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A Tokaji-Nagyhegy foldtani fejlodéstorténete és morfogenetikai vazlata. (The geological evolutional history and morphological outlines of the Tokaj-Nagyhegy)

Some conclusions reached at the symposium on geological changes in the western Netherlands during the period 1000-1300 AD

Geological investigations in the centre of Haarlem (The Netherlands) and the development of the river Spaarne

Strukturno-geologiceskaja desifrovka kosmiceskih televizionnyh snimkov (KTS) Balkanskogo poluostrova Structural-geological interpretation of television space images of the Balkan peninsula

Zusammenhänge zwischen geologischem Untergrund und Flozbildung am Beispiel der Braunkohlenlagerstätte Wallendorf. (Connections between geologic underground and formation of seams at the exemple of the Wallendorf brown-coal deposit)
results of the main prospection work led to essential conclusions on the interrelations between the geologic underground formation of seams and coal qualities. Thus it became possible to find out possible areas of brine-breakthrough, to explain deposit

In the monography the principles for definition of geological age of archeological sites are given as well as geological description of the main Paleolithic sites and paleogeographic characteristics of the time of inhabitation of Paleolithic man
. The description is produced for the important regions-West Siberia and Altai, Yenisei river valley, Upper Angara, Upper Lena, West Transbaikalian, Aldan, Far East and North-East. The scheme of geological division of Paleolithic is proposed for mentioned regions.

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

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.

Geomorphological and geological investigations on closed topographic depressions and valley systems on the Drente plateau allow correlations to be made between the location of pingo remnants on the plateau and the Weichselian drainage pattern
. In general, the depth of the remnants varies between 2 and 7m, but locally the geological structure of outcropping sediments is responsible for the development of extremely deep pingo remnants, reaching a maximum of 17m. This figure gives a tentative estimate

Sea-level change and water-level movements in The Netherlands during the Holocene. A contribution to Project 61 of the International Geological Correlation Programme

Tjornes, North Iceland: a bibliographical review of the geological research history

De geologische en mineralogische kartering in België onder het Hollands bewind. in Leven en werken van J.G.S. van Breda (1788-1867).. (The geological and mineralogical mapping of Belgium during the Dutch administration)

Holocene geologische geschiedenis van Centraal en Noordelijk Noord-Holland. (Holocene geological history of the central and northern part of the province of Noord-Holland, The Netherlands)

Archeologische-Geologische kaart van's-Gravenhage, schaal 1:15 000. (Archaeological-geological map of The Hague, The Netherlands, 1:15 000

Geological thinking and mapping in the Netherlands before and during Staring's lifetime

Influence of contrasted rock types and geological structure on solutional processes in North West Yorkshire in Geographical approaches to fluvial processes.

Results of an inventory of the largest deposits as well as the small occurrences of the district undertaken by the Geological Survey of Belgium. A model of the mechanisms of ore concentration and guides for the prospection are proposed. (LW).

Geological composition, paleogeographical development history of the landscape, geomorphological character of the small landscapes together with the climate, hydrology, natural vegetation and soil. (CK).

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