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Stratigraphic and morphologic constraints on the Weichselian glacial history of northern Prins Karls Forland, western Svalbard
  • Stratigraphic and morphologic constraints on the Weichselian glacial history of northern Prins Karls Forland, western Svalbard
  • This paper reports stratigraphic and morphologic data from the Mc Vitiepynten area, northern Prins Karl Forland that further constrain the Weichselian glacial history of Prins Karls Forland and highlight the question of the westward extension
  • of the Barents Sea ice sheet. The results indicate similar environmental histories for central and northern Prins Karls Forland. It is concluded that during the period c. 70 to 10 ka, northern Prins Karls Forland experienced cold subaerial polar desert conditions
Use of Ground Penetrating Radar (GPR) soundings for investigating internal structures in rock glaciers. Examples from Prins Karls Forland, Svalbard.
  • Use of Ground Penetrating Radar (GPR) soundings for investigating internal structures in rock glaciers. Examples from Prins Karls Forland, Svalbard.
  • Arctique ; Glacier ; Glacier rocheux ; Ground Penetrating Radar ; Méthodologie ; Norvège ; Prins Karls Forland ; Radar ; Structure géologique ; Svalbard ; Technique de recherche
  • Les AA. présentent les quatre profils de glaciers rocheux obtenus par la méthode du GPR (Ground Penetrating Radar) au Svalbard à Prins Karls Forland (Norvège). Ils débattent des possibilités offertes par cette méthode pour étudier la structure
Rock glaciers on Prins Karls Forland, Svalbard. I : internal structure, flow velocity and morphology
  • Rock glaciers on Prins Karls Forland, Svalbard. I : internal structure, flow velocity and morphology
  • Etude des glaciers rocheux (structure, vitesse, morphologie) sur l'île Prins Karls Forland, dans le Svalbard occidental. Dans la partie nord-ouest de l'île, des glaciers rocheux lobés constituent une transition continue entre la falaise rocheuse et
Rock glaciers on Prins Karls Forland. II : GPR soundings and the development of internal structures
  • Rock glaciers on Prins Karls Forland. II : GPR soundings and the development of internal structures
  • les structures internes de 4 glaciers rocheux de la zone du pergélisol continu sur l'île Prins Karls Forland, Svalbard occidental, ont été étudiées en utilisant un radar dont les ondes pénètrent le sol (GPR). Une étude comparative a été réalisée sur
Holocene rockwall retreat and the estimation of rock glacier age, Prins Karls Forland
  • Holocene rockwall retreat and the estimation of rock glacier age, Prins Karls Forland
  • glacier transition zone. The model was applied to 2 rock glaciers at Prins Karls Forland, Svalbard. The main goal of the model is to produce a reasonable estimate of rock glacier initiation age and corresponding rockwall retreat rates, based on geometrical
The rock glaciers on Prins Karls Forland : corrections of surface displacement rates
  • The rock glaciers on Prins Karls Forland : corrections of surface displacement rates
Inuit landscape use and responses to climate change in the Wollaston Forland – Clavering Ø region, Northeast Greenland
  • Inuit landscape use and responses to climate change in the Wollaston Forland – Clavering Ø region, Northeast Greenland
Faunal Remains from the Wollaston Forland – Clavering Ø region, Northeast Greenland – Thule culture subsistence in a high Arctic polynya and ice-edge habitat
  • Faunal Remains from the Wollaston Forland – Clavering Ø region, Northeast Greenland – Thule culture subsistence in a high Arctic polynya and ice-edge habitat
  • The GeoArk project conducted interdisciplinary studies between 2003 and 2008 to investigate the Thule culture (c. 1400 AD until c. 1850 AD) in the Wollaston Forland – Clavering Ø region (74°N). Faunal remains of recent excavations and re-analyses
Durée du manteau nival en Europe du Nord
  • FORLAND, È.
Icings and their geomorphological significance exemplified from Oscar II Land and Prins Karl Forland, Svalbard in Results of investigations of the Second Torun polar expedition, Spitsbergen-1977 and Third Torun polar expedition, Spitsbergen 1978.
  • Icings and their geomorphological significance exemplified from Oscar II Land and Prins Karl Forland, Svalbard in Results of investigations of the Second Torun polar expedition, Spitsbergen-1977 and Third Torun polar expedition, Spitsbergen 1978.
In search of Thule children : construction of playinghouses as a means of socializing children
  • This paper examines the miniature playhouse structures of Thule children that date from the pre-contact Thule period of approximately 1400-1800 AD. Implemented during the 2008 field season, the study explored the region of Wollaston Forland
Durée du manteau nival stable au nord de l'Eurasie dans les conditions des changements climatiques actuels
  • FORLAND, È.
Lichen growth rates on glacier forelands in southern Norway : preliminary results from a 25-year monitoring programme
  • A unique 25-year lichen growth monitoring programme involving 2,795 individuals of the Rhizocarpon subgenus at 47 sites on 18 glacier forlands in the Jotunheimen-Jostedalsbreen regions is reported. Relating to direct lichenometry, the AA. study
Exemple de croquis géomorphologique synthétique appliqué au strandflat nord-est de l'île du Prince Charles (Svalbard)
  • Arctique ; Carte ; Carte synthétique ; Cartographie ; Croquis géomorphologique ; Dynamique de versant ; Estran rocheux ; Généralités sur la géographie ; Géomorphologie ; Ile ; Lagune ; Littoral ; Prins Karls forland ; Sol ; Strandflat ; Svalbard