Shinarump Member

E757094

Shinarump Member is a prominent sandstone-dominated stratigraphic unit of Late Triassic age in the southwestern United States, known for its fluvial deposits and uranium-bearing horizons.

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All labels observed (1)

Label Occurrences
Shinarump Member canonical 1

Statements (47)

Predicate Object
instanceOf geologic member
stratigraphic unit
ageRange Carnian
associatedWith Colorado Plateau uranium province NERFINISHED
color light brown
yellowish brown
contains carbonaceous material
copper ore
fossil wood
silicified wood
uranium ore
country United States of America
surface form: United States
depositionalEnvironment braided-stream
fluvial
diagenesis cemented by calcite
cemented by iron oxides
cemented by silica
economicImportance copper mining
uranium mining
exposedIn Arizona NERFINISHED
Colorado NERFINISHED
Nevada NERFINISHED
New Mexico NERFINISHED
Utah NERFINISHED
geologicAge Late Triassic
geologicPeriod Triassic
knownFor prominent sandstone-dominated cliff-former
uranium-bearing horizons
lithology conglomeratic sandstone
mudstone
sandstone
siltstone
namedAfter Shinarump Cliffs NERFINISHED
overlies Kaibab Formation NERFINISHED
Moenkopi Formation NERFINISHED
partOf Chinle Formation NERFINISHED
porosity locally high
primarySedimentaryStructures channel-fill geometry
cross-bedding
region southwestern United States NERFINISHED
stratigraphicPosition basal member of the Chinle Formation in many areas
tectonicSetting Colorado Plateau NERFINISHED
thickness highly variable
typeLocality Shinarump Cliffs, Utah NERFINISHED
underlies Monitor Butte Member
Moss Back Member
Petrified Forest Member NERFINISHED

Referenced by (1)

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

Chinle Formation hasMember Shinarump Member