About: Upper Greensand Formation

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The Upper Greensand Formation is a Cretaceous formation of Albian to Cenomanian in age, found within the Wessex Basin and parts of the Weald Basin in southern England. It overlies the Gault Clay and underlies the Chalk Group. It varies in thickness from zero to 75 m. It is predominantly a glauconitic fine-grained sandstone, locally becoming silty. Fragmentary dinosaur remains, such as those assigned to Iuticosaurus, have been recovered from this formation. It has been quarried as a building stone from Roman times, and used in London and the area of its outcrop from Devon to East Sussex.

Attributes	Values
rdfs:label	Formación Arena Verde (es) Upper Greensand Formation (en)
rdfs:comment	La Formación Arena Verde o Green Sand, es una formación geológica de Cambridge, Inglaterra, formada por sedimentos de mediados del Cretácico, entre el Albiense y el Cenomaniense, hace aproximadamente 112 a 93,5 millones de años. La litología es de caliza, arenisca y conglomerados correspondientes a paleoambientes terrestres y marinos. Se divide en una parte superior y otra inferior. (es) The Upper Greensand Formation is a Cretaceous formation of Albian to Cenomanian in age, found within the Wessex Basin and parts of the Weald Basin in southern England. It overlies the Gault Clay and underlies the Chalk Group. It varies in thickness from zero to 75 m. It is predominantly a glauconitic fine-grained sandstone, locally becoming silty. Fragmentary dinosaur remains, such as those assigned to Iuticosaurus, have been recovered from this formation. It has been quarried as a building stone from Roman times, and used in London and the area of its outcrop from Devon to East Sussex. (en)
name	Upper Greensand Formation (en)
foaf:depiction
dcterms:subject	Phosphorite formations Geologic formations of England Cretaceous England Upper Cretaceous Series of Europe Lower Cretaceous Series of Europe Albian Stage Cenomanian Stage
Wikipage page ID	53531435 (xsd:integer)
Wikipage revision ID	1039103808 (xsd:integer)
Link from a Wikipage to another Wikipage	Potterne Roman Britain Barford St Martin Blackdown Hills Bonchurch Branscombe River Stour, Dorset Ventnor Early modern period Cretaceous Chert Geological formation Glauconite West Sussex Cenomanian Wiltshire Winchester Castle Vale of Pewsey Albian Phosphorite formations East Sussex Eastbourne Amberley Castle Geologic formations of England Exeter Cathedral Norman and Medieval London Hampshire Isle of Wight Iuticosaurus Siltstone Cretaceous England Upper Cretaceous Series of Europe Lower Cretaceous Series of Europe Chalk Group Albian Stage Cenomanian Stage Surrey Reigate Stone Freestone (masonry) Mere, Wiltshire Middle ages Mining Okeford Fitzpaine Selborne Group Shaftesbury Sandstone Foreshore Weald Basin Wessex Basin Gault Clay Malmstone
sameAs	Upper Greensand Formation Upper Greensand Formation Upper Greensand Formation Upper Greensand Formation
underlies	Chalk Group
unitof	Selborne Group
dbp:wikiPageUsesTemplate	dbt:Infobox_rockunit dbt:Reflist dbt:Use_British_English dbt:Use_dmy_dates dbt:Fossil_range
thumbnail	wiki-commons:Special:FilePath/Blackgang_Cliffs_-_geograph.org.uk_-_25067.jpg?width=300
age	Albian–Cenomanian (en)
area	Weald Basin Wessex Basin
caption	Sandstones of the Upper Greensand Formation above Blackgang, Isle of Wight (en)
country	England (en)
period	Cenomanian (en)
Thickness	-4500.0 (second)
type	Geological formation
has abstract	La Formación Arena Verde o Green Sand, es una formación geológica de Cambridge, Inglaterra, formada por sedimentos de mediados del Cretácico, entre el Albiense y el Cenomaniense, hace aproximadamente 112 a 93,5 millones de años. La litología es de caliza, arenisca y conglomerados correspondientes a paleoambientes terrestres y marinos. Se divide en una parte superior y otra inferior. (es) The Upper Greensand Formation is a Cretaceous formation of Albian to Cenomanian in age, found within the Wessex Basin and parts of the Weald Basin in southern England. It overlies the Gault Clay and underlies the Chalk Group. It varies in thickness from zero to 75 m. It is predominantly a glauconitic fine-grained sandstone, locally becoming silty. Fragmentary dinosaur remains, such as those assigned to Iuticosaurus, have been recovered from this formation. It has been quarried as a building stone from Roman times, and used in London and the area of its outcrop from Devon to East Sussex. (en)
otherlithology	Siltstone
overlies	Gault Clay
prilithology	Sandstone
prov:wasDerivedFrom	wikipedia-en:Upper_Greensand_Formation?oldid=1039103808&ns=0
page length (characters) of wiki page	6539 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Upper_Greensand_Formation
is Link from a Wikipage to another Wikipage of	Quercy Phosphorites Formation List of fossiliferous stratigraphic units in England Beaminster Beeding Hill to Newtimber Hill Binnel Bay List of plesiosaur-bearing stratigraphic units

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