• Facets (new session)
• Description
• Metadata
• Settings
  • Rule: ActivityStreamsMapasEquivalentb3sb3sifpdbprdf-labelfacetshttp://dbpedia.org/resource/inference/rules/dbpedia#http://dbpedia.org/resource/inference/rules/opencyc#http://dbpedia.org/resource/inference/rules/umbel#http://dbpedia.org/resource/inference/rules/yago#http://dbpedia.org/schema/property_rules#http://www.ontologyportal.org/inference/rules/SUMO#http://www.ontologyportal.org/inference/rules/WordNet#http://www.w3.org/2002/07/owl#ldpoplwebskos-transurn:det:rdf:labelvirtrdf-labelvirtrdf-urlNone
    
  • Inverse Functional Properties: Disabled (fastest) Apply to subjects only Apply to objects only Apply to both subjects and objects
  • "Same As": Disabled (fastest) Apply to subjects only Apply to objects only Apply to both subjects and objects (recommended) Apply to subjects, objects and predicates (not recommended on big datasets) Apply to predicates only (special use cases only)

About: Hampton Rocks Cutting     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : umbel-rc:Place, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: Thingplacedbo:Locationschema:PlaceSite of Special Scientific InterestSite of Special Scientific Interestgeo:SpatialThingyago:WikicatSitesOfSpecialScientificInterestInAvonyago:WikicatSitesOfSpecialScientificInterestNotifiedIn1990yago:GeographicalArea108574314yago:Location100027167yago:Object100002684yago:PhysicalEntity100001930yago:Region108630985yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Site108651247yago:Tract108673395umbel-rc:Place New Facet based on Instances of this Class

Hampton Rocks Cutting (grid reference ST779666) is a 1.3 hectare geological Site of Special Scientific Interest near the village of Bathampton, Somerset, notified in 1990. The site is listed in the Geological Conservation Review, for its exposure of Pleistocene rocks made up of coarse fluvial gravels showing scour-and-fill structures and planar bedding. Their sedimentology gives a clear indication that the deposits were laid down under 'cold-stage' conditions, probably during the Devensian glacial period.