Garber-Wellington aquifer system

E945413

The Garber-Wellington aquifer system is a major groundwater resource in central Oklahoma, composed of Permian-age sandstones and related formations that supply water for municipal, industrial, and agricultural use.

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Statements (47)

Predicate Object
instanceOf aquifer system
groundwater resource
aquiferType bedrock aquifer
composedOf Garber Sandstone NERFINISHED
Wellington Formation NERFINISHED
related Permian formations
sandstone
contains groundwater in pore spaces
country United States of America
surface form: United States
developedForUseSince early 20th century
dischargeTo springs
streams
wells
geologicAge Permian NERFINISHED
hasIssue groundwater-level decline in some areas
water-quality concerns in some areas
hasLithology fine- to coarse-grained sandstone
shale
siltstone
hostRockType clastic sedimentary rock
hydrogeologicUnitType confined aquifer
unconfined aquifer
locatedIn central Oklahoma NERFINISHED
managedBy Oklahoma Water Resources Board NERFINISHED
local water utilities
monitoredBy Oklahoma state agencies NERFINISHED
U.S. Geological Survey NERFINISHED
overlies older Paleozoic rocks
partOf Oklahoma groundwater resources
porosityType primary porosity
secondary porosity
primaryUse agricultural water supply
industrial water supply
municipal water supply
rechargeMechanism infiltration through outcrop areas
leakage from overlying units
rechargeSource precipitation
region Southern Great Plains NERFINISHED
suppliesWaterTo Oklahoma City metropolitan area NERFINISHED
central Oklahoma communities
supportsUse industrial wells
irrigation wells
public water-supply systems
underlies younger surficial deposits
waterQualityConcern elevated total dissolved solids in some wells
naturally occurring radionuclides in some areas
nitrate contamination in some areas

Referenced by (1)

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

Permian Garber Sandstone partOf Garber-Wellington aquifer system