Sundance Formation

Sundance Formation
Stratigraphic range: Bathonian - Oxfordian
TypeGeological formation
Sub-unitsCanyon Springs Sandstone Member, Hulett Sandstone Member, Lak Member, Pine Butte Member, Redwater Shale Member, Stockade Beaver (Shale) Member, Windy Hill Sandstone Member
UnderliesMorrison Formation
OverliesGypsum Springs Formation
ThicknessUp to 100 m
Lithology
Primaryshale
Otherlimestone, sandstone
Location
RegionWestern North America
CountryUnited States
Type section
Named forSundance, Wyoming
Named byDarton
Year defined1904

The Sundance Formation is a western North American sequence of Middle Jurassic to Upper Jurassic age Dating from the Bathonian to the Oxfordian, around 168-157 Ma, It is up to 100 metres thick and consists of marine shale, sandy shale, sandstone, and limestone deposited in the Sundance Sea, an inland sea that covered large parts of western North America during the Middle and early Late Jurassic.