Permian Garber Sandstone

E279782

Permian Garber Sandstone is a geologic formation from the Permian period in Oklahoma, notable as the primary host rock for the distinctive barite "rose rock" concretions.

All labels observed (1)

Label Occurrences
Permian Garber Sandstone canonical 1

How this entity was disambiguated

Statements (37)

Predicate Object
instanceOf geologic formation ⓘ
sedimentary rock unit ⓘ
ageRange Early Permian ⓘ
aquiferRole major freshwater aquifer ⓘ
associatedWith Wellington Formation ⓘ
color reddish-brown ⓘ
contains conglomeratic beds ⓘ
shale ⓘ
siltstone ⓘ
containsCement calcite ⓘ
iron oxide ⓘ
containsFossils rare vertebrate and invertebrate fossils ⓘ
containsMineral barite ⓘ
quartz ⓘ
country United States ⓘ
diageneticFeature barite-cemented concretions ⓘ
environmentOfDeposition deltaic ⓘ
fluvial ⓘ
formsPartOf Permian red beds of Oklahoma ⓘ
geologicAge Permian ⓘ
geologicPeriod Permian period ⓘ
linked to: Permian Period
geologicProvince Midcontinent region of the United States ⓘ
hostRockFor barite rose rocks ⓘ
hydrologicCharacteristic moderate to high permeability ⓘ
lithology sandstone ⓘ
locatedIn Oklahoma ⓘ
namedFor Garber, Oklahoma ⓘ
notableFor barite rose rock concretions ⓘ
overlies Chase Group ⓘ
partOf Garber-Wellington aquifer system ⓘ
porosityType primary intergranular porosity ⓘ
primaryComposition fine- to medium-grained sandstone ⓘ
regionalExtent central Oklahoma ⓘ
stratigraphicUnitOf Central Oklahoma ⓘ
linked to: central Oklahoma
underlies Hennessey Group ⓘ
usedFor groundwater supply ⓘ
weatheringCharacteristic forms ledges and slopes ⓘ

How these facts were elicited

Referenced by (1)

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

Rose rock → foundIn → Permian Garber Sandstone ⓘ