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Regularities of mountain geosystems
Altitudinal zonation ; Europe ; Geosystem ; Holocene ; Mountain ; Pleistocene ; Precipitation ; Quaternary ; Temperature
The main features of the mountains are considered and relation with the vertical zonality of temperature and precipitations are observed. Taking into account the mesoclimatic belts in mountain valleys, the diversity of vertical belts and the slope
assymetry in various climatic zones are discussed. Reconstruction of changes of vertical zones in European mountains during the Pleistocene and early Holocene is proposed. - (DG)

Carpathian Mountains ; Holocene ; Mountain ; Palaeogeography ; Poland ; Quaternary

Shifting of climatic vegetation belts in Eurasian mountains and their expression in slope evolution
Eurasia ; Geomorphology ; Glacial features ; Glacier fluctuation ; Inheritated geomorphological features ; Mountain ; Permafrost ; Quaternary ; Slope dynamics ; World
Climatic, vegetation vertical zones controlled mainly by changes in the temperature, shifting in the Quaternary, decide on the rate and direction of slope evolution. In the Eurasian Mountains beside vertical displacement of geomorphic processes
of uplift cause accelerated incision of valleys and large slope failures, it may be more important than the secular processes acting in various climatic vertical zones. The mountain glaciers during advances separate valley sides into supraglacial

The reflection of the Holocene climatic variations in the slope and fluvial deposits and forms in the European mountains

First stages of relief transformation of the young uplifted mountains
The outlined picture of the complexity of influence of positive tectonic movements on the origin and initial stages of relief transformations of mountains, inclines to underline the statement by M. Morisawa (1975) about the composite character, both
the position of base-levels of erosion which, especially in the case of difference in the size of uplifting block, can involve various effects in its later evolution. The regularity of mountain degradation to lag behind upward movements, so distinctive of jump
-type movements, is easily readable on comparing the dissection and lowering of mountains composed of different lithological complexes. Bedrock resistance is of essential importance since it controls the size of slope evolution retardation relative

Earth surface processes ; Geomorphogenesis ; Geosystem ; Inherited features ; Mountain

Carpathians ; Human impact ; Impact study ; Mountain ; Natural environment ; Orogeny ; Poland

Carpathian Mountains ; Holocene ; Poland ; Quaternary ; Sedimentology ; Slope deposit ; Valley ; Valley floor evolution ; Watershed ; Wisła

in extraglacial mountain valleys with changeable flood frequencies and tectonic tendencies. In the middle parts there is a distinct phase of continental climate. In the zone of last glaciation ice marginal streamways were developed in association with superimposed

Erosion ; Flood ; Fluvial dynamics ; Fluvial processes ; Mountain ; Poland ; Runoff ; Slope deposit ; Slope dynamics ; Wisła

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