Mersey–Dee glacial meltwater landscape

E561600

The Mersey–Dee glacial meltwater landscape is a distinctive post-glacial terrain in northwest England and northeast Wales, characterized by features such as meres, kettle holes, and meltwater channels formed during the last Ice Age.

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Statements (41)

Predicate Object
instanceOf glacial meltwater landscape
post-glacial landscape
associatedWith River Dee NERFINISHED
River Mersey NERFINISHED
characterizedBy kettle holes
meltwater channels
meres
undulating lowland topography
continent Europe
country United Kingdom
formedBy meltwater from wasting ice sheets
formedDuring Last Glacial Period NERFINISHED
geologicalPeriod Quaternary
hasClimateHistory periglacial conditions after ice retreat
hasEcologicalCharacteristic meres and mosses system
wetland habitats
hasGeologicalOrigin glacial deposition
glacial meltwater erosion
hasHydrologicalFeature poorly drained depressions
hasLandform dry meltwater channel
kettle hole lake
overdeepened basin
pitted outwash plain
hasProcess glacial retreat
ice-contact sedimentation
meltwater incision
hasScientificInterest Quaternary geomorphology
hydrogeology of lowland glacial terrains
palaeoglaciology
hasSediment glaciofluvial sands and gravels
glaciolacustrine silts and clays
hasSoilType glacial till-derived soils
sandy outwash deposits
hasSurfaceHydrology numerous small lakes and ponds
hasTopographicRelief low
isExampleOf lowland deglaciation landscape
isRelevantTo landscape evolution in northeast Wales
landscape evolution in northwest England
locatedIn northeast Wales
northwest England NERFINISHED
partOf British lowland glacial landscapes

Referenced by (1)

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

Ellesmere meres partOf Mersey–Dee glacial meltwater landscape