Würm glaciation

E309210

The Würm glaciation was the last major glacial period of the Pleistocene in the Alps, marked by extensive ice coverage and shaping much of the region’s modern landscape.

All labels observed (4)

Label Occurrences
Würm glaciation canonical 3
Weichselian glaciation 2
Devensian glaciation 1

How this entity was disambiguated

Statements (54)

Predicate Object
instanceOf Pleistocene glaciation
Quaternary glacial period
glaciation
associatedWith expansion of continental ice sheets
lowered global sea levels
periglacial processes in areas beyond the ice margin
caused deepening of Alpine valleys
formation of U-shaped valleys in the Alps
formation of glacial lakes in the Alpine region
formation of moraines in the Alpine foreland
overdeepened lake basins such as Lake Constance
overdeepened lake basins such as Lake Garda
overdeepened lake basins such as Lake Geneva
characterizedBy extensive valley glaciers
large piedmont glaciers
thick ice caps over the Alps
climate cold glacial climate
correspondsTo Last Glacial Period
surface form: Devensian glaciation

Last Glacial Period
Last Glacial Period
surface form: Weichselian glaciation

Wisconsin glaciation
countryContext Austria
France
Germany
Italy
Switzerland
endedWith transition to Holocene
endTime approximately 11,700 years ago
end of Pleistocene
evidence glacial striations on Alpine bedrock
outwash plains in front of Alpine glaciers
terminal moraines in Alpine foreland
follows Saalian glaciation
surface form: Riss glaciation
hasPart Last Glacial Maximum in the Alps
early Würm
late Würm
middle Würm
influenced distribution of sediments in the Alpine foreland
drainage patterns in and around the Alps
modern Alpine landscape
maximumExtentTime around 24,000–20,000 years ago
namedAfter Würm River
surface form: River Würm
occursIn Alps
partOf Pleistocene epoch
Quaternary period
precededBy Saalian glaciation
surface form: Riss glaciation
region Central Alps
Alps
surface form: Northern Alps

southern Alps
surface form: Southern Alps
startTime approximately 115,000 years ago
studiedIn Quaternary geology
geomorphology
paleoclimatology
timeEquivalent Cenozoic glaciations
surface form: Marine Isotope Stages 5d–2

How these facts were elicited

Referenced by (7)

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

Wisconsin glaciation correlatesWith Würm glaciation
this entity surface form: Weichselian glaciation
Wisconsin glaciation correlatesWith Würm glaciation
this entity surface form: Devensian glaciation
Wisconsin glaciation correlatesWith Würm glaciation
Fennoscandian Ice Sheet majorGlaciation Würm glaciation
this entity surface form: Weichselian glaciation
Last Glacial Maximum alsoKnownAs Würm glaciation
this entity surface form: LGM
Wisconsin Stage correlatesWith Würm glaciation
Würm namedAfter Würm glaciation