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The Wealden Group, occasionally also referred to as the Wealden Supergroup, is a group (a sequence of rock strata) in the lithostratigraphy of southern England. The Wealden group consists of paralic to continental (freshwater) facies sedimentary rocks of Berriasian to Aptian age and thus forms part of the English Lower Cretaceous. It is composed of alternating sands and clays. The sandy units were deposited in a flood plain of braided rivers, the clays mostly in a lagoonal coastal plain.

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rdfs:label
  • Wealden (Geologie) (de)
  • Wealdien (fr)
  • Wealden-groep (nl)
  • Wealden Group (en)
rdfs:comment
  • De Wealden Group (verouderd, ook wel: Wealden Formation) is een stratigrafische groep, een opeenvolging van gesteentelagen, in de ondergrond van het zuidoosten van Engeland en het zuidwesten van België. De groep bestaat uit tot continentaal (op het land afgezet) sedimentair gesteente met een Valanginien tot Barremien ouderdom (140 tot 125 miljoen jaar oud) en is daarmee deel van het Onder-Krijt van Engeland. De naam Wealden is afkomstig van de regio Weald in Kent, Sussex, Surrey en Hampshire. (nl)
  • Wealden [ˈwiːldən] ist in der regionalen Geologie des westlichen Europas die traditionelle Bezeichnung für im Süß- und Brackwasser abgelagerte Sedimente bzw. die daraus hervorgegangenen Sedimentgesteine der (tieferen) Unterkreide. Der Begriff leitet sich vom Namen der südenglischen Landschaft Weald bzw. des nach dieser benannten Bezirks Wealden ab. Er wurde bereits vom englischen Geologie-Pionier William Smith an der Wende vom 18. zum 19. Jahrhundert benutzt. (de)
  • Le Wealdien ou faciès wealdien (Weald ou Wealden facies en anglais) est un ensemble de faciès d’alternances de grès, de sables et d’argiles d'environnement continental à paralique. Il est daté du Berriasien supérieur au Barrémien et localement jusqu’à l’Aptien supérieur (Crétacé inférieur). (fr)
  • The Wealden Group, occasionally also referred to as the Wealden Supergroup, is a group (a sequence of rock strata) in the lithostratigraphy of southern England. The Wealden group consists of paralic to continental (freshwater) facies sedimentary rocks of Berriasian to Aptian age and thus forms part of the English Lower Cretaceous. It is composed of alternating sands and clays. The sandy units were deposited in a flood plain of braided rivers, the clays mostly in a lagoonal coastal plain. (en)
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  • Wealden Group (en)
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