In the Belianske Tatry Mts the basic part of the rock is formed by stratigraphic units of the Jura chalks of Kriznansky nappe. They are mainly Muran Limestones, marls, nodular limestones, quartzites, Ramsau Dolomites and limestones of Guttenstein layers. In evaluation of the selected part of the area we aimed mainly at investigation of the influence of carbonates on soil forming processes and flora. There arc mentioned the migration of certain macro - and microelements in the system rock - soil - plant.The representation of the elements in single components of the given system has been divided into the categories main, secondary and trace element by semiquantitative analysis. The next step was the selection of the most significant elements from among the elements determined by semiquantitative analysis. They were investigated by quantitative analysis and their representation in the system rock - soil - plant was established. Sample collection for single analyses was realized in the Belianske Tatry Mts in the transect Hlupy vrch hill (2060.8 in a.s.l.) - Kopske sedlo saddle (1750.2 in a.s.l) from different geological-substratum complex. Attention was paid to one plant species (Carex firma) occurring at all sites of the transects. Each pattern (9) was divided into 3 fractions (rock, soil and plant).From among macrobiogeneous elements we aimed at migration of calcium, magnesium, iron, potassium and phosphorus. From among microbiogeneous elements we investigated the movement of manganese, zinc, and from further important elements also nickel, strontium, lead, chromium, cadmium, arsenic, aluminium and cesium.