Claron Formation

E289403

The Claron Formation is a geologic rock unit of colorful limestones and mudstones best known for forming the striking hoodoos and cliffs of Bryce Canyon and other parts of the Paunsaugunt Plateau in southern Utah.

All labels observed (5)

How this entity was disambiguated

Statements (41)

Predicate Object
instanceOf geologic formation
rock unit
climateInfluenceOnErosion freeze-thaw cycles
color pink
red
white
contains fossil freshwater mollusks
fossil plants
country United States
depositionalEnvironment fluvial
lacustrine
drainageBasin Colorado River basin
Sevier River basin
linked to: Sevier River
erosionalLandforms fins
spires
windows
exposedAt Bryce Canyon National Park
Cedar Breaks National Monument
Red Canyon
forms cliffs
hoodoos
geologicAge Eocene
Paleogene
lithology limestone
mudstone
locatedIn Paunsaugunt Plateau
southern Utah
namedFor Claron, Utah
notableFor colorful badlands
eroded amphitheaters
overlies Kaiparowits Formation
Wahweap Formation
partOf Colorado Plateau
region Garfield County, Utah
Kane County, Utah
rockType sedimentary rock
stratigraphicUnitOf Bryce Canyon area
subunit Pink Member
White Member
thickness hundreds of meters
weatheringStyle differential erosion

How these facts were elicited

Referenced by (8)

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

Queen's Garden Trail hasGeologicalFeature Claron Formation
Fairyland Loop Trail geology Claron Formation sedimentary rocks
linked to: Claron Formation
Bryce Amphitheater composedOf Claron Formation
Thor's Hammer hoodoo composedOf Claron Formation dolomite
linked to: Claron Formation
Thor's Hammer hoodoo composedOf Claron Formation mudstone
linked to: Claron Formation
Sunrise Point geologicalFeatureVisible Claron Formation hoodoos
linked to: Claron Formation
Peekaboo Loop Trail geologicalContext Claron Formation