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A 9000-year-old ash bed on the Faroe Islands
  • MANGERUD, J.
Aminostratigraphy of European marine interglacial deposits
  • MANGERUD, J.
The glacial history of Norway in Glacial deposits in north-west Europe.
  • MANGERUD, J.
New radiocarbon dates for the Vedde Ash and the Saksunarvatn Ash from Western Norway
  • MANGERUD, J.
The margin of the last Barents-Kara ice sheet at Markhida, northern Russia
  • MANGERUD, J.
Late Weichselian marine C 14 reservoir ages at the western coast of Norway
  • MANGERUD, J.
The Last Glacial Maximum on Spitsbergen, Svalbard
  • MANGERUD, J.
Late Weichselian and Holocene sea-level history for a cross-section of western Norway
  • MANGERUD, J.
Erosion rate of a Younger Dryas cirque glacier at Krakenes, western Norway
  • MANGERUD, J.
Correlation of the Eemian (interglacial) stage and the deep-sea oxygen-isotope stratigraphy
  • MANGERUD, J.
Lake sediments and the lateglacial environment in Northern Scotland
  • Les changements climatiques sont étudiés à partir de diagrammes de pollens et de diatomées pour neuf lacs écossais depuis-13000 et sont confrontés aux subdivisions de Mangerud| on note au début du Bolling le passage à une végétation fermée de lande
Moraine exposure dates imply synchronous Younger Dryas glacier advances in the European Alps and in the Southern Alps of New Zealand
  • 26 concentrations for boulders on the Julier Pass moraines in the Swiss Alps. These exposure dates shox synchronous glacier advances both in the Southern Alps and in the European Alps during the European Younger Dryas chronozone of Mangerud et al.
Reflection of Scandinavian Ice Sheet fluctuations in Norwegian Sea sediments during the past 150,000 years
  • MANGERUD, J.
Diatom stratigraphy related to late Weichselian sea-level changes in Sunnmore, western Norway
  • MANGERUD, J.
A Younger Dryas ash bed in western Norway, and its possible correlations with tephra in cores from the Norwegian Sea and the North Atlantic
  • MANGERUD, J.
The stratigraphic subdivision of the Lateglacial of NW Europe: a discussion in Studies in the Lateglacial of North-West Europe.
  • for the Lateglacial of NW Europe is suggested which encompasses flexibility, simplicity, and accuracy in reflecting the uncertainty of present knowledge. The main purpose of the paper is to stimulate discussion for we agree with Mangerud and Berglund (1978) that NW
Ice-front variations of different parts of the Scandinavian ice sheet, 13,000-10,000 years BP in Studies in the Lateglacial of North-West Europe.
  • MANGERUD, J.