Niobrara Chalk

E683719

Niobrara Chalk is a Late Cretaceous marine sedimentary rock formation of soft, fossil-rich chalk and shale that is especially noted for its abundant marine reptile and fish fossils across the central United States.

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Observed surface forms (1)

Surface form Occurrences
Niobrara Formation 2

Statements (49)

Predicate Object
instanceOf chalk formation
geologic formation
sedimentary rock unit
age Campanian
Coniacian
Santonian
color light-colored
contains coccoliths
foraminifera
microfossils
country United States of America
surface form: United States
depositionalEnvironment Western Interior Seaway NERFINISHED
epicontinental sea
discoveredBy early American geologists
economicUse source of limestone
fossilContent ammonites
birds
invertebrates
marine turtles
mosasaurs
plesiosaurs
pterosaurs
teleost fish
fossilPreservation exceptional vertebrate fossils
geologicPeriod Late Cretaceous NERFINISHED
knownFor well-preserved fish skeletons
well-preserved mosasaur skeletons
well-preserved pterosaur fossils
lithology chalk
shale
namedFor Niobrara River NERFINISHED
notableFor abundant fish fossils
abundant marine reptile fossils
outcropsIn Colorado NERFINISHED
Kansas NERFINISHED
Nebraska NERFINISHED
New Mexico NERFINISHED
South Dakota NERFINISHED
Wyoming NERFINISHED
overlies Carlile Shale NERFINISHED
paleontologicalSignificance important vertebrate fossil lagerstätte
primaryMineral calcite
region central United States
rockType marine sedimentary rock
stratigraphicUnitOf Western Interior Seaway succession
subunit Fort Hays Limestone Member NERFINISHED
Smoky Hill Chalk Member NERFINISHED
texture soft
underlies Pierre Shale NERFINISHED

Referenced by (3)

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

Gove County, Kansas hasGeology Niobrara Chalk
Western Interior Basin includesFormation Niobrara Chalk
this entity surface form: Niobrara Formation
Pierre Shale overlies Niobrara Chalk
this entity surface form: Niobrara Formation