Shinarump Conglomerate

E757093

Shinarump Conglomerate is a Late Triassic fluvial sandstone and conglomerate unit of the southwestern United States, notable as a resistant, cliff-forming layer that hosts uranium and copper mineralization.

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Statements (48)

Predicate Object
instanceOf conglomerate
geologic formation
sandstone
sedimentary rock unit
ageEstimate approximately 225 million years old
color light brown
yellowish brown
contains cobbles
pebbles
quartz grains
siliciclastic sediments
country United States of America
surface form: United States
depositionalEnvironment fluvial
diageneticFeature cemented by calcite
cemented by silica
economicImportance copper ore source
uranium ore source
exposedIn Grand Canyon region NERFINISHED
Navajo Nation lands NERFINISHED
forms cliffs
geologicAge Late Triassic
geologicEpoch Late Triassic
geologicPeriod Triassic
hosts roll-front uranium deposits
stratabound copper deposits
isPartOf Chinle Group NERFINISHED
lithology conglomerate
sandstone
locatedIn Arizona NERFINISHED
Colorado
New Mexico
Utah
southwestern United States NERFINISHED
mechanicalProperty resistant
namedFor Shinarump Cliffs NERFINISHED
notableFor copper mineralization
uranium mineralization
oreDepositType copper-bearing sandstone
uranium-bearing sandstone
overlies Moenkopi Formation NERFINISHED
partOf Chinle Formation NERFINISHED
region Colorado Plateau province NERFINISHED
rockType clastic sedimentary rock
stratigraphicRank member
stratigraphicUnitOf Colorado Plateau NERFINISHED
tectonicSetting back-arc continental basin
thicknessRange up to about 30 meters
underlies Chinle mudstones

Referenced by (1)

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

Chinle Formation overlies Shinarump Conglomerate