Crab Creek coulee

E431193

Crab Creek coulee is a prominent erosional valley in Washington’s Channeled Scablands, formed by cataclysmic Ice Age floods and noted for its striking basalt cliffs and dry coulee landscape.

All labels observed (1)

Label Occurrences
Crab Creek coulee canonical 1

How this entity was disambiguated

Statements (34)

Predicate Object
instanceOf coulee
erosional valley
landform
associatedWith Crab Creek
country United States
erosionType fluvial erosion
evidenceFor Missoula-style floods
linked to: Missoula floods
formedAsResultOf rapid flood incision
formedBy Ice Age floods
linked to: Missoula floods

cataclysmic glacial outburst floods
formedDuring late Pleistocene megaflood events
geologicalPeriod Pleistocene
linked to: Pleistocene epoch
hasFeature exposed columnar basalt
stepped coulee walls
hasPhysicalCharacteristic basalt cliffs
dry coulee floor
scabland topography
steep valley walls
hasScientificInterest Quaternary geology
geomorphology
megaflood processes
landscapeType dry coulee landscape
locatedIn Channeled Scablands
United States
Washington
notableFor Channeled Scablands geomorphology
evidence of cataclysmic flooding
striking basalt cliffs
partOf Channeled Scablands erosional system
linked to: Channeled Scablands

Columbia Plateau
primaryRockType basalt
regionType semi-arid
state Washington
surfaceWaterRegime mostly dry

How these facts were elicited

Referenced by (1)

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

Channeled Scablands notableSite Crab Creek coulee