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Connexion

(Article of periodic en Anglais - 1981)

Document title

Ice-pushed Lower and Middle Pleistocene deposits near Rhenen (Kwintelooijen): sedimentary-structural and lithological/granulometrical investigations

Authors(s) and Affiliation(s)

RUEGG G. H. J. ;

Abstract

In the Kwintelooijen sandpit, located in the inside of a large ice-pushed ridge, a number of thrust sheets are exposed which were formed by pushing inland ice during the Saalian glacial time. In these glaciotectonic units periglacial and fluvial Lower Pleistocene deposits fluvial middle Pleistocene deposits and fluvial mass flow and alluvial fan Saalian deposits are involved. The most complete thrust sheets are up to 25 m thick.

Source

Article of periodic

published at : Mededelingen van de Rijks geologische Dienst Haarlem

Editor :

Millesime : 1981, vol. 35, no2-7 [pp. 165-177]

Bibliographic references : 34 réf.

Language

Anglais

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