Code
NUNASC
Status
Formal (Weerts 2003).
Lithologische beschrijving
Light yellow to grey very fine to fine sand, calcareous, locally shelly. Thin intercalated palaeosols or peat layers at different levels. Common large-scale cross-bedding.
Afzettingsmilieu
Coastal dune (aeolian), interdune swale (pond).
Definitie ondergrens
Base may be marked by shells. Sharp but commonly conformable contact with beach sand (Zandvoort Member, Naaldwijk Formation). Inland, unconformable contact with clastic tidal deposits (Wormer and Walcheren Members, Naaldwijk Formation) or with peat (Hollandveen Member, Nieuwkoop Formation).
Definitie bovengrens
Commonly exposed at the surface. Inland, partly overlain by clastic tidal deposits (Wormer and Walcheren Members, Naaldwijk Formation) or by peat (Hollandveen Member, Nieuwkoop Formation).
Dikte indicatie
Up to about 50 m (where dunes are highest, near Schoorl).
Geografische verbreiding
Up to about 5-km-wide belt along the Dutch North Sea coast.
Regionale correlatie
North Sea: not present; UK: British Coastal Deposits Group with the North Denes Formation (McMillan et al. 2011); GER: Küstenholozän (Barckhausen et al. 1977; Preuss, 1979); BEL: De Panne Member, Vlaanderen Formation (Gullentops et al. 2001).
Ouderdom
Holocene (Northgrippian - Meghalayan).
Holostratotype
Well:
B19A1113 (Schoorl)
Depth (thickness) AH:
0 - 5.6 m (5.6 m) below land surface
Oorsprong naam
Named after the village of Schoorl, northwest of Amsterdam.
Vorige benaming(en)
Younger Dune Deposits (Doppert et al. 1975).
Gereviewed door (datum)
Wim Dubelaar (2018), Sytze van Heteren (2019).
Referenties
Barckhausen, J., Preuss, H., Streif, H.-J. 1977. Ein lithologisches Ordnungsprinzip für das Küstenholozän und seine Darstellung in Form van Profiltypen. Geologisches Jahrbuch Reihe A 44, 45-77.
Doppert, J.W.Chr., Ruegg, G.H.J., Van Staalduinen, C.J., Zagwijn, W.H., Zandstra, J.G. 1975. Formaties van het Kwartair en Boven-Tertiair in Nederland. In: Zagwijn, W.H., Van Staalduinen, C.J. (eds.): Toelichting bij geologische overzichtskaarten van Nederland. Rijks Geologische Dienst, Haarlem, 11-56.
Gullentops, F., Bogemans, F., De Moor, G., Paulissen, E., Pissart, A. 2001. Quaternary lithostratigraphic units (Belgium). In: Bultynck, P., Dejonghe, L. (eds.), Guide to a revised lithostratigraphic scale of Belgium, Geologica Belgica, 4/1-2, 153-164.
McMillan, A.A., Hamblin, R.J.O., Merritt, J.W. 2011. A lithostratigraphical framework for onshore Quaternary and Neogene (Tertiary) superficial deposits of Great Britain and the Isle of Man. British Geological Survey Research Report, RR/10/03, 343 p.
Preuss, H. 1979. Die Holozäne Entwicklung der Nordseeküste im Gebiet der östlichen Wesermarsch. Geologisches Jahrbuch Reihe A 53, 3-84.
Weerts, H.J.T. 2003. Beschrijving lithostratigrafische eenheid. Nederlands Instituut voor Toegepaste Geowetenschappen TNO. Utrecht.
Cite as
TNO-GDN ([YEAR]). Schoorl Member. In: Stratigraphic Nomenclature of the Netherlands, TNO – Geological Survey of the Netherlands. Accessed on [DATE] from http://acc.dinoloket.nl/en/stratigraphic-nomenclature/schoorl-member.