Latitude: 42.817809 | Longitude: 19.866599 | Country: Montenegro | Year: 2018 |
| F | 11.69991 | km2 | Surface area of the drainage basin |
| Fm | 3.9262 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 7.77371 | km2 | Surface area of greater portion of the drainage basin |
| O | 17.97199 | km | The length of the watershed |
| Lv | 7.32939 | km | Natural length of the main watercourse |
| Lb | 8.95886 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.26373 ","2.44888 ","3.41644 ","6.61094 ","5.77042 ","4.94255 ","4.89357 ","4.17590 ","0.68560 "] | km | Contour line length |
| f | ["1.46015 ","1.21997 ","0.85333 ","0.98065 ","2.09782 ","1.89411 ","1.20545 ","1.27968 ","0.67651 ","0.03226 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 690 | m | Lowest altitude in the drainage basin |
| Hmax | 1567 | m | Highest altitude in the draigane basin |
| ΣL | 7.32939 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 6.06925 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.7788 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.2212 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.569665531 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.361735681 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.068598788 | 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 |
| 33.07 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 37.63 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 29.3 % | 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 |
| 6.86 % | Plough-lands |
| 3.34 % | Orchards and vineyards |
| 13.62 % | Mountain pastures |
| 19.22 % | Meadows |
| 34.18 % | Degraded forests |
| 22.79 % | Well-constituted forests |
| 3.5 % | Depth erosion |
| 3.11 % | 80% of the river basin under rill and gully erosion |
| 2.72 % | 50% of the river basin under rill and gully erosion |
| 2.33 % | 100% of the river basin under surface erosion |
| 19.22 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.17 % | 50% of the river basin under surface erosion |
| 0.78 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 6.86 % | The river basin mostly under plough-land |
| 60.31 % | The river basin under forests and perennial vegetation |
| A | 0.47814866585077 | / | Coefficient of the river basin form |
| m | 0.60446566749059 | / | Coefficient of the watershed development |
| B | 1.3059596868352 | km | Average river basin width |
| a | 0.65769907631768 | / | (A)symmetry of the river basin |
| G | 0.6264484085775 | / | Density of the river network of the basin |
| K | 1.2076269720311 | / | Coefficient of the river basin tortuousness |
| Hsr | 1045.517269791 | m | Average river basin altitude |
| Dsr | 355.517269791 | m | Average elevation difference of the river basin |
| Isr | 30.092564814601 | % | Average river basin decline |
| Hleb | 877 | m | The height of the local erosion base of the river basin |
| Er | 150.93991129251 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3406486806972 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.46636 | / | Coefficient of the region's permeability |
| S2 | 0.6997866514 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 285.67426131384 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 59.763495936829 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.51992326106903 | / | Coefficient of the river basin erosion |
| Wgod | 13012.215743941 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.29172601205162 | / | Coefficient of the deposit retention |
| Ggod | 3796.0018069353 | m3 god-1 | Real soil losses |
| Ggod km-2 | 324.44709463024 | m3 km-2 god-1 | Real soil losses per km2 |