Palisades Sill

E574673

Palisades Sill is a prominent Jurassic-age igneous intrusion along the Hudson River, best known for forming the steep basalt cliffs of the New Jersey–New York Palisades.

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Statements (45)

Predicate Object
instanceOf geologic formation
igneous intrusion
sill
approximateAgeMa 200
associatedWith opening of the Atlantic Ocean
coolingHistory slow cooling at shallow crustal depths
country United States of America
surface form: United States
emplacementEnvironment subsurface sill intrusion
eruptionStyle non-eruptive intrusive body
exposedIn Palisades Interstate Park NERFINISHED
extendsFrom Jersey City, New Jersey NERFINISHED
extendsTo near Nyack, New York
forms New Jersey Palisades NERFINISHED
New York Palisades NERFINISHED
Palisades cliffs NERFINISHED
geologicAge Jurassic
hasFeature chilled margins
coarse-grained interior
hasImportance classic site for studying sill emplacement
landmark along the Hudson River
intrudedInto Newark Basin sequence NERFINISHED
lithology basaltic rock
diabase
dolerite
locatedAlong Hudson River NERFINISHED
locatedIn Hudson River Palisades NERFINISHED
New Jersey, United States
surface form: New Jersey

New York NERFINISHED
maximumThickness approximately 300 meters
mineralogy olivine (local)
plagioclase
pyroxene
notableFor columnar jointing
prominent vertical cliffs
overlies sedimentary rocks of the Newark Basin
partOf Central Atlantic Magmatic Province NERFINISHED
protectedBy Palisades Interstate Park Commission NERFINISHED
relatedFeature Newark Basin NERFINISHED
Watchung basalts NERFINISHED
rockType mafic intrusive rock
studiedInDiscipline geomorphology
igneous petrology
structural geology
tectonicSetting rift-related magmatism
visibleAs steep basalt cliffs

Referenced by (2)

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

Palisades (across the river in some segments) hasRockUnitName Palisades Sill
subject surface form: Palisades
New Jersey Palisades partOf Palisades Sill