Owl Rock Member

E757097

Owl Rock Member is a distinctive upper unit of the Late Triassic Chinle Formation, known for its colorful mudstones and limestones that preserve important terrestrial and lacustrine fossils in the southwestern United States.

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Statements (46)

Predicate Object
instanceOf member
stratigraphic unit
chronostratigraphy Norian
color colorful
contains carbonate nodules
freshwater limestone beds
paleosols
continent North America
country United States of America
surface form: United States
depositionalSetting fluvial-lacustrine
diagenesis carbonate cementation
environmentOfDeposition lacustrine
terrestrial
exposedIn Arizona NERFINISHED
Colorado NERFINISHED
New Mexico NERFINISHED
Utah NERFINISHED
formationPartOf Chinle Formation NERFINISHED
fossilType invertebrate fossils
plant fossils
vertebrate fossils
geologicAge Late Triassic NERFINISHED
geologicGroup Chinle Group NERFINISHED
geologicPeriod Triassic
hasSedimentaryStructures lamination
mud cracks
ripple marks
knownFor colorful mudstones
fossil preservation
limestones
lithology limestone
mudstone
locatedIn southwestern United States NERFINISHED
namedFor Owl Rock NERFINISHED
overlies Petrified Forest Member NERFINISHED
paleoclimateIndicator semi-arid conditions
partOf Chinle Formation NERFINISHED
preserves lacustrine fossils
terrestrial fossils
region Colorado Plateau NERFINISHED
researchImportance Late Triassic terrestrial ecosystems
Triassic lake environments
stratigraphicHierarchy member of Chinle Formation
stratigraphicPosition upper unit of the Chinle Formation NERFINISHED
typeOf continental sedimentary unit
underlies Rock Point Member NERFINISHED

Referenced by (1)

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

Chinle Formation hasMember Owl Rock Member