Inyan Kara Group

Inyan Kara Group
Stratigraphic range: Cretaceous
TypeGroup
Sub-unitsFall River Sandstone
Lakota Formation
Location
RegionSouth Dakota
CountryUnited States

The Inyan Kara Group is a geologic group classification applied in South Dakota and adopted in portions of Wyoming and Montana. It preserves fossils of the mid-Cretaceous period. Of late Albian age, this classification correlates with the lower Dakota Formation (Nishnabotna member) known in the southwest corner of the State.

The South Dakota Geological Survey has also extended the Graneros to group other formations into a unit that correlates with the upper Dakota Formation (Note: This definition is widely different than the generally consistent definitions of Graneros/Belle Fourche.[1]). These state definitions of the Inyan Kara and Graneros Groups thereby cover the first two sequences of the Western Interior Seaway recorded by the Dakota Formation.[2][3]

North Dakota also classifies the same strata as Inyan Kara, but only of formation rank without recognizing further formal subdivision, and assigns this Inyan Kara Formation as the lowest member of the Dakota Group.[4]

  1. ^ Hattin, Donald E. (1965). "Stratigraphy of the Graneros Shale (Upper Cretaceous) in Central Kansas". Kansas Geological Survey Bulletin (178). Kansas Geological Survey: Stratigraphy / Graneros Shale / Name and Definition. Retrieved September 6, 2021. The lithologic equivalent of the Graneros in the Black Hills and surrounding areas is the Belle Fourche Shale. Considerable similarity exists between these two formations, and, if the name Graneros is to be perpetuated in the Black Hills region, it would be best used to replace the name Belle Fourche over which the former has priority.
  2. ^ South Dakota Stratigraphic Correlation Chart, SDGS, 2007.
  3. ^ "Geologic Unit: Inyan Kara". National Geologic Database. Geolex — Significant Publications. United States Geological Survey. Retrieved 2021-09-04.
  4. ^ North Dakota Stratigraphic Column, North Dakota Geological Survey, 2009.