Latitude: 42.965364 | Longitude: 19.822026 | Country: Montenegro | Year: 2018 |
| F | 40.23096 | km2 | Surface area of the drainage basin |
| Fm | 12.4476 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 27.78336 | km2 | Surface area of greater portion of the drainage basin |
| O | 29.8793 | km | The length of the watershed |
| Lv | 8.46906 | km | Natural length of the main watercourse |
| Lb | 12.16551 | km | Surface area of greater portion of the drainage basin |
| Liz | ["20.14833 ","33.17354 ","30.38447 ","14.58891 ","9.80364 ","7.63453 ","2.80515 "] | km | Contour line length |
| f | ["4.88120 ","9.81131 ","9.50161 ","7.45868 ","3.61518 ","2.96913 ","1.60158 ","0.39228 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 619 | m | Lowest altitude in the drainage basin |
| Hmax | 1356 | m | Highest altitude in the draigane basin |
| ΣL | 12.37249 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 7.0783 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.1025 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1193 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.7782 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.498684400 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.352763084 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.148552517 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 157.6 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 8.9 | °C | Average annual air temperature |
| Hgod | 983.7 | mm | Average annual quantity of precipitation |
| 5.1 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 92.46 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 2.44 % | 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 |
| 14.86 % | Plough-lands |
| 1.89 % | Orchards and vineyards |
| 19.36 % | Mountain pastures |
| 14.03 % | Meadows |
| 29.92 % | Degraded forests |
| 19.95 % | Well-constituted forests |
| 4.98 % | Depth erosion |
| 4.42 % | 80% of the river basin under rill and gully erosion |
| 3.87 % | 50% of the river basin under rill and gully erosion |
| 3.32 % | 100% of the river basin under surface erosion |
| 14.03 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.66 % | 50% of the river basin under surface erosion |
| 1.11 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 14.86 % | The river basin mostly under plough-land |
| 51.76 % | The river basin under forests and perennial vegetation |
| A | 0.68797050676226 | / | Coefficient of the river basin form |
| m | 0.376660500986 | / | Coefficient of the watershed development |
| B | 3.3069686351004 | km | Average river basin width |
| a | 0.76238598333224 | / | (A)symmetry of the river basin |
| G | 0.30753653405238 | / | Density of the river network of the basin |
| K | 1.1964822061795 | / | Coefficient of the river basin tortuousness |
| Hsr | 881.73659639243 | m | Average river basin altitude |
| Dsr | 262.73659639243 | m | Average elevation difference of the river basin |
| Isr | 29.46451439389 | % | Average river basin decline |
| Hleb | 737 | m | The height of the local erosion base of the river basin |
| Er | 93.14885399898 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.6799766814581 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.90271 | / | Coefficient of the region's permeability |
| S2 | 0.7299736242 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 455.39681016669 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 346.83145682303 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.49716044480634 | / | Coefficient of the river basin erosion |
| Wgod | 43364.604433765 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.3034105639269 | / | Coefficient of the deposit retention |
| Ggod | 13157.279085716 | m3 god-1 | Real soil losses |
| Ggod km-2 | 327.04362723922 | m3 km-2 god-1 | Real soil losses per km2 |