Jurassic carbonate depositional systems of the Mt. Catria-Mt. Acuto area (Umbria-Marche Apennines, Italy)
A geologic survey, integrated with sedimentalogic observations and macrofacies analysis, has been carried out for the Jurassic deposits outcropping in the Mt. Catria - Mt. Acuto area. The study area is located within the northern Umbria-Marche
of the area. The data obtained allowed for the identification of two isolated, uplifted blocks of the carbonate platform (Corno di Catria and Mt. Acuto), reduced in size, bounded by escarpments of tectonic origin and separated by a narrow Jurassic basinal area
Sucasné exogénne reliéfotvorné procezy Dumbierskych Tatier. (The present day exogenic morphogenetic processes in the Dumbier Tatra Mts.)
Information on the research of the present exogenic morphogenetic processes in the Dumbier Tatra Mts which are the highest part of Low Tatra Mts. (Central Slovakia). Processes are described in the individual geoecological types of the investigated
A Bükk szerkezet-és felszinfejlodésének vazlata. (An outline of structural and geomorphological development of Bükk Mts)
Bükk Mts can be classified as young formation of Alpine structural features and shows the pecularities of denuded plateaus and block-mountains composed by sedimentary, igneous and eruptive rocks and ophiolites. (CK).
Vybrané aspekty obrazu podmalokarpatskych miest. (Selected aspects of towns image under the Malé Karpaty Mts.)
A comparative analysis of the geographical image of Jur, Pezinok and Modra, three small towns under the Malé Karpaty Mts near Bratislava, the capital of Slovakia. Results of the research serve as a basis for planning to achieve better symbiosis
The Quaternary sculpturing of sandstones in the Rusavská hornatina Mts.
An analysis of rock landforms in the NW part of the Hostýn Hills. Periglacial and land forms are formed in the Pleistocene and in the Holocene, in the relationship among rock landforms, geological and climate conditions in the Rusavská hornatina Mts
Macrolepidopterous Moth fauna on a volcano Mt. Usu six years after the 1977-78 eruptions
In total 4747 samples of 329 macrolepidopterous moth species were obtained in the surveys conducted at Yosomi Hill and at the crater basin of Mt. Usu in 1984. The level of species diversity was almost the same throughout all seasons. - (SGA)
The bee fauna was surveyed on and around Mt. Usu in 1984, six years after the 1977-78 eruptions of this volcano which has caused faunal and vegetational damage especially around the mountaintop area. In total 46 species of 6 families were obtained
Ground beetles on Mt. Usu six years after the 1977-78 eruptions
Survey made of the ground beetles on and around Mt. Usu which had suffered vegetational damage from volcanic eruptions in 1977-78. A total of 2485 specimens of 29 species were collected.
Mud and debris flows on Mt. Usu after the 1977-1978 eruption
Post-eruption erosion in the world is summarized, and the characteristics of mud and debris flows after the 1977-1978 eruption of Mt. Usu are discussed and its process of time-spatial sequence is explained.
Channel subsystems in the Polish Tatra Mts. are isolated from the slope systems and they characterize by the high vertical and horizontal stability. The stream channels eroded in the moraine and glacio-fluvial deposits are the most stabile
Some characteristics of alpine permafrost, Mt. Daisetsu, central Hokkaido, northern Japan
Alpine permafrost occurs on the flat summit of Mt. Daisetsu, which is located in central Hokkaido at an altitude of 2.200 m a.s.l. Under present climatic conditions, the ground surface temperature is one of the major controlling factors
in the distribution of permafrost on Mt. Daisetsu. The contraction cracking process was examined in a quantitative manner based on the results of both field and laboratory experiments. The depth of permafrost was estimated by geo-electric resistivity survey.
The DEM of Mt. Etna : geomorphological and structural implications
A Digital Elevation Model (DEM) of Mt. Etna is presented. This 3-D view of Mt. Etna allowed both recognition and location of the main morphostructural and volcano-tectonic features of the volcano. A slope map has been generated from the DEM
hydrometeorological characteristics and factors is presented. In the following part are given the regional problems of the Ore Mts., Jizerské Mts., Giant Mts., Beskides, Tatra Mts., South Moravia, East Slovakian Lowlands, the capital of Prague and Bratislava. Further