and/or biochemical, mainly aragonitic, precipitations. In the western part occur abundant sheet-flood detritus while gypsum precipitates within an algal mat which develops both in the intertidal and in the infratidal zones. Thus, algal mats are not absolute
The relations between the circulation of subterranean waters and the formation of Karst are as a matter of fact different. The Slovak territory is by its geographical position, geological and morphological structure a classic region for the study
The open space is generally public, multi-purpose and standardized, accessible to everyone. What matters is not that the urban space should have formal values, but that it should be a place for living, a living space. For this, there must be special
, exchange capacity, base saturation and organic matter status. A procedure is described for the actual evaluation. Similar results are obtained when relative limitation scale or a numerical parametric approach is used.
mechanism is effected by geosynergetic processes and their internal and external matter and energy exchange. The concept of geo-systems of the geographic landscape research employs the characteristics of these systems, calling for an aspect-confined
the subtransluscent to opaque matter in these composites, which principally represent actual rock fragments. This suggests that the sediments investigated contain products of rather freshly disintegrated rocks. The opaque components enable2 important groups of rocks
In experimental plots, annual losses of organic and inorganic matter in liquids and solids washed away are very low (e. g. Under beets: in 1975, kg/ha: KO: 1,1| CaO: 3,8, MgO: 0,6| NaO: 2,1| N: 0,4| SO: 2,1| PO: 0,4). During rather long periods
conception which is questionable in matter of urban geography. Does resorting to structuralism and its methods allow to avoid this mythology? To what extent does the analysis of the social standards, granted and handed down, account for the making up
and indirect data. Geological maps are divided on subject-matter basis into the following types: geologic maps, stratigraphic maps, tectonic maps, palinspatic maps and paleogeographic maps, hydrogeological maps, engineering geology maps, geochemical maps