About: Bourne SSSI, Avon     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : umbel-rc:Place, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)
QRcode icon
http://dbpedia.demo.openlinksw.com/c/67oziLPdXY

Bourne SSSI, Avon (grid reference ST484600) is an 8.47 hectare geological Site of Special Scientific Interest near the village of Burrington, North Somerset, notified in 1992. This site is of considerable importance because it has provided detailed information upon the composition of a north Mendip Pleistocene alluvial fan. An alluvial fan is a fan-shaped deposit formed where a fast flowing stream flattens, slows, and spreads typically at the exit of a canyon onto a flatter plain.

AttributesValues
rdf:type
rdfs:label
  • Bourne SSSI, Avon (en)
rdfs:comment
  • Bourne SSSI, Avon (grid reference ST484600) is an 8.47 hectare geological Site of Special Scientific Interest near the village of Burrington, North Somerset, notified in 1992. This site is of considerable importance because it has provided detailed information upon the composition of a north Mendip Pleistocene alluvial fan. An alluvial fan is a fan-shaped deposit formed where a fast flowing stream flattens, slows, and spreads typically at the exit of a canyon onto a flatter plain. (en)
foaf:name
  • Bourne (en)
name
  • Bourne (en)
geo:lat
geo:long
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Bourne_SSSI,_Avon.jpg
dct:subject
Wikipage page ID
Wikipage revision ID
Link from a Wikipage to another Wikipage
sameAs
dbp:wikiPageUsesTemplate
thumbnail
georss:point
  • 51.33674 -2.7421
has abstract
  • Bourne SSSI, Avon (grid reference ST484600) is an 8.47 hectare geological Site of Special Scientific Interest near the village of Burrington, North Somerset, notified in 1992. This site is of considerable importance because it has provided detailed information upon the composition of a north Mendip Pleistocene alluvial fan. An alluvial fan is a fan-shaped deposit formed where a fast flowing stream flattens, slows, and spreads typically at the exit of a canyon onto a flatter plain. At Bourne sections have shown highly weathered gravels overlain by sandy silts and clay loams, the highest levels in the sequenceshowing evidence of cryoturbation. Two phases of fan sediment deposition were separated by a long period of subaerial weathering, which may represent an interglacial period. (en)
aos
  • Avon (en)
displaymap
  • Somerset (en)
enref
interest
  • Geological (en)
prov:wasDerivedFrom
page length (characters) of wiki page
area total (m2)
interest
  • Geological
foaf:isPrimaryTopicOf
geo:geometry
  • POINT(-2.7421000003815 51.336738586426)
is Link from a Wikipage to another Wikipage of
is Wikipage disambiguates of
is foaf:primaryTopic of
Faceted Search & Find service v1.17_git147 as of Sep 06 2024


Alternative Linked Data Documents: ODE     Content Formats:   [cxml] [csv]     RDF   [text] [turtle] [ld+json] [rdf+json] [rdf+xml]     ODATA   [atom+xml] [odata+json]     Microdata   [microdata+json] [html]    About   
This material is Open Knowledge   W3C Semantic Web Technology [RDF Data] Valid XHTML + RDFa
OpenLink Virtuoso version 08.03.3331 as of Sep 2 2024, on Linux (x86_64-generic-linux-glibc212), Single-Server Edition (378 GB total memory, 58 GB memory in use)
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2024 OpenLink Software