Moses Coulee

E430715

Moses Coulee is a large, steep-walled canyon in central Washington State carved by Ice Age floods, known for its dramatic basalt cliffs and distinctive Channeled Scablands geology.

All labels observed (1)

Label Occurrences
Moses Coulee canonical 1

How this entity was disambiguated

Statements (45)

Predicate Object
instanceOf canyon
geologic formation
landform
accessibleFrom U.S. Route 2 vicinity
climate continental semi-arid climate
country United States of America
surface form: United States
culturalRegion traditional lands of Native American tribes in central Washington
currentHydrology mostly dry channel
drainageTo Columbia River basin NERFINISHED
erosionalProcess catastrophic outburst flooding
formedBy Ice Age floods
Missoula floods NERFINISHED
formedDuring Pleistocene epoch NERFINISHED
geologicalFeature basalt cliffs
coulee
steep-walled canyon
geomorphicType ephemeral flood channel
habitatType sagebrush steppe
shrub-steppe grasslands
hasBiodiversity raptor nesting habitat
hasFeature basalt columns
coulee floor
dry waterfalls
hanging valleys
scabland topography
steep canyon walls
knownFor distinctive Channeled Scablands geology
dramatic basalt cliffs
well-preserved flood-erosion features
locatedIn Douglas County, Washington NERFINISHED
Washington
surface form: Washington State

central Washington
namedAfter Chief Moses NERFINISHED
near Columbia River NERFINISHED
partOf Channeled Scablands NERFINISHED
Columbia Plateau NERFINISHED
Columbia River Basalt Group landscape NERFINISHED
region semi-arid shrub-steppe
rockType basalt
scientificSignificance evidence for Ice Age megafloods
key example of flood-carved coulee
tourism hiking and nature observation
scenic canyon views
usedFor field education in geomorphology
geologic research

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 Moses Coulee