Results 251 to 260 of about 180,240 (308)

Human occupation of the Afroalpine Bale Mountains at the onset of the African Humid Period. [PDF]

Landsc Ecol
Ossendorf G, Tekelemariam MG, Taipale N, Groos AR, Negash A, Cnuts D, Akçar N, Vockenhuber C, Tariku ZK, Kahsay TH, Rots V, Vogelsang R.   +11 more
europepmc   +1 more source

Tectonism rather than "snowball Earth" glaciation is responsible for the Great Unconformity. [PDF]

Proc Natl Acad Sci U S A
Zhan RR, Duan L, Zattin M, Christie-Blick N, Wan B, Wei RH, Yang Z, Wang J, Gou L, Olivetti V, Chen KY, Zhang X.   +11 more
europepmc   +1 more source

Late Miocene Arctic warmth and terrestrial climate recorded by North Greenland speleothems. [PDF]

Nat Geosci
Moseley GE, Koltai G, Baker JL, Wang J, Stoll H, Donner A, Friedrich L, Spötl C, Smith MP, Scholz D, Cheng H, Hartland A, Hejny C, Edwards RL.   +13 more
europepmc   +1 more source

Late Pleniglacial and Late Glacial aeolian phases in The Netherlands

, 1999
openaire   +1 more source

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Last Glacial Maximum, Late Glacial and Holocene of Patagonia

2022
Fil: Coronato, Andrea Maria Josefa. Consejo Nacional de Investigaciones Científicas y Técnicas.
Rabassa, Jorge Oscar, Coronato, Andrea Maria Josefa, Martínez, Oscar Alfredo, Reato, Agustina   +3 more
openaire   +2 more sources

The late proterozoic glacial era

Palaeogeography, Palaeoclimatology, Palaeoecology, 1985
Abstract The Late Proterozoic glacial record is reviewed on a global basis as a setting and introduction for that part of the symposium concerned with West African tillites. No unequivocal glacial deposits have yet been recorded in the interval 1.0–2.0 Ga.
M.J. Hambrey, W.B. Harland
openaire   +1 more source

Glacial and Late Glacial Processes in Western Iceland

Geografiska Annaler: Series A, Physical Geography, 1975
The presence of glacial marine drift, a hybrid deposit containing sub-fossil shells of age about 12,000 years B.P.
openaire   +1 more source

A note on the glacial and late glacial history of caithness

Geological Journal, 1981
AbstractIt is generally accepted that in the last glaciation Scottish ice from the Moray Firth flowed to the northwest across Caithness depositing shelly drift. Examination of striae along the east coast of Caithness shows that some were formed by ice flowing into and not out of the Moray Firth.
openaire   +1 more source

Late glacial and post‐glacial shorelines in north‐east Antrim

Irish Geography, 1965
Abstract not available...
openaire   +1 more source