Geological models for the configuration, history and style of disintegration of the Laurentide ice sheet in Models in geomorphology.
Presents models derived from current glacial geological information on three aspects of the Laurentide ice sheet : its configuration and centers of outflow| the latter part of its history of waxing and Waning and the style of its final deterioration
Simulation of the climate of 18,000 years BP : results for the North America/North Atlantic/European sector and comparison with the geologic record of North America
temperature were prescribed from CLIMAP (1981). The geologic evidence is generally compatible with the model simulation.
Based on a joint analysis of molluscs, ostracods and mammals as well as available geological and paleogeographical information, an attempt was made to correlate the Pannonian sediments with those of Eastern and Mediterranean. DLO).
A correlation is analysed between strength characteristics of solid rocks and selective weathering processes, field observation data being used from an alpine area in Central Tien-Shan. Geological and geomorphological survey revealed coincidence
The term biosphere is elucidated in the light of the Earth's geological history, and the basic requirements for active life processes such as temperature and water as well as the factors involved in interspecific competition such as growth, light
, melts of probably intermediate composition were let off into the crust, where the crust segment of the Erzgebierge-Fichtelgebirge anticlinale has been concerned very much. This model conception is strongly confirmed by several geophysical, geologic
The question of whether a possible landbridge (s) existed between Britain and Ireland during Devensian (Midlandian) Late-glacial and Holocene time is analysed in the light of new geological and related environmental information. If any landbridge
Thermoluminescence dating of Pleistocene sediments. A review and some preliminary results on sand formations from Brazil in Quaternary of South America and Antarctic Peninsula. Vol. 3 (1985). With selected papers of the international symposium
Results are presented for the thermoluminescence behaviour of sands from various geological contexts in Brazil. They show that the coarse ( 100-200 m) quartz fraction of coastal and intra-continental, eolian and fluvial-type deposits, might