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Breda Formation

The Breda Formation (Dutch: Formatie van Breda; abbreviation: BR) is a geologic formation in the subsurface of the Netherlands. The formation consists of marine glauconiferous sands and clays that were deposited during the Miocene epoch. Although the formation is not very rich in fossils, sometimes bones of fishes, mammals (Leptophoca cf. proxima, Protophocaena minima),[1] shells and shark teeth (a.o of megalodon) are found.

Breda Formation
Stratigraphic range: Chattian-Pliocene
~28–3.6 Ma
TypeGeological formation
Unit ofUpper North Sea Group
Sub-unitsAalten Mb., Delden Mb., Eibergen Mb., Zenderen Mb.
UnderliesOosterhout Fm., Kiezeloolite Fm.
OverliesRupel Fm., Veldhoven Fm.
Thicknessup to more than 700 m (2,300 ft)
Lithology
PrimaryMarine sandstones and clays
OtherConglomerate
Location
RegionEurope
Country Netherlands
Type section
Named forBreda (North Brabant)

Stratigraphy and lithology edit

The Breda Formation was deposited in the shallow sea that covered the Netherlands during the Miocene. It is mostly on top of the Oligocene clays of the Rupel Formation or late Oligocene sands and clays of the Veldhoven Formation. The Breda Formation can be a couple of meters (in the Roerdal Graben) to more than 700 metres (2,300 ft) thick. The top is formed by an erosional disconformity in the south and east of the Netherlands. In the west the contact with the Pliocene Oosterhout Formation is more gradual. In the Roerdal Graben the mostly Pliocene Kiezeloolite Formation is sometimes on top of the Breda Formation.

Locally the Breda Formation can be subdivided into members: the Aalten Member (silty calcareous clay, rich in shells), the Eibergen Member (clay alternating with thin sand layers, with a basal conglomerate in which shark teeth and whale bones were found), the Zenderen Member (green, glauconiferous fine sand) and the Delden Member (sandy, glauconite and goethite bearing clay and loam.

The Breda Formation corresponds largely with the Berchem Formation of northern Belgium.

References edit

  1. ^ Liessel at Fossilworks.org

Bibliography edit

  • Doppert, J.W.C.; Ruegg, G.H.J.; Staalduinen, C.J. van; Zagwijn, W.H. & Zandstra, J.G.; 1975: Formaties van het Kwartair en Boven-Tertiair in Nederland, in: Zagwijn, W.H. & Staalduinen, C.J. van (eds.): Toelichting bij geologische overzichtskaarten van Nederland, Rijks Geologische Dienst, Haarlem, pp. 11–56. ((in Dutch))

External links edit

  • Westerhoff, W.E.; 2003: Formatie van Breda, TNO website (in Dutch)

breda, formation, dutch, formatie, breda, abbreviation, geologic, formation, subsurface, netherlands, formation, consists, marine, glauconiferous, sands, clays, that, were, deposited, during, miocene, epoch, although, formation, very, rich, fossils, sometimes,. The Breda Formation Dutch Formatie van Breda abbreviation BR is a geologic formation in the subsurface of the Netherlands The formation consists of marine glauconiferous sands and clays that were deposited during the Miocene epoch Although the formation is not very rich in fossils sometimes bones of fishes mammals Leptophoca cf proxima Protophocaena minima 1 shells and shark teeth a o of megalodon are found Breda FormationStratigraphic range Chattian Pliocene 28 3 6 Ma PreꞒ Ꞓ O S D C P T J K Pg NTypeGeological formationUnit ofUpper North Sea GroupSub unitsAalten Mb Delden Mb Eibergen Mb Zenderen Mb UnderliesOosterhout Fm Kiezeloolite Fm OverliesRupel Fm Veldhoven Fm Thicknessup to more than 700 m 2 300 ft LithologyPrimaryMarine sandstones and claysOtherConglomerateLocationRegionEuropeCountry NetherlandsType sectionNamed forBreda North Brabant Contents 1 Stratigraphy and lithology 2 References 2 1 Bibliography 3 External linksStratigraphy and lithology editThe Breda Formation was deposited in the shallow sea that covered the Netherlands during the Miocene It is mostly on top of the Oligocene clays of the Rupel Formation or late Oligocene sands and clays of the Veldhoven Formation The Breda Formation can be a couple of meters in the Roerdal Graben to more than 700 metres 2 300 ft thick The top is formed by an erosional disconformity in the south and east of the Netherlands In the west the contact with the Pliocene Oosterhout Formation is more gradual In the Roerdal Graben the mostly Pliocene Kiezeloolite Formation is sometimes on top of the Breda Formation Locally the Breda Formation can be subdivided into members the Aalten Member silty calcareous clay rich in shells the Eibergen Member clay alternating with thin sand layers with a basal conglomerate in which shark teeth and whale bones were found the Zenderen Member green glauconiferous fine sand and the Delden Member sandy glauconite and goethite bearing clay and loam The Breda Formation corresponds largely with the Berchem Formation of northern Belgium References edit Liessel at Fossilworks org Bibliography edit Doppert J W C Ruegg G H J Staalduinen C J van Zagwijn W H amp Zandstra J G 1975 Formaties van het Kwartair en Boven Tertiair in Nederland in Zagwijn W H amp Staalduinen C J van eds Toelichting bij geologische overzichtskaarten van Nederland Rijks Geologische Dienst Haarlem pp 11 56 in Dutch External links editWesterhoff W E 2003 Formatie van Breda TNO website in Dutch Retrieved from https en wikipedia org w index php title Breda Formation amp oldid 1193159121, wikipedia, wiki, book, books, library,

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