Okanogan Lobe

E1023530

The Okanogan Lobe was a large outlet glacier of the Cordilleran Ice Sheet that advanced into north-central Washington State, profoundly shaping the region’s valleys, lakes, and glacial landforms.

All labels observed (2)

How this entity was disambiguated

Statements (31)

Predicate Object
instanceOf glacial lobe
outlet glacier
advancedInto north-central Washington State
affected Columbia River tributary valleys
Okanogan River valley
linked to: Okanogan Valley
associatedWith Cordilleran Ice Sheet maximum extent
country United States
eroded valley floors
valley sides
formed eskers
kettles
moraines
outwash plains
geologicContext Pleistocene glaciation
influenced drainage patterns in north-central Washington
locatedIn Washington State
linked to: Washington
locatedOn North American continent
linked to: North America
meltwaterProduced glacial meltwater streams
namedAfter Okanogan region
linked to: Okanogan Valley
partOf Cordilleran Ice Sheet
process glacial deposition
glacial erosion
region Okanogan region
linked to: Okanogan Valley
scientificDiscipline Quaternary geology
glacial geology
shaped glacial landforms of north-central Washington
lakes of north-central Washington
valleys of north-central Washington
timePeriod Late Pleistocene
transported erratics
glacial till

How these facts were elicited

Referenced by (2)

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

Cordilleran Ice Sheet majorLobe Okanogan Lobe
Glacial Lake Columbia relatedTo Okanogan lobe of the Cordilleran Ice Sheet
linked to: Okanogan Lobe