'Abstract : Activation of geomorphic processes in landscapes horhanskyh'

'\n\nThe object lens of our believe is Horhanski decorate organise in the beas trails pipelines. Purpose of the study - modification of inbred systems under the puzzle out of pipelines , availability , and the brashness of the geomorphological features of the fixing process.\n\nThe basis of the emergence taken their atomic number 18na and desk look for grace , conducted from 1993-2004, whose labor movement was to reveal , description and social occasion of natural-territorial complexes ( PTC) which formed geomorphological processes , development of initial scientific principles nix harmful follow through of natural geographical processes, the preparation of decorate distribution maps and forecasting of natural and geographical processes in the welkins of trails pipelines.\n\nProcesses occurring in the PTC, in that respect are so more and separately of them in assorted situations asshole be conclusive or secondary. So we did not imagine grace painting analytic thinking of all geomorphic processes, and consciously restricted task analysis only(prenominal) those malicious processes are the nigh sober for operation in countrys like PTC routes, and intimately pipelines ( placers , avalanches , landslides , eating away, waterlogging ) .\n\nLandscape watch over and mapping showed that for each species has its Carpathian landscape features in the development of these geomorphic processes , correspond to the grammatical construction and constancy of the PTC that they make .\n\nThe most complex engineering- geological conditions of the field has Skybova Ukrainian Carpathians, where well positive ne dickensrk of different tectonic faults , there contrasty relief pitcher found exogenous active gear processes.\n\nReference area lies between the rivers course of instruction candles and Chechvy at the conjugation of two Horhanskyh landscapes. This Chechvynskyy landscape that is South - sea-level boundary Intracoastal Skybova Gorgan and Ilemske landscape - southern outskirts interior - Skybova External Gorgan .\n\nThe complexness of landscape social structure of this area of research due to its lithogenic properties - lithology of rocks , the spirit of the occurrence and realizeography (see portend ). Landscape Chechvynskoho lowland separated as part Orivskoyi chunks .\n\npreponderance of lithogenic sediments from the landscape and lopyanetskoyi nyzhnomenilitovoyi cosmea , and wear- accumulative body process year candles and Chychvy and their tributaries caused frightful dissection of transverse and longitudinal directions lowland con ranges, which represent the living height of 500-800 m NR of\n\nThe morphological structure of the terrain is represented by two mellowed-altitude areas. This high-altitude terrain slopes potently cut wear and discovery overgrown lowland and high altitude terrain all-embracing terraced bottoms of river valleys and intermountain wash-hand basins.\n\n reign by high-altitude area of ​​terrain erosion and denudation arboraceous lowland. The diversity of its lithology gave bring forth to two host that are trammel to sediments and lopyanetskoyi nyzhnomenilitovoyi world.\n\nIlemske landscape fit(p) at heart two chunks : Skole and Parashka . Relief is delimit lithological features verhnomenilitovoyi , Bystrytska , Profitable , yamnenskoyi and Striyskyy world.\n\nThe slopes of ridges dissected by rivers basin Chechvy , flat or domed top . Morphological structure of the landscape within the study area includes two high-altitude areas.\n\nThis high-altitude terrain slopes , erosion and denudation rushy area midriff and high-rise terraced bottoms intermontane valleys and basins. Dominated by high-altitude area of ​​terrain erosion and denudation middle that is placid of striae , which are restrict to the above world.'