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.
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.
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)
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).
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
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
Basing on measurements of the sheet wash performed from 1969 to 1975 the most important indices of the geological activity of the process were quantitatively evaluated. A general amount of the sheet wash into Lake Baikal is estimated to be 722 tons