| http://data.bgs.ac.uk/ref/Lexicon/hasLithologyDescription | ['Limestone, coralliferous, variably ooidal, shelly: member typically formed of two beds: a lower shelly, ooidal, bioclastic packstone/wackestone with coral debris, and an upper very fossiliferous calcilutite with many corals \r\nin life position, coral debris and a shelly fauna of bivalves, gastropods and echinoids. This passes laterally in places into a sparsely fossiliferous, laminated limestone facies.'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasOldestAgeValue | ['163.5'] |
| http://www.w3.org/2000/01/rdf-schema#label | ['Coral Rag Member (Cleveland Basin)'] |
| http://www.w3.org/2004/02/skos/core#broader | ['http://data.bgs.ac.uk/id/Lexicon/NamedRockUnit/COO'] |
| http://www.w3.org/2004/02/skos/core#prefLabel | ['Coral Rag Member (Cleveland Basin)'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasYoungestAge | ['http://data.bgs.ac.uk/id/Geochronology/Division/JO'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasBroaderPredominantAge | ['http://data.bgs.ac.uk/id/Geochronology/Division/J'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasLowerBoundaryDefinition | ['Non sequence or erosional disconformity: generally a poorly to moderately shelly ooid-limestone (Malton Oolite Member, Coralline Oolite Formation) sharply overlain by a moderately to highly fossiliferous, moderately ooidal, lime-muddy, bioclastic limestone (Coral Rag Member); locally boulders of Malton Oolite may be set in Coral Rag limestone (Wright, 1972, p. 241).'] |
| http://www.w3.org/2004/02/skos/core#notation | ['CLRG'] |
| https://www.w3.org/2003/06/sw-vocab-status/ns#term_status | ['stable'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasYoungestAgeValue | ['157.3'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasObsoleteEquivalent | ['http://data.bgs.ac.uk/id/Lexicon/NamedRockUnit/H2706'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasOldestAge | ['http://data.bgs.ac.uk/id/Geochronology/Division/JO'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasThicknessDescription | ['Up to 12m: Tabular Hills 1 to 9m, Hambleton Hills 4.5 to 8m, Howardian Hills 0 to at least 12m.'] |
| http://www.w3.org/2004/02/skos/core#altLabel | ['Coral Rag [Obsolete: use CLRG, WYLS]'] |
| http://www.w3.org/2004/02/skos/core#inScheme | ['http://data.bgs.ac.uk/ref/Lexicon'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasPredominantAge | ['http://data.bgs.ac.uk/id/Geochronology/Division/JO'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasUpperBoundaryDefinition | ['Non-sequence: rubbly coralliferous shelly limestone (Coral Rag Member) sharply overlain by silty mudstone and fine-grained sandstone (Newbridge Member) or fine-grained calcareous sandstone (Spaunton Sandstone Member) or unfossiliferous fine-grained limestone (North Grimston Cementstone Member) or mudstone (Langton Clay Member) or sandstone (Limekiln Member), all of Upper Calcareous Grit Formation.'] |
| http://www.w3.org/1999/02/22-rdf-syntax-ns#type | ['http://www.w3.org/2004/02/skos/core#Concept'] |
| http://data.bgs.ac.uk/ref/Lexicon/hasRockUnitRank | ['http://data.bgs.ac.uk/id/Lexicon/RockUnitRank/M'] |
| http://www.w3.org/2004/02/skos/core#definition | ['Limestone with subsidiary ooid-limestone. Stratified bedrock. Occurs onshore. Deposited during the Oxfordian Age (Jurassic Period) (163.5-157.3 Ma BP).'] |