Lower Mississippian | Pahasapa Limestone | This is the cave-forming unit in the Black hills. Called Madison Limestone elsewhere and in older literature. | |||
Upper Devonian - Lower Mississippian | Englewood Limestone | This photo nicely shows the two-toned nature of the Englewood: pink below, buff above. | |||
Unconformity | |||||
Cambrian | Deadwood Formation | Various shades of red but has glauconitic members near the base in places. | |||
Unconformity | Here 500 m.y. Deadwood Sandstone rests on 1.7 b.y. old schist. One quarter of the age of the earth is missing here. |
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Created 7 April 2003, Last Update 06 June 2020