Latitude: 42.663653 | Longitude: 19.902088 | Country: Montenegro | Year: 2018 |
| F | 3.07806 | km2 | Surface area of the drainage basin |
| Fm | 1.32927 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 1.74879 | km2 | Surface area of greater portion of the drainage basin |
| O | 9.1759 | km | The length of the watershed |
| Lv | 2.78414 | km | Natural length of the main watercourse |
| Lb | 4.32931 | km | Surface area of greater portion of the drainage basin |
| Liz | ["1.45953 ","1.55601 ","1.48878 ","1.33318 ","1.3085 ","1.23931 ","1.1613 ","1.2656 ","0.5191 ","0.30147 ","0.12045 "] | km | Contour line length |
| f | ["0.27895 ","0.26845 ","0.36231 ","0.34325 ","0.3416 ","0.41414 ","0.31605 ","0.35195 ","0.26197 ","0.08884 ","0.04375 ","0.00952 "] | km2 | The area between the two neighboring contour lines |
| h0 | 900 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 842 | m | Lowest altitude in the drainage basin |
| Hmax | 1988 | m | Highest altitude in the draigane basin |
| ΣL | 2.78414 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.60557 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.0605 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1562 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.7833 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.653552485 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.296261262 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.050186253 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 89.4 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 8.1 | °C | Average annual air temperature |
| Hgod | 1182.3 | mm | Average annual quantity of precipitation |
| 7.06 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 91.27 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 1.67 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 0 % | Brown forest soils and Mountain soils |
| 0 % | Epieugleysol and Marshlands |
| 0 % | Good structured Chernozems and alluvial well-structured deposits |
| 0 % | Bare, compact igneous |
| 0 % | Bare lands |
| 5.02 % | Plough-lands |
| 7.49 % | Orchards and vineyards |
| 0 % | Mountain pastures |
| 22.14 % | Meadows |
| 16.14 % | Degraded forests |
| 49.21 % | Well-constituted forests |
| 0 % | Depth erosion |
| 0 % | 80% of the river basin under rill and gully erosion |
| 0 % | 50% of the river basin under rill and gully erosion |
| 0 % | 100% of the river basin under surface erosion |
| 22.14 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0 % | 50% of the river basin under surface erosion |
| 0 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 5.02 % | The river basin mostly under plough-land |
| 72.84 % | The river basin under forests and perennial vegetation |
| A | 0.64267619444424 | / | Coefficient of the river basin form |
| m | 0.44765928560151 | / | Coefficient of the watershed development |
| B | 0.71098165758516 | km | Average river basin width |
| a | 0.27258727900041 | / | (A)symmetry of the river basin |
| G | 0.9045112830809 | / | Density of the river network of the basin |
| K | 1.0685339484259 | / | Coefficient of the river basin tortuousness |
| Hsr | 1283.3423747425 | m | Average river basin altitude |
| Dsr | 441.3423747425 | m | Average elevation difference of the river basin |
| Isr | 38.18388855318 | % | Average river basin decline |
| Hleb | 1146 | m | The height of the local erosion base of the river basin |
| Er | 275.40097575211 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.1204169188381 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.91684 | / | Coefficient of the region's permeability |
| S2 | 0.6793267536 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 163.25852027443 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 73.218360258248 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.95393920141695 | / | Temperature coefficient of the region |
| Z | 0.29663005078001 | / | Coefficient of the river basin erosion |
| Wgod | 1761.9681707672 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.31482602601334 | / | Coefficient of the deposit retention |
| Ggod | 554.71343716462 | m3 god-1 | Real soil losses |
| Ggod km-2 | 180.21527753345 | m3 km-2 god-1 | Real soil losses per km2 |