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  • Stratification of Quaternary depositional layers on the southern bank of the Swartspruit near Hartbeespoort Dam, Transvaal
  • Palaeo-environment ; Quaternary ; Sedimentary ; South Africa ; Stratigraphy ; Transvaal
  • 1991
  • The genesis of quaternary landscapes with stone-lines
  • Comparative studies ; Landscape ; Pediment ; Pedogenesis ; Quaternary ; Soil ; Soil evolution ; Subtropical zone ; Theory ; Tropical zone
  • 1991
  • Geomorphologic and lithologic evidence for an expanded mountain ice sheet on Mount Kenya during the early Quaternary
  • The analysis and interpretation of pre-Brunhes (>.73 -.79 my) glacial landforms in the Nithi River Basin, on the eastern flank of Mount Kenya, provide evidence for the dynamics of early Quaternary ice. - (L'A.).
  • 1991
  • Paleoecological and geomorphological evolution in Lower and Middle Belgium during the Late Quaternary
  • Belgium ; Geomorphology ; Palaeo-ecology ; Palaeo-environment ; Quaternary
  • Paleoecological and geomorphological evolution of Low and Middle Belgium in the late Quaternary. - (LW)
  • 1991
  • Late Quaternary pollen records and vegetation history of the southwest Yukon Territory : a review
  • Canada ; Holocene ; Paleo-environment ; Palynology ; Pollen diagrams ; Quaternary ; Vegetation ; Yukon
  • 1991
  • Late Quaternary fluvial sedimentation in the Voidomatis Basin, Epirus, Northwest Greece
  • The aim of this study is to establish the sequence, depositional environments, and ages of Quaternary alluvial, colluvial, and glacial units in the Voidomatis basin.
  • 1991
  • Late Quaternary snowline reconstructions for the Southern and Central Sierra Nevada, California and a reassessment of the « Recess Peak Glaciation »
  • California ; Climatic variation ; Dating ; Glaciation ; Lichenometry ; Paleo-environment ; Quaternary ; Sierra Nevada ; Snow line ; United States
  • 1991
  • Size variation in the Cape Dune Molerat (Bathyergus suillus) and late Quaternary climatic change in the southwestern Cape Province, South Africa
  • Cape Province ; Climatic variation ; Fossil fauna ; Paleo-environment ; Paleobiogeography ; Precipitation ; Quaternary ; Rodents ; South Africa
  • 1991
  • Paleoclimatic implications of late Quaternary lacustrine sediments in Western Nubia, Sudan
  • Climatic variation ; Lacustrine sediment ; Microstructure ; Paleo-environment ; Paleoclimatology ; Quaternary ; Sudan
  • 1991
  • Climatic transfer function from Quaternary molluscs in european loess deposits
  • Alsace ; Europe ; France ; Loess ; Mollusca ; Multivariate analysis ; Paleo-environment ; Paleoclimatology ; Palynology ; Quaternary ; Statistics
  • 1991
  • Aminostratigraphy and electron spin resonance studies of late Quaternary sea level change and coastal neotectonics in Tasmania, Australia
  • Aminostratigraphy ; Australia ; Coastal environment ; Dating ; Neotectonics ; Quaternary ; Sea level ; Tasmania
  • 1991
  • Geomorphological evidence for Quaternary climatic change in the low Sino-Burman Ranges
  • Climatic variation ; Earth surface processes ; Hydrogeology ; Karst ; Paleo-environment ; Quaternary ; Sedimentation ; Structural geomorphology ; Thailand ; Tropical zone
  • 1991
  • On late Quaternary glaciation of the foothill area of the East Kunlun Mountains, West China
  • China ; Deglaciation ; Glacial landform ; Glaciation ; Holocene ; Kame ; Piedmont ; Quaternary ; Terrace
  • 1991
  • The Late Quaternary climate and human impact on aeolian processes in Poland
  • Archeological site ; Eolian features ; Human impact ; Loess ; Paleoclimate ; Paleosols ; Periglacial features ; Poland ; Quaternary
  • Detailed field studies, radiocarbon measurements, palaeobotanical analyses and archaeological finds in sites spread all over Poland show that the late Quaternary aeolian phenomena can be divided into two main groups. The first one is represented
  • 1991
  • Alluvial cone ; Carpathian Mountains ; Fluvial processes ; Fluvioglacial features ; Geomorphogenesis ; Geomorphological map ; Mountain ; Neotectonics ; Poland ; Quaternary ; Terrace
  • The present relief and Quaternary deposits of Orawa Basin give possibility to distinguish two different parts of big complex Czarny Dunajec fan. The western part with 6 levels documents 6 phases of uplift. The eastern part of big fan represent
  • the youngest Late Vistulian and Holocene accumulation environment. Infill of Wróblówka graben is related to the periods of uplift in western part. Maximal amplitude of tectonic movement during Quaternary is 200 m. Thus the evolution consists two stages
  • of subsidence, Neogene and Quaternary. - (DG)
  • 1991
  • Arid land;Arid environment ; Coastal environment ; Fluvial processes ; Namibia ; Quaternary ; River mouth ; Sea level ; Stream ; Tectonics ; Terrace ; Vertical displacement
  • The Quaternary tectonic history of the river mouth region is related to the complex geomorphological features. Evidence on the terraces suggests recent continuous uplift. - (AJC)
  • 1991
  • Comparative uranium-thorium and thermoluminescence dating of weathered Quaternary alluvium in the tropics of Northern Australia
  • 1991
  • Late quaternary aeolian geomorphology of the Dale Lake Sand Sheet, Southern Mojave Desert, California
  • California ; Desert ; Dune ; Eolian deposit ; Eolian features ; Geomorphology ; Grain size distribution;Granulometry ; Lake ; Mineralogy ; Multivariate analysis ; Paleo-environment ; Quartz ; Quaternary ; Sedimentology ; Statistical analysis
  • 1991
  • Quaternary glaciation of the north slope of Karakorum mountains
  • China ; Cirques ; Glacial features ; Glaciation ; Heave ; Karakoram ; Moraines ; Paleogeography ; Pleistocene ; Quaternary ; Tectonics ; Xizáng Zizhiqu
  • 1991
  • On the development of the Late Quaternary river valleys in the Saale-Elbe lowland with emphasis on radio carbon data
  • C 14 dating ; Earth surface processes ; Fluvial dynamics ; Fluvial terrace ; Germany ; Holocene ; Quaternary ; Terrace
  • the Late Quaternary. Hence, it is possible to confirm the Weichselian age of the intact and the reduced low terrace and to record chronostratigraphically the greatly differentiated fluvial dynamics during the Holocene. - (L'A.).
  • 1991