Results 101 to 110 of about 4,167 (219)
An outcrop of Eemian and Early Weichselian deposits at Beernem (N.W. Belgium) [PDF]
The authors study the sedimentological and paleobotanical characteristics of a continuous succession of Eemian and Weichselian deposits older than 50.000 y, B.F.
De Moor, G., De Groote, V., Heyse, I.
core
A lacustrine sediment core from Fiddaun, western Ireland was studied to reconstruct summer temperature changes during the Weichselian Lateglacial. This site is located close to the Atlantic Ocean; and so is potentially sensitive to climatic changes ...
Hoek, Wirri Z. +13 more
core +1 more source
The extreme yet transient nature of glacial erosion. [PDF]
Patton H +10 more
europepmc +1 more source
Palaeovegetation and environment during Weichselian stadials and interstadials at Mamontovaya Kurja and Sokolova in the Pechora basin, northern Russia [PDF]
The vegetation and climate history of the Pechora area of northwestern Russia during the Early- and Mid Weichselian have been studied. Sediments from two sites have been analysed in this study; from Sokolova and Mamontovaya Kurja.
Halvorsen, Lene S.
core
Fluvial processes under late Pleni-Weichselian environmental conditions: a case study from the Warenka site in central Poland [PDF]
Strong aggradational tendencies during the late Pleni-Weichselian have been noted in river valleys in central Europe. Thick series of mineral deposits were laid down, but also organic or mineral-organic horizons were formed under favourable conditions ...
Pawłowski, Dominik +3 more
core +1 more source
Thick sandy‑silty saprolites occur on some plateaus and lower areas of the Lofoten‑Vesterålen islands. Their location and their thickness (up to 8 m) suggest a pre‑Weichselian or pre‑glacial origin.
Jean-Pierre Peulvast
doaj
Late Pleistocene Expansion of Small Murid Rodents across the Palearctic in Relation to the Past Environmental Changes. [PDF]
Kozyra K +6 more
europepmc +1 more source

