Wellington Formation

E279783

The Wellington Formation is a Permian-age geological formation in the central United States, particularly Oklahoma, known for its red beds, evaporite deposits, and distinctive barite "rose rock" concretions.

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All labels observed (1)

Label Occurrences
Wellington Formation canonical 2

Statements (43)

Predicate Object
instanceOf geologic formation
stratigraphic unit
ageStatus early Permian
colorCharacteristic red
containsFossilsOf Permian invertebrates
trace fossils
containsMineral anhydrite
barite
gypsum
halite
country United States of America
surface form: United States
depositionalEnvironment continental
evaporitic
playa lake
economicImportance collector source of barite rose rocks
source of evaporite minerals
geologicAge Permian
geologicPeriod Cisuralian
hasConcretionType barite rose
hasRockType chemical sedimentary rock
clastic sedimentary rock
hasSedimentaryStructure mud cracks
ripple marks
knownFor barite rose rock concretions
lithology anhydrite
evaporite
gypsum
halite
red beds
sandstone
shale
siltstone
locatedIn Kansas
Oklahoma
Texas
central United States
namedFor Wellington, Kansas
overlies Chase Group
partOf Permian Period
surface form: Permian System

Permian red beds of the Midcontinent
stratigraphicUnitOf Central United States
surface form: Midcontinent region
underlies Harper Sandstone
Ninnescah Shale

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Rose rock foundIn Wellington Formation
Permian Garber Sandstone associatedWith Wellington Formation