Hythe Beds

E503031

Hythe Beds are a geological formation in southeast England characterized by layers of limestone and sandstone, notably including Kentish ragstone, deposited during the Early Cretaceous period.

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Statements (47)

Predicate Object
instanceOf geological formation
lithostratigraphic unit
age approximately 125–120 million years ago
chronostratigraphicUnit Lower Cretaceous
containsFossils bivalves
gastropods
marine invertebrates
country England
depositionalEnvironment nearshore
shallow marine
economicUse aggregate
building stone
foundIn North Downs NERFINISHED
Weald of Kent NERFINISHED
geologicalAge Aptian NERFINISHED
geologicalPeriod Early Cretaceous
hasColor brown
grey
hasPermeability locally high
hasPorosity moderate
hasSedimentaryStructures bedding planes
cross-bedding
lithology calcareous sandstone
limestone
ragstone
sandstone
memberOf Wealden Basin succession NERFINISHED
namedAfter Hythe NERFINISHED
notableLithology Kentish ragstone
notableStone Kentish ragstone NERFINISHED
notableUseLocation Maidstone area
Medway Valley NERFINISHED
outcropArea Kent NERFINISHED
Surrey NERFINISHED
Sussex NERFINISHED
overlies Atherfield Clay Formation NERFINISHED
partOf Lower Greensand Group NERFINISHED
primaryMineralogy calcite
quartz
region southeast England
rockTypeClass sedimentary rock unit
stratigraphicRank formation
thickness up to several tens of metres
underlies Sandgate Beds NERFINISHED
usedSince Roman period (for building stone)
weatheringCharacteristic forms blocky outcrops
forms rubbly slopes

Referenced by (1)

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

Kentish ragstone partOf Hythe Beds