Springfield Plateau

E150534

The Springfield Plateau is a geologic region within the Ozarks characterized by gently rolling terrain, extensive karst features, and thick layers of Mississippian limestone and chert.

All labels observed (1)

Label Occurrences
Springfield Plateau canonical 3

How this entity was disambiguated

Statements (46)

Predicate Object
instanceOf geologic region
plateau
borderedBy Boston Mountains
Osage Plains
Salem Plateau
characterizedBy caves
gently rolling terrain
karst topography
sinkholes
springs
climateType humid subtropical to humid continental transition
composedPrimarilyOf Mississippian limestone
chert
contains extensive groundwater aquifers
karst springs used for water supply
drainedBy James River (Missouri)
Neosho River
Sac River
White River
elevationRange approximately 1,000 to 1,700 feet above sea level
geologicAge Mississippian
geologicUnitIncludes Boone Formation
Springfield Plateau aquifer
hasEconomicActivity agriculture
limestone quarrying
tourism related to caves and springs
hasMajorCity Fayetteville, Arkansas, United States
surface form: Fayetteville, Arkansas

Joplin, Missouri
Springfield, Missouri
hasSoilsDerivedFrom cherty residuum
weathered limestone
hydrologyInfluencedBy karst drainage
isSubregionOf Interior Highlands
landUse cropland
pasture
urban development
locatedIn Arkansas
Missouri
Oklahoma
United States of America
surface form: United States
namedAfter Springfield, Missouri
overlies older Ordovician rocks
partOf Ozark Plateau
surface form: Ozarks
physiographicProvinceOf Ozark Plateau
surface form: Ozark Plateaus
supportsEcosystem oak-hickory forest
tallgrass prairie remnants

How these facts were elicited

Referenced by (3)

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

Ozarks region (partly) hasPart Springfield Plateau
subject surface form: Ozarks
Ozark Plateau hasPart Springfield Plateau
Interior Highlands contains Springfield Plateau