This HTML5 document contains 148 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
yago-reshttp://yago-knowledge.org/resource/
dbohttp://dbpedia.org/ontology/
n13http://dbpedia.org/resource/File:
foafhttp://xmlns.com/foaf/0.1/
n19https://global.dbpedia.org/id/
yagohttp://dbpedia.org/class/yago/
dbthttp://dbpedia.org/resource/Template:
rdfshttp://www.w3.org/2000/01/rdf-schema#
freebasehttp://rdf.freebase.com/ns/
dbpedia-pthttp://pt.dbpedia.org/resource/
n12http://commons.wikimedia.org/wiki/Special:FilePath/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
owlhttp://www.w3.org/2002/07/owl#
wikipedia-enhttp://en.wikipedia.org/wiki/
dbchttp://dbpedia.org/resource/Category:
dbphttp://dbpedia.org/property/
provhttp://www.w3.org/ns/prov#
xsdhhttp://www.w3.org/2001/XMLSchema#
wikidatahttp://www.wikidata.org/entity/
dbrhttp://dbpedia.org/resource/

Statements

Subject Item
dbr:Weald_Clay
rdf:type
yago:Group100031264 yago:Formation108426461 yago:Abstraction100002137 yago:WikicatGeologicFormationsOfTheUnitedKingdom yago:Arrangement107938773
rdfs:label
Formação Weald Clay Weald Clay
rdfs:comment
A Formação Weald Clay, também conhecida simplesmente como Weald Clay é uma unidade de rocha sedimentar do Cretáceo Inferior subjacente às áreas do Sudeste da Inglaterra, entre as Colinas do Norte e do Sul, em uma área chamada . É a unidade mais alta do de rochas dentro da Bacia Weald, e a porção superior da unidade é equivalente em idade à porção exposta da Formação Wessex na Ilha de Wight. Ele consiste predominantemente em lamito com camadas finas. Weald Clay or the Weald Clay Formation is a Lower Cretaceous sedimentary rock unit underlying areas of South East England, between the North and South Downs, in an area called the Weald Basin. It is the uppermost unit of the Wealden Group of rocks within the Weald Basin, and the upper portion of the unit is equivalent in age to the exposed portion of the Wessex Formation on the Isle of Wight. It predominantly consists of thinly bedded mudstone. The un-weathered form is blue/grey, and the yellow/orange is the weathered form, it is used in brickmaking.
dbp:name
Weald Clay
foaf:depiction
n12:Gallois_Geological_Map_of_Wealden_District_1965.jpg n12:Iguanodon_new_NT.jpg n12:Leptocleidus1DB.jpg n12:Mantellisaurus_atherfieldensis_Steveoc.jpg n12:Baryonyx_walkeri_restoration.jpg n12:Weald_Clay_Cooden_Beach.jpg n12:Clay_Pit,_Clock_House,_near_Capel_-_geograph.org.uk_-_1779315.jpg
dcterms:subject
dbc:Geologic_formations_of_the_United_Kingdom dbc:Lower_Cretaceous_Series_of_Europe dbc:Geology_of_England dbc:Barremian_Stage dbc:Hauterivian_Stage dbc:Claystone
dbo:wikiPageID
1770941
dbo:wikiPageRevisionID
1115442793
dbo:wikiPageWikiLink
dbr:Mudstone dbr:England dbr:Limestone dbr:Salamander dbr:Isle_of_Wight dbr:Ilerdocossus dbr:Ommatidae dbr:Wyleyia dbr:Iguanodon dbr:Omma dbr:Sauropoda n13:Iguanodon_new_NT.jpg dbr:South_Downs dbr:Siltstone dbr:Clock_House_Brickworks dbr:Lower_Cretaceous dbr:Dorsetisaurus dbr:Wealden_Group dbr:Englathauma dbc:Geology_of_England dbr:Sedimentary_rock dbr:Wealden_District dbr:Phasmatodea dbr:Horsham_Stone dbr:Principiala dbr:Dryosauridae dbr:Spinosauridae dbr:Weald dbr:Wessex_Formation dbr:Weald_Basin dbr:Palaeontinidae dbr:Zygadenia dbr:Atlas_(anatomy) dbr:Marine_transgression dbr:Mesoraphidiidae dbr:Cretophasmomima dbr:Mantellisaurus dbr:Scorpionfly dbr:Baryonyx dbr:Proraphidia dbr:London_Clay dbr:Smokejack_Clay_Pit n13:Weald_Clay_Cooden_Beach.jpg dbr:Brochocoleus dbr:Valdosaurus n13:Mantellisaurus_atherfieldensis_Steveoc.jpg dbr:Cionocoleus dbr:Auclaye dbr:Brackish_water dbr:Sussex_Marble dbr:Brick dbr:North_Downs n13:Baryonyx_walkeri_restoration.jpg dbc:Hauterivian_Stage dbr:Ironstone dbr:Diluticupes dbr:Alluvial_plain dbr:Ankylosaur dbc:Barremian_Stage dbr:Balveherpeton dbr:Polacanthinae dbr:Shale dbr:Polacanthus dbr:Horshamosaurus dbr:Tunbridge_Wells_Sand_Formation dbr:Ithonidae dbr:Leptocleidus dbr:Oxford_Clay dbr:Geological_formation dbr:Valdicossus dbr:Frog dbc:Claystone dbr:Barremian dbr:Hauterivian dbr:Aptian dbr:Atherfield_Clay_Formation n13:Leptocleidus1DB.jpg dbr:Tarsophlebiidae dbr:List_of_dinosaur-bearing_rock_formations dbc:Lower_Cretaceous_Series_of_Europe dbr:Lacustrine_deposits dbr:Sandstone dbr:Lagoon dbc:Geologic_formations_of_the_United_Kingdom
