Latitude: 42.99937 | Longitude: 19.783771 | Country: Montenegro | Year: 2018 |
| F | 19.88449 | km2 | Surface area of the drainage basin |
| Fm | 4.33285 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 15.55164 | km2 | Surface area of greater portion of the drainage basin |
| O | 18.87811 | km | The length of the watershed |
| Lv | 4.61118 | km | Natural length of the main watercourse |
| Lb | 8.47295 | km | Surface area of greater portion of the drainage basin |
| Liz | ["4.71580 ","7.09187 ","9.06489 ","12.09064 ","9.39542 ","8.02450 ","3.10048 ","1.45538 "] | km | Contour line length |
| f | ["5.46874 ","1.96215 ","1.76201 ","2.47458 ","3.14015 ","2.55860 ","1.73104 ","0.55649 ","0.23072 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 670 | m | Lowest altitude in the drainage basin |
| Hmax | 1474 | m | Highest altitude in the draigane basin |
| ΣL | 8.96687 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 3.4541 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.5922 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1445 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.2633 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.564559451 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.350041601 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.085398949 | 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 | 944.3 | mm | Average annual quantity of precipitation |
| 24.35 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 71.13 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 3.53 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 1 % | 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 |
| 8.54 % | Plough-lands |
| 3.27 % | Orchards and vineyards |
| 9.02 % | Mountain pastures |
| 22.72 % | Meadows |
| 33.87 % | Degraded forests |
| 22.58 % | Well-constituted forests |
| 2.32 % | Depth erosion |
| 2.06 % | 80% of the river basin under rill and gully erosion |
| 1.8 % | 50% of the river basin under rill and gully erosion |
| 1.55 % | 100% of the river basin under surface erosion |
| 22.72 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.77 % | 50% of the river basin under surface erosion |
| 0.52 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 8.54 % | The river basin mostly under plough-land |
| 59.72 % | The river basin under forests and perennial vegetation |
| A | 0.79832742378307 | / | Coefficient of the river basin form |
| m | 0.29170905822571 | / | Coefficient of the watershed development |
| B | 2.3468201747915 | km | Average river basin width |
| a | 1.1283960513948 | / | (A)symmetry of the river basin |
| G | 0.45094794988456 | / | Density of the river network of the basin |
| K | 1.3349874062708 | / | Coefficient of the river basin tortuousness |
| Hsr | 933.00922176028 | m | Average river basin altitude |
| Dsr | 263.00922176028 | m | Average elevation difference of the river basin |
| Isr | 27.629061645534 | % | Average river basin decline |
| Hleb | 804 | m | The height of the local erosion base of the river basin |
| Er | 121.1930072017 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3599658789281 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.60133 | / | Coefficient of the region's permeability |
| S2 | 0.7041679004 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 320.32602015572 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 147.26189109066 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.48514937173591 | / | Coefficient of the river basin erosion |
| Wgod | 19933.682148869 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.305006748772 | / | Coefficient of the deposit retention |
| Ggod | 6079.907583281 | m3 god-1 | Real soil losses |
| Ggod km-2 | 305.76130357284 | m3 km-2 god-1 | Real soil losses per km2 |