Weald Clay

E834841

Weald Clay is a thick sequence of Early Cretaceous clay-rich sedimentary rocks in southeast England, notable for forming heavy soils and influencing the region’s low-lying, poorly drained landscapes.

All labels observed (3)

Label Occurrences
Weald Clay canonical 1
Wealden Clay 1
Wealden Greensand 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf geologic formation
sedimentary rock unit
age Aptian
Barremian
Hauterivian
climateIndicator humid temperate continental conditions in Early Cretaceous Weald Basin
contains calcareous concretions
freshwater limestones
ironstone nodules
sandstone lenses
country United Kingdom
depositionalEnvironment floodplain
lacustrine
lagoonal
non-marine
economicUse brickmaking
tile manufacture
engineeringProperty shrink–swell behavior
fossilContent crocodyliforms
dinosaurs
fish remains
freshwater molluscs
ostracods
plant fossils
turtles
geologicPeriod Early Cretaceous
hasColor brown
grey
hydrologicalProperty low permeability
poor drainage
influences low-lying topography
poorly drained landscapes
knownFor heavy clay soils
lithology clay
mudstone
siltstone
namedAfter Weald
outcropsIn Weald Basin
overlies Hastings Beds
Tunbridge Wells Sand Formation
partOf Wealden Group
region southeast England
linked to: South East England
soilTypeDerived gleyed clay soils
stratigraphicUnitOf Weald Basin
typicalThickness up to 450 m
underlies Lower Greensand Group
weatheringProduct sticky clay soils

How these facts were elicited

Referenced by (3)

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

Low Weald underlainBy Weald Clay
Greensand Ridge around Leith Hill ecoregion Wealden Greensand
linked to: Weald Clay
Geology of Kent includesRockType Wealden Clay
linked to: Weald Clay