owl:sameAs
wikidata:Q7977996 freebase:m.05vnx1 dbpedia-pt:Formação_Weald_Clay yago-res:Weald_Clay n19:4xuNe
dbp:subunits
Horsham Stone Member
dbp:underlies
dbr:Atherfield_Clay_Formation
dbp:unitof
dbr:Wealden_Group
dbp:wikiPageUsesTemplate
dbt:Flag dbt:Clear dbt:Fossilrange dbt:UK-geology-stub dbt:Short_description dbt:Portal dbt:ISBN dbt:Infobox_rockunit dbt:Use_dmy_dates dbt:Reflist
dbo:thumbnail
n12:Clay_Pit,_Clock_House,_near_Capel_-_geograph.org.uk_-_1779315.jpg?width=300
dbp:age
Hauterivian-Barremian,
dbp:caption
Weald Clay exposed at Clock House Brickworks
dbp:mapCaption
Extent of the Weald Clay within the Weald Basin, shown with horizontal lines
dbp:period
Barremian
dbp:region
dbr:England
dbp:thickness
27600.0
dbp:type
dbr:Geological_formation
dbo:abstract
A Formação Weald Clay, também conhecida simplesmente como Weald Clay é uma unidade de rocha sedimentar do Cretáceo Inferior subjacente às áreas do Sudeste da Inglaterra, entre as Colinas do Norte e do Sul, em uma área chamada . É a unidade mais alta do de rochas dentro da Bacia Weald, e a porção superior da unidade é equivalente em idade à porção exposta da Formação Wessex na Ilha de Wight. Ele consiste predominantemente em lamito com camadas finas. A formação foi depositada em condições lagunares, lacustres e aluviais que variaram de água doce a salobra. A argila se alterna com outras litologias subordinadas, notavelmente leitos duros de pedra-ferro, calcário (Mármore de Sussex) e arenitos, incluindo a unidade de arenito calcário referida como a . Ele tem um contato gradual e conformável com a subjacente e tem um contato brusco e inconformável com a sobrejacente, uma unidade marinha rasa depositada após a transgressão marinha durante o Aptiano. Weald Clay or the Weald Clay Formation is a Lower Cretaceous sedimentary rock unit underlying areas of South East England, between the North and South Downs, in an area called the Weald Basin. It is the uppermost unit of the Wealden Group of rocks within the Weald Basin, and the upper portion of the unit is equivalent in age to the exposed portion of the Wessex Formation on the Isle of Wight. It predominantly consists of thinly bedded mudstone. The un-weathered form is blue/grey, and the yellow/orange is the weathered form, it is used in brickmaking. The formation was deposited in lagoonal, lacustrine and alluvial conditions that varied from freshwater to brackish. The clay alternates with other subordinate lithologies, notably hard red-weathering beds of ironstone, limestone (Sussex Marble) and sandstones, notably including the calcareous sandstone unit referred to as the Horsham Stone. It has a gradual, conformable contact with the underlying Tunbridge Wells Sand Formation, and has a sharp, unconformable contact with the overlying Atherfield Clay Formation, a shallow marine unit deposited after marine transgression during the Aptian.
dbp:namedfor
dbr:Weald
dbp:otherlithology
dbr:Siltstone dbr:Sandstone dbr:Ironstone dbr:Limestone
dbp:overlies
dbr:Tunbridge_Wells_Sand_Formation
dbp:prilithology
dbr:Mudstone dbr:Shale
prov:wasDerivedFrom
wikipedia-en:Weald_Clay?oldid=1115442793&ns=0
dbo:wikiPageLength
15120
foaf:isPrimaryTopicOf
wikipedia-en:Weald_Clay