Summerville Formation

E273048

The Summerville Formation is a Late Jurassic sedimentary rock unit in the western United States, characterized by thin-bedded mudstones and sandstones deposited in tidal flat and coastal environments.

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All labels observed (1)

Label Occurrences
Summerville Formation canonical 2

Statements (48)

Predicate Object
instanceOf geologic formation
sedimentary rock unit
beddingCharacteristic thin-bedded
climateIndicator arid to semi-arid conditions
colorCharacteristic brown
red
contains evaporite beds
gypsum
limestone lenses
country United States of America
surface form: United States
depositionalEnvironment coastal
tidal flat
diageneticFeature cemented by calcite
iron-oxide staining
exposedIn canyons of the Colorado Plateau
fossilContent dinosaur tracks
invertebrate trace fossils
geologicAge Jurassic
geologicPeriod Late Jurassic
grainSize fine-grained
hasEconomicInterest construction stone (local use)
hasStratigraphicRank formation
hasStratigraphicRelationship correlative with Curtis Formation in some areas
lithology mudstone
sandstone
locatedIn western United States
namedFor Summerville Point, Emery County, Utah
notableExposure Arches National Park
Capitol Reef National Park
Dinosaur National Monument
overlies Entrada Sandstone
paleogeography nearshore marine to coastal plain
partOf San Rafael Group
primarySedimentaryProcess tidal deposition
region Colorado
New Mexico
Utah
Wyoming
researchField sedimentology
stratigraphy
sedimentaryStructure mud cracks
ripple marks
stratigraphicUnitOf Colorado Plateau
surface form: Colorado Plateau region
tectonicSetting passive continental margin
thickness generally less than 100 meters
timeSpanEnd Kimmeridgian stage
surface form: Kimmeridgian
timeSpanStart Oxfordian
underlies Morrison Formation

Referenced by (2)

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

Morrison Formation overlies Summerville Formation
San Rafael Group isRegionalEquivalentOf Summerville Formation