Wisconsin glaciation

E63649

The Wisconsin glaciation was the last major advance of continental ice sheets in North America during the Pleistocene, profoundly reshaping the continent’s landscapes and drainage systems.

All labels observed (8)

How this entity was disambiguated

Statements (58)

Predicate Object
instanceOf Pleistocene glaciation
glaciation
affectedRegion Canada
Northeastern United States
Northern Great Plains
linked to: Great Plains

Rocky Mountains
Upper Midwestern United States
alsoKnownAs Wisconsin Stage
Wisconsinan glaciation
causedEvent Missoula floods in the Pacific Northwest
isostatic depression of the crust in formerly glaciated areas
chronostratigraphicUnit Wisconsinan Stage
continent North America
correlatesWith Devensian glaciation
linked to: Würm glaciation

Weichselian glaciation
linked to: Würm glaciation

Würm glaciation
createdFeature Lake Agassiz basin
Lake Missoula basin
basins of the modern Great Lakes (modification of preexisting basins)
createdLandform drumlins in New York and New England
eskers in Canada and northern United States
glacial till plains
kettle lakes in glaciated regions
moraines in the upper Midwest
outwash plains
proglacial lake basins
endApproximate about 11,000 years ago
evidenceType glacial striations
loess deposits
morainic ridges
radiocarbon-dated organic material in glacial sediments
exposedFeature Bering land bridge between Siberia and Alaska
followedBy Holocene epoch
linked to: Holocene

Holocene interglacial
geologicTimeScaleSeries Pleistocene
linked to: Pleistocene epoch
geologicTimeScaleSystem Quaternary
linked to: Quaternary period
influenced distribution of Pleistocene megafauna in North America
migration routes of humans into the Americas
lastGlacialMaximumApproximate about 21,000 years ago
lastMajorAdvanceOf Cordilleran Ice Sheet
Greenland Ice Sheet (North American sector)
Laurentide Ice Sheet
maximumIceExtentReached Last Glacial Maximum
modified Mississippi River drainage
St. Lawrence River drainage
drainage systems of central North America
namedAfter U.S. state of Wisconsin
linked to: Wisconsin
nameProposedBy geologists of the Wisconsin Geological and Natural History Survey
partOf Late Pleistocene
linked to: Pleistocene epoch
precededBy Sangamon interglacial
resultedIn ongoing postglacial isostatic rebound
seaLevelChangeAtMaximum global sea level about 120 meters lower than present
southernIceMarginApproximate Cape Cod
Long Island
Missouri River valley
Nantucket
Ohio River valley
linked to: Ohio Valley region
startApproximate about 75,000 years ago

How these facts were elicited

Referenced by (11)

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

Niagara Falls formedBy Wisconsin glaciation
Baltic Ice Lake formedDuring Weichselian glaciation
linked to: Wisconsin glaciation
Littorina Sea formedAfter Weichselian glaciation
linked to: Wisconsin glaciation
Wisconsin glaciation alsoKnownAs Wisconsinan glaciation
linked to: Wisconsin glaciation
Wisconsin glaciation chronostratigraphicUnit Wisconsinan Stage
linked to: Wisconsin glaciation
Wisconsin glaciation precededBy Sangamon interglacial
linked to: Wisconsin glaciation
Missoula floods timePeriod Late Wisconsin glaciation
linked to: Wisconsin glaciation
Wisconsin Stage hasAlternativeName Wisconsin Glaciation
linked to: Wisconsin glaciation
Wisconsin Stage hasAlternativeName Wisconsinan Glaciation
linked to: Wisconsin glaciation
Wisconsin Stage hasAlternativeName Wisconsinan Stage
linked to: Wisconsin glaciation
Würm glaciation correspondsTo Wisconsin glaciation