Solr Search · GéoProdig, portail d'information géographique

An outline of the geological structure of the Northeastern Hohes Venn Area and of its Northern foreland
Lower Paleozoic (Cambrian, Ordovician), Devonian, and Carboniferous sedimentary rocks are exposed in the northeastern part of the Hohes Venn area (Northern Eifel) and in its northern forelands. The regional geological development represented
by these sediments and their Caledonian and Variscan structural characteristics are obtained from geological profiles across the Eifel's northern boundary zone.
1985

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
1985

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.
1985

Carte géologique internationale de l'Afrique = International geological map of Africa. Feuille 3.
1985

A morahalmi Madarasz-to foldtani és vizfoldtani viszonyai. (The geological and hydrogeological conditions of Lake Madarasz near Morahalom)
1985

The economic geological importance of the lignite at the foreland of the Northern Hungarian Uplands in Problems of the Neogene and Quaternary in the Carpathian Basin.
1985

Philosophie und Geologie. Beiträge zum III. DDR-UdSSR-Symposium zur Geschichte der geologischen Wissenschaften.. (Philosophy and geology. Papers of the third GDR-USSR-Symposium on History of geological sciences)
1985

Toelichting bij de Geologische kaart van Nederland 1: 50 000. Blad Eindhoven West (51 W).. (Explanation to the Geological map of the Netherlands 1: 50 000. Sheet Eindhoven West (51 W)
1985

A volume for the 8th Congress of the Regional Committee on Mediterranean Neogene stratigraphy, Budapest, September 1985. The study of the conditions and rate of deposition of the several thousand metres of Neogene and Quaternary sediments
in the Great Hungarian Plain and the denudation chronology of the Hungarian Mountains are studied with the application of geological, sedimentological, stratigraphical, paleontological and geomorphological methods and various absolute dating techniques. DLO).
1985

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).
1985

The well known Clovis and Plainview paleo-indian sites of New Mexico and Texas have yielded new data on regional late Quaternary geologic, paleoclimatic, and pedologic histories.
1985

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
1985

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
1985

Geological and palynological investigations of two main dune systems west of Nieuwpoort. The Old Dune system is believed to be older than 4300 B.P. The Young Dune area has a complex history: older dunes (2800-900 B.P.) underneath the Young Dune
1985

, 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
1985

Since 1973 geologists from the GDR have been involved in geologic activities in Antarctica included in the SCAR program. As participants of Soviet Antarctic expeditions they have generally dealt with problems of structural geology in selected
1985

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
1985

South of Budapest, the Danube formed a loess bluff of 30 to 50 m height along 180 km length, where landslides are frequent. Observations underline the role of infiltration above the impervious layer and the reduction of spring activity. Geological
1985

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