Gettysburg–Newark Lowland section

E800558

The Gettysburg–Newark Lowland section is a geologic and topographic region characterized by broad lowlands underlain by Triassic and Jurassic sedimentary and igneous rocks within the Piedmont of the northeastern United States.

Try in SPARQL Jump to: Statements Referenced by

Statements (45)

Predicate Object
instanceOf geologic region
physiographic section
topographic region
characterizedBy broad lowlands
contains Culpeper Basin NERFINISHED
Deerfield Basin NERFINISHED
Gettysburg Basin NERFINISHED
Hartford Basin NERFINISHED
Newark Basin NERFINISHED
rift basin deposits
contrastsWith adjacent crystalline highlands
extendsInto Connecticut NERFINISHED
Maryland NERFINISHED
Massachusetts NERFINISHED
New Jersey NERFINISHED
Pennsylvania NERFINISHED
Virginia NERFINISHED
formedBy Mesozoic rifting along eastern North America
hasClimate humid temperate
hasEconomicResource building stone
crushed stone
hasGeologicAge Mesozoic
hasPhysiographicDivision Appalachian Highlands division NERFINISHED
hasPhysiographicProvince Piedmont NERFINISHED
hasRockType basalt
conglomerate
diabase
sandstone
shale
hasSoilDerivedFrom weathered basalt
weathered sedimentary rocks
hasTopography broad valleys
low relief
locatedIn northeastern United States NERFINISHED
mappedBy United States Geological Survey NERFINISHED
namedAfter Gettysburg NERFINISHED
Newark NERFINISHED
partOf Appalachian Highlands NERFINISHED
Piedmont physiographic province NERFINISHED
supportsLandUse agriculture
urban development
underlainBy Jurassic igneous rocks
Jurassic sedimentary rocks
Triassic igneous rocks
Triassic sedimentary rocks

Referenced by (1)

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

Piedmont Province in Pennsylvania contains Gettysburg–Newark Lowland section