About: Woburn Sands Formation     Goto   Sponge   NotDistinct   Permalink

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The Woburn Sands Formation is a geological formation in England. Part of the Lower Greensand Group, it is the only unit of the group where it occurs, and thus is sometimes simply referred to as the 'Lower Greensand' in these areas. It was deposited during the late Aptian to early Albian stages of the Early Cretaceous. The lithology consists of sandstone or loose sand with rare wisps or thin seams of clay. The formation was extensively exploited in the 19th century for the "coprolite industry", with coprolite being a local term referring to phosphate nodules of varying origins (often the internal moulds of shells), named due to their resemblance to real coprolites. The formation contains reworked fossils of late Tithonian-Berriasian age from deposits that are no longer found locally, equiva

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rdf:type
rdfs:label
  • Woburn Sands Formation (en)
rdfs:comment
  • The Woburn Sands Formation is a geological formation in England. Part of the Lower Greensand Group, it is the only unit of the group where it occurs, and thus is sometimes simply referred to as the 'Lower Greensand' in these areas. It was deposited during the late Aptian to early Albian stages of the Early Cretaceous. The lithology consists of sandstone or loose sand with rare wisps or thin seams of clay. The formation was extensively exploited in the 19th century for the "coprolite industry", with coprolite being a local term referring to phosphate nodules of varying origins (often the internal moulds of shells), named due to their resemblance to real coprolites. The formation contains reworked fossils of late Tithonian-Berriasian age from deposits that are no longer found locally, equiva (en)
name
  • Woburn Sands Formation (en)
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Wikipage page ID
Wikipage revision ID
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sameAs
underlies
unitof
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period
  • Aptian (en)
region
Thickness
  • up to (en)
type
georss:point
  • 52.036 -0.3906
has abstract
  • The Woburn Sands Formation is a geological formation in England. Part of the Lower Greensand Group, it is the only unit of the group where it occurs, and thus is sometimes simply referred to as the 'Lower Greensand' in these areas. It was deposited during the late Aptian to early Albian stages of the Early Cretaceous. The lithology consists of sandstone or loose sand with rare wisps or thin seams of clay. The formation was extensively exploited in the 19th century for the "coprolite industry", with coprolite being a local term referring to phosphate nodules of varying origins (often the internal moulds of shells), named due to their resemblance to real coprolites. The formation contains reworked fossils of late Tithonian-Berriasian age from deposits that are no longer found locally, equivalent in age to the in Norfolk and the Spilsby Sandstone of Lincolnshire, these include Dicranodonta and the ammonite . Reworked dinosaur material is known from the Potton locality within the formation. (en)
extent
location ts
  • Disused fuller's earth workings between Woburn Sands and Woburn (en)
namedfor
otherlithology
overlies
  • Jurassic or older rocks, usually mudstones of the Ancholme Group like the Oxford Clay, Kimmeridge Clay and Ampthill Clay (en)
prilithology
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page length (characters) of wiki page
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  • POINT(-0.39059999585152 52.035999298096)
is Link from a Wikipage to another Wikipage of
is Wikipage redirect of
is foaf:primaryTopic of
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