Latitude: 42.824718 | Longitude: 19.865157 | Country: Montenegro | Year: 2018 |
| F | 9.06427 | km2 | Surface area of the drainage basin |
| Fm | 2.54038 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 6.52389 | km2 | Surface area of greater portion of the drainage basin |
| O | 18.83541 | km | The length of the watershed |
| Lv | 7.39243 | km | Natural length of the main watercourse |
| Lb | 6.30663 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.98027 ","3.45141 ","3.09451 ","3.40738 ","1.63245 ","1.73714 ","1.68626 ","1.49858 ","1.57264 ","1.62960 "] | km | Contour line length |
| f | ["2.47668 ","1.77392 ","1.09381 ","1.02734 ","0.79795 ","0.37830 ","0.30285 ","0.31578 ","0.24904 ","0.30478 ","0.34385 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 691 | m | Lowest altitude in the drainage basin |
| Hmax | 1650 | m | Highest altitude in the draigane basin |
| ΣL | 8.44057 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 6.99319 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.2659 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.5604 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.1737 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.653931210 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.309242057 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.036826733 | 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 |
| 28.6 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 58.37 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 13.03 % | 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 |
| 3.68 % | Plough-lands |
| 4.2 % | Orchards and vineyards |
| 10.4 % | Mountain pastures |
| 16.32 % | Meadows |
| 39.24 % | Degraded forests |
| 26.16 % | Well-constituted forests |
| 2.67 % | Depth erosion |
| 2.38 % | 80% of the river basin under rill and gully erosion |
| 2.08 % | 50% of the river basin under rill and gully erosion |
| 1.78 % | 100% of the river basin under surface erosion |
| 16.32 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.89 % | 50% of the river basin under surface erosion |
| 0.59 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 3.68 % | The river basin mostly under plough-land |
| 69.6 % | The river basin under forests and perennial vegetation |
| A | 0.49684676757169 | / | Coefficient of the river basin form |
| m | 0.69265324320911 | / | Coefficient of the watershed development |
| B | 1.4372604703304 | km | Average river basin width |
| a | 0.87894778068173 | / | (A)symmetry of the river basin |
| G | 0.93119137007172 | / | Density of the river network of the basin |
| K | 1.0570898259593 | / | Coefficient of the river basin tortuousness |
| Hsr | 929.88334306017 | m | Average river basin altitude |
| Dsr | 238.88334306017 | m | Average elevation difference of the river basin |
| Isr | 25.032617077823 | % | Average river basin decline |
| Hleb | 959 | m | The height of the local erosion base of the river basin |
| Er | 175.92822707776 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3402478688542 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.67234 | / | Coefficient of the region's permeability |
| S2 | 0.6765791046 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 206.11464580277 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 62.434404984637 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.44203943705981 | / | Coefficient of the river basin erosion |
| Wgod | 7902.8587842721 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.24392156888443 | / | Coefficient of the deposit retention |
| Ggod | 1927.6777133318 | m3 god-1 | Real soil losses |
| Ggod km-2 | 212.66772871194 | m3 km-2 god-1 | Real soil losses per km2 |