The paper systematizes morphological forms of alveolar weathering cavities and presents patterns of their evolution. We have studied the forms of tafoni (cavities 2–10 cm in size), which are found in the crags in the Ukrainian Beskydy. The factors that caused the formation of tafoni in our latitudes are humidity and the inherent specificity of selective weathering in sandstones due to structural and textural features formed during the formation of sediments. In winter periods, the role of frost weathering increases. The crags are composed of sandstones of the Yamna suite of the Palaeocene of the Lower Paleogene age. The lithological composition of the sandstones is represented by quartz and feldspar, which allows us to classify them as typical feldspar-quartz sandstones. The cement is clay-siliceous, sometimes with chlorite, of the basal or contact cementation type. In research region tafoni are distributed on rock surfaces in two ways: locally in small areas or covering large areas e.g. whole crag surface of particular aspect. In the first case, the forms are located in small groups of 10–30 pieces in separate parts of a tor wall. In the second case, they occupy the entire plane of the tor surface or half of the surface of particular exposure. Local groups of tafoni can be divided into three shape varieties: 1) vertical bands, 2) horizontal bands, and 3) lenticular bands. Tafoni concentrations that occupy the entire one plane of the tor can be located on it: a) chaotically, b) in a chain-like manner. The following shapes of particular cavities can be distinguished in the Ukrainian Beskydy: 1) rounded, 2) ellipsoid, 3) vertically elongated, and 4) subtriangular. In the Beskyds, the largest length of ellipsoidal cavities is 20–30 cm, the diameter of rounded cavities reaches 10 cm, and the greatest depth is 15 cm. Investigating the morphology of tafoni in the Beskydy, we distinguished the following stages of their evolution: emergence – deepening – expansion – merging – degradation – re-emergence. On the walls of the Beskydy tors, one can observe tafonic forms at various stages of evolution. We identified morpho-evolutionary varieties of tafoni: A) with all four clear edges, B) with three clear and one leveled wall, C) with all unclear walls. The confinement of cavities to slope exposures was also investigated. Cavities in the Carpathians develop more actively on walls of warm exposures than on cold ones. Tafoni forms on tors, their morphology, evolution and formation factors can be the subject of expert interpretations during geotourism excursions. Key words: cavities, tafoni; morphology, evolution, alveolar weathering; tors; Beskydy, Ukrainian Carpathians.
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