Latitude: 42.751792 | Longitude: 19.788604 | Country: Montenegro | Year: 2018 |
| F | 10.5856 | km2 | Surface area of the drainage basin |
| Fm | 3.68039 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 6.90521 | km2 | Surface area of greater portion of the drainage basin |
| O | 15.36462 | km | The length of the watershed |
| Lv | 2.9127 | km | Natural length of the main watercourse |
| Lb | 6.60504 | km | Surface area of greater portion of the drainage basin |
| Liz | ["5.00500 ","4.98801 ","4.05822 ","3.33958 ","3.45037 ","3.20026 ","2.78777 ","1.48300 ","0.22885 "] | km | Contour line length |
| f | ["2.50054 ","1.85878 ","1.85338 ","1.16409 ","1.06377 ","0.70530 ","0.69200 ","0.51245 ","0.21541 ","0.01988 "] | km2 | The area between the two neighboring contour lines |
| h0 | 800 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 726 | m | Lowest altitude in the drainage basin |
| Hmax | 1640 | m | Highest altitude in the draigane basin |
| ΣL | 2.9127 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.8697 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.0486 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.3995 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.5519 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.494792756 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.454165783 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.051041461 | 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 |
| 12.84 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 78.72 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 6.92 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 1.53 % | 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 |
| 5.1 % | Plough-lands |
| 12.84 % | Orchards and vineyards |
| 8.86 % | Mountain pastures |
| 23.72 % | Meadows |
| 9.79 % | Degraded forests |
| 39.69 % | Well-constituted forests |
| 2.28 % | Depth erosion |
| 2.03 % | 80% of the river basin under rill and gully erosion |
| 1.77 % | 50% of the river basin under rill and gully erosion |
| 1.52 % | 100% of the river basin under surface erosion |
| 23.72 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.76 % | 50% of the river basin under surface erosion |
| 0.51 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 5.1 % | The river basin mostly under plough-land |
| 62.32 % | The river basin under forests and perennial vegetation |
| A | 1.0286335358945 | / | Coefficient of the river basin form |
| m | 0.25254169103003 | / | Coefficient of the watershed development |
| B | 1.6026549422865 | km | Average river basin width |
| a | 0.60928431076179 | / | (A)symmetry of the river basin |
| G | 0.27515681680774 | / | Density of the river network of the basin |
| K | 1.0149841446841 | / | Coefficient of the river basin tortuousness |
| Hsr | 1003.1726704202 | m | Average river basin altitude |
| Dsr | 277.1726704202 | m | Average elevation difference of the river basin |
| Isr | 26.962156136638 | % | Average river basin decline |
| Hleb | 914 | m | The height of the local erosion base of the river basin |
| Er | 161.29371808927 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3751701123048 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.85099 | / | Coefficient of the region's permeability |
| S2 | 0.711249741 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 239.92883439137 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 205.42160885251 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.34829787407486 | / | Coefficient of the river basin erosion |
| Wgod | 8091.578186912 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.31963111466604 | / | Coefficient of the deposit retention |
| Ggod | 2586.3201552901 | m3 god-1 | Real soil losses |
| Ggod km-2 | 244.32437984527 | m3 km-2 god-1 | Real soil losses per km2 |