2020
DOI: 10.26471/cjees/2020/015/118
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The Problem of Long-Term Prediction of Landslide Processes Within the Transcarpathian Inner Depression of the Carpathian Region of Ukraine

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Cited by 5 publications
(3 citation statements)
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“…The geological, tectonic, and geomorphological structure are known to be constant factors in the development of landslide processes [Kasiyanchuk et al, Davybida et al, 2018;Shtohryn et al, 2021], as well as the seismic regime of the area and hydrogeological conditions. According to the scheme of regional-zonal engineering-geological zoning by Klymchuk et al, [2008], most of the territory of the Chernivtsi region belongs to the Carpathian mountain-fold system (Ж) [Ponomar, 1969], within which a significant area is occupied by the Preсarpathian depression (Figure 1).…”
Section: Study Areamentioning
confidence: 99%
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“…The geological, tectonic, and geomorphological structure are known to be constant factors in the development of landslide processes [Kasiyanchuk et al, Davybida et al, 2018;Shtohryn et al, 2021], as well as the seismic regime of the area and hydrogeological conditions. According to the scheme of regional-zonal engineering-geological zoning by Klymchuk et al, [2008], most of the territory of the Chernivtsi region belongs to the Carpathian mountain-fold system (Ж) [Ponomar, 1969], within which a significant area is occupied by the Preсarpathian depression (Figure 1).…”
Section: Study Areamentioning
confidence: 99%
“…A long-standing temporal prediction is performed. Then, using the normalized Laplace function, the integral indicator was calculated into the value of the probability of landslide processes [Shtohryn et al, 2020] (3):…”
Section: Solar Activitymentioning
confidence: 99%
“…Factor 2 shows the influence of relief on the development of landslides and is determined by the connection of the parameters "absolute mark" of the landslide "head", "angle of inclination of the daylight surface" of the landslide "head" and "distance to the river". The inverse correlation of the parameter "distance to the river" with the spread of landslides indicates that they develop far from rivers and not only under the influence of spatial conditions: geological, tectonic structure, lithological composition, type of relief, degree of destruction of the upper layer of rocks, but to a large extent, they are also caused by external influences -anomalous values of precipitation [Shtohryn et al, 2020]. As we can see, the geomorphological parameters have a much smaller share of the total dispersion (0.28), so their influence is not determining.…”
Section: Confinedness Of Landslide Processes To the Fault Zonesmentioning
confidence: 99%