## 4 Results

Table 4: Ranking in points of the potential impact of geodynamic processes on the environmental state of high-mountain territories and the levels of their manifestation in various geological and geomorphological conditions. \begin{table}
\begin{tabular}{c l c c c c} \hline \hline \multirow{2}{*}{**No.**} & \multirow{2}{*}{**Types of Impact**} & \multicolumn{5}{c}{**Level of Impact**} \\ \cline{3-6}  & & **Weak** & **Middle** & **Hight** & **Regressive** \\ \hline \multirow{2}{*}{7} & Distribution of Quaternary formations at altitude intervals: & 1700–2000 m; 2000–2300 m; 2300–2600 m and above & 1700–2000 & 2000–2300 & 2300–2600 & \textgreater{}2600 \\ \hline \multirow{2}{*}{8} & Soft bedrock (up to 50 MPa), exposure 40\%; 50\%; 60\%; 70\%; or more & 40\% & 50\% & 60\% & \textgreater{}70\% \\ \hline \multirow{2}{*}{9} & Erosion basis 1000 m or more, at altitudes of 2000 and above, taking into account glaciation & 2000–2500 & 2500–3000 & 3300–3500 & 3500–4000 \\ \hline \multirow{2}{*}{10} & Erosion basis 500 m at altitudes of 1500 and above & 1500–1700 & 1700–1800 & 1800–1900 & 1900–2000 \\ \hline \multirow{2}{*}{11} & Erosion basis up to 500 m at altitudes from 1500 m and below & 1300–1500 & 1100–1300 & 1000–1100 & \textgreater{}1000 \\ \hline \multirow{2}{*}{12} & Terrain surface inclination angles up to 15\({}^{\circ}\) according to & landslide- & moraine & debris & landslide \\ \multicolumn{6}{c}{genetic soil types:} & scree & deposits & flows & landslide \\ \hline \multirow{2}{*}{13} & Terrain surface inclination angles 15\({}^{\circ}\)–20\({}^{\circ}\) according to & landslide- & landslide- & debris & landslides \\ \multicolumn{6}{c}{genetic soil types:} & scree & scree & flows & landslides \\ \hline \multirow{2}{*}{14} & Terrain surface inclination angles \textgreater{}20\({}^{\circ}\) according to genetic & landslide- & scree & scree & flows & landslides \\ \multicolumn{6}{c}{soil types:} & scree & scree & flows & flows & landslides \\ \hline \multirow{2}{*}{15} & Thickness of Quaternary deposits 0–5 m, at slope angles of & 12–15 & 15–20 & 20–25 & \textgreater{}25 \\ \multicolumn{6}{c}{12\({}^{\circ}\)–25\({}^{\circ}\) and more} & & & \\ \hline \multirow{2}{*}{16} & Thickness of Quaternary deposits 5–12 m, at slope angles of & 12–150 & 15–20 & 20–25 & \textgreater{}25 \\ \multicolumn{6}{c}{12\({}^{\circ}\)–25\({}^{\circ}\) and more} & & & \\ \hline \multirow{2}{*}{17} & Thickness of Quaternary deposits more than 12 m, at & 12–15 & 15–20 & 20–25 & \textgreater{}25 \\ \multicolumn{6}{c}{slope angles of 12\({}^{\circ}\)–25\({}^{\circ}\) and more} & & & \\ \hline \multirow{2}{*}{18} & Number of mudflows, from one to 5 and more per season, & & & & \\ volumes from 10 thousand m\({}^{3}\) and more & & & & & \\ \hline \multirow{2}{*}{19} & Landslides in the total volume for the year from 10 thousand to 2 million m\({}^{3}\) & 50 & 75 & 100 & 150 \\ \hline \multirow{2}{*}{20} & Landslides-scree up to 5000 m\({}^{3}\) & 75 & 100 & 150 & 200 \\ \hline \multirow{2}{*}{21} & Flat wash, area from 0.05 to 0.10 km\({}^{2}\) and more, per km\({}^{2}\) & 0.05 & 0.06 & 0.07 & \textgreater{}0.1 \\ \hline \multirow{2}{*}{22} & Erosive activity of rivers from 1 to 5 m/hour of lateral erosion & 1.0 & 2.5 & 4.0 & 5.0 \\ \hline \multirow{2}{*}{23} & Soliflution with vertical capture power from 1 to 4 m & 1.0 & 2.0 & 3.0 & 4.0 \\ \hline \multirow{2}{*}{24} & Stream erosion on slopes of 200 or more & 20 & 25 & 30 & \textgreater{}35 \\ \hline \multirow{2}{*}{25} & Karst formation, from one to three or more manifestations per & 1 & 2 & 3 & \textgreater{}3 \\ \multicolumn{6}{c}{km\({}^{2}\) of area} & & & & \\ \hline \multirow{2}{*}{26} & Avalanches, up to 4 or more descents per season & 1 & 2 & 3 & 4 \\ \hline \multirow{2}{*}{27} & Glaciers and glaciers up to three or more flood-type events & 1 & 2 & 3 & \textgreater{}3 \\ \multicolumn{6}{c}{per area} & & & & & \\ \hline \hline \end{tabular}
\end{table}