Latitude: 42.775302 | Longitude: 19.827458 | Country: Montenegro | Year: 2018 |
| F | 39.30106 | km2 | Surface area of the drainage basin |
| Fm | 14.08734 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 25.21372 | km2 | Surface area of greater portion of the drainage basin |
| O | 34.96124 | km | The length of the watershed |
| Lv | 13.83445 | km | Natural length of the main watercourse |
| Lb | 15.94679 | km | Surface area of greater portion of the drainage basin |
| Liz | ["6.00891 ","6.14476 ","5.92980 ","3.80681 ","4.06229 ","9.15918 ","23.16723 ","28.49943 ","29.58575 ","18.10096 ","6.55870 "] | km | Contour line length |
| f | ["1.79194 ","1.53032 ","1.53571 ","1.17150 ","0.87034 ","1.39986 ","4.05783 ","6.08236 ","8.25404 ","7.20836 ","4.39681 ","1.00200 "] | km2 | The area between the two neighboring contour lines |
| h0 | 800 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 721 | m | Lowest altitude in the drainage basin |
| Hmax | 1876 | m | Highest altitude in the draigane basin |
| ΣL | 16.4327 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 12.62873 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.1344 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0524 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.8132 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.706685953 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.289831663 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.003482384 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 115 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 9.0 | °C | Average annual air temperature |
| Hgod | 1183.7 | mm | Average annual quantity of precipitation |
| 2.13 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 88.67 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 0.7 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 8.5 % | 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 |
| 0.35 % | Plough-lands |
| 0.13 % | Orchards and vineyards |
| 14.02 % | Mountain pastures |
| 14.84 % | Meadows |
| 18.27 % | Degraded forests |
| 52.39 % | Well-constituted forests |
| 3.6 % | Depth erosion |
| 3.2 % | 80% of the river basin under rill and gully erosion |
| 2.8 % | 50% of the river basin under rill and gully erosion |
| 2.4 % | 100% of the river basin under surface erosion |
| 14.84 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.2 % | 50% of the river basin under surface erosion |
| 0.8 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 0.35 % | The river basin mostly under plough-land |
| 70.8 % | The river basin under forests and perennial vegetation |
| A | 0.49278733885337 | / | Coefficient of the river basin form |
| m | 0.62252218635761 | / | Coefficient of the watershed development |
| B | 2.4645122936967 | km | Average river basin width |
| a | 0.56621271792669 | / | (A)symmetry of the river basin |
| G | 0.41812358241737 | / | Density of the river network of the basin |
| K | 1.0954743667811 | / | Coefficient of the river basin tortuousness |
| Hsr | 1440.7855632902 | m | Average river basin altitude |
| Dsr | 719.7855632902 | m | Average elevation difference of the river basin |
| Isr | 35.882955828672 | % | Average river basin decline |
| Hleb | 1155 | m | The height of the local erosion base of the river basin |
| Er | 146.83549293981 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3057283178395 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.90364 | / | Coefficient of the region's permeability |
| S2 | 0.6593592862 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 744.99472794661 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 285.61639764054 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.26981878989408 | / | Coefficient of the river basin erosion |
| Wgod | 20483.49544393 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.42093965497042 | / | Coefficient of the deposit retention |
| Ggod | 8622.315504756 | m3 god-1 | Real soil losses |
| Ggod km-2 | 219.39142366023 | m3 km-2 god-1 | Real soil losses per km2 |