Toroweap Formation

E1006661

The Toroweap Formation is a Permian-age sedimentary rock unit of the southwestern United States, notable for its sandstone, limestone, and gypsum layers that form prominent cliffs and slopes in the Grand Canyon region.

Try in SPARQL Jump to: Statements Referenced by

Statements (47)

Predicate Object
instanceOf geologic formation
sedimentary rock unit
ageRange middle Permian
contains eolian sandstone beds
evaporite deposits
marine limestone beds
containsFossils marine invertebrates
containsMineral anhydrite
calcite
gypsum
country United States of America
surface form: United States
depositionalEnvironment coastal eolian
shallow marine
tidal flat
exposedIn Grand Canyon NERFINISHED
forms cliff-forming units
slope-forming units
geologicAge Permian
geologicPeriod Permian period
geologicProvince Colorado Plateau Province NERFINISHED
hasColor gray
reddish-brown
tan
hasMember Brady Canyon Member NERFINISHED
Seligman Member
Wood Ranch Member NERFINISHED
isImportantFor reconstructing Permian paleoenvironments
isMappedBy U.S. Geological Survey NERFINISHED
isPartOfSequence Permian stratigraphic sequence of the Grand Canyon
isWellExposedAt North Rim of the Grand Canyon NERFINISHED
Toroweap Overlook NERFINISHED
lithology gypsum
limestone
sandstone
locatedIn Arizona NERFINISHED
Nevada
Utah
namedFor Toroweap Valley NERFINISHED
notableFor prominent cliffs
slopes
overlies Coconino Sandstone NERFINISHED
partOf Colorado Plateau NERFINISHED
Grand Canyon stratigraphy NERFINISHED
region southwestern United States
surface form: Southwestern United States
stratigraphicUnitOf Grand Canyon Supergroup NERFINISHED
thickness approximately 70 to 150 meters
underlies Kaibab Formation NERFINISHED

Referenced by (1)

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