Magnesian Limestone succession

E206821

The Magnesian Limestone succession is a geological sequence of Permian-age dolomitic limestone formations that forms a distinctive belt across parts of northern and central England.

Try in SPARQL Jump to: Surface forms Statements Referenced by

All labels observed (2)

Statements (30)

Predicate Object
instanceOf Permian rock unit
geological formation
stratigraphic succession
contains dolomite
limestone
country England
depositionalEnvironment evaporitic
shallow marine
extendsFrom Nottinghamshire
extendsTo County Durham
forms distinctive belt
geologicalAge Permian
hasCharacteristic magnesium-rich carbonate
well-developed escarpments
hasEconomicImportance construction industry
quarrying
hasOutcropsIn Durham
Nottinghamshire
Yorkshire
hasStratigraphicRank group
isPartOf Magnesian Limestone succession self-linksurface differs
surface form: Permian stratigraphy of the United Kingdom
isRecognizedBy British Geological Survey
lithology dolomitic limestone
overlies Carboniferous rocks
partOf Permian Basin of northern England
region central England
Northern England
surface form: northern England
underlies Triassic rocks
usedFor aggregate
building stone

Referenced by (2)

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

Anston limestone partOf Magnesian Limestone succession
Magnesian Limestone succession isPartOf Magnesian Limestone succession self-linksurface differs
this entity surface form: Permian stratigraphy of the United Kingdom