Results 151 to 160 of about 190 (177)
Abstract The Pleistocene is a key period for understanding the evolutionary history and palaeobiogeography of the European rabbit (Oryctolagus cuniculus). The species was first documented in southeastern Iberia at the beginning of the Middle Pleistocene and appears to have rapidly spread throughout Southwestern Europe, where it was found in numerous ...
Maxime Pelletier
wiley +1 more source
An osteohistological analysis of Triceratops (Ornithischia: Ceratopsidae) cranial ornamentation
Abstract Ceratopsids are among the most distinctive and well known extinct Cretaceous vertebrates, yet many details regarding the growth and composition of their cranial features are still not fully anatomically described or understood. In particular, striking cranial adornments such as the postorbital horns and parietal‐squamosal frill of Triceratops ...
Kyle D. Obuszewski +2 more
wiley +1 more source
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Quaternary Research, 1977
A Pleistocene drift sequence in hummocky terrain along part of the southern Avalon Peninsula of Newfoundland is interpreted to comprise complexly interrelated lodgement till, melt-out till, flow till, supraglacial and proglacial outwash, and supraglacial rhythmites.
Nicholas Eyles, Roger M. Slatt
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A Pleistocene drift sequence in hummocky terrain along part of the southern Avalon Peninsula of Newfoundland is interpreted to comprise complexly interrelated lodgement till, melt-out till, flow till, supraglacial and proglacial outwash, and supraglacial rhythmites.
Nicholas Eyles, Roger M. Slatt
openaire +1 more source
Journal of Geophysical Research: Oceans, 1991
Four Synthetic Aperture Radar (SAR) images were collected during the Labrador Ice Margin Experiment (LIMEX) in March 1989 to study mesoscale ocean features over the Newfoundland shelf. Ice floe movement is detected by displacement in the first two images collected on consecutive days.
M. Ikeda, C. E. Livingstone, I. Peterson
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Four Synthetic Aperture Radar (SAR) images were collected during the Labrador Ice Margin Experiment (LIMEX) in March 1989 to study mesoscale ocean features over the Newfoundland shelf. Ice floe movement is detected by displacement in the first two images collected on consecutive days.
M. Ikeda, C. E. Livingstone, I. Peterson
openaire +1 more source
Late
Palaeoglaciological reconstructions of the North Sea sector of the last British Ice Sheet have, as other shelf areas, suffered from a lack of dates directly related to ice‐front positions. In the present study new high‐resolution TOPAS seismic data, bathymetric records and sediment core data from the Witch Ground Basin, central North Sea, were compiled.
Hans Petter Sejrup +4 more
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Frazil Ice in the Antarctic Marginal Ice Zone
Journal of Marine Science and Engineering, 2021Jörg Schröder +2 more
exaly
Ice-marginal lakes associated with enhanced recession of the Greenland Ice Sheet
Global and Planetary Change, 2021Cassandra Raby +2 more
exaly
Granular effects in sea ice rheology in the marginal ice zone
Philosophical Transactions Series A, Mathematical, Physical, and Engineering Sciences, 2022Agnieszka Herman
exaly
Numerical Study on Wave-Ice Interaction in the Marginal Ice Zone
Journal of Marine Science and Engineering, 2021Tiecheng Wu, Rui Deng, Dapeng Jiang
exaly
Marginal ice zone dynamics: future research perspectives and pathways
Philosophical Transactions Series A, Mathematical, Physical, and Engineering Sciences, 2022Alison Kohout +2 more
exaly

