Latitude: 42.978454 | Longitude: 19.762097 | Country: Montenegro | Year: 2018 |
| F | 11.59289 | km2 | Surface area of the drainage basin |
| Fm | 4.33652 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 7.25637 | km2 | Surface area of greater portion of the drainage basin |
| O | 15.51315 | km | The length of the watershed |
| Lv | 5.94182 | km | Natural length of the main watercourse |
| Lb | 7.01044 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.36384 ","10.12389 ","13.01776 ","5.28770 ","2.56176 "] | km | Contour line length |
| f | ["0.04403 ","2.54123 ","3.65344 ","3.38590 ","1.47726 ","0.49102 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 593 | m | Lowest altitude in the drainage basin |
| Hmax | 1026 | m | Highest altitude in the draigane basin |
| ΣL | 5.94182 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 5.38445 | km | The shortest distance between the fountain - head and mouth |
| fp | 0 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0934 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.9066 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.558266472 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.357922474 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.083811054 | 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 |
| 11.33 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 88.67 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 0 % | 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 |
| 8.38 % | Plough-lands |
| 4.97 % | Orchards and vineyards |
| 8.55 % | Mountain pastures |
| 22.28 % | Meadows |
| 36.29 % | Degraded forests |
| 19.54 % | Well-constituted forests |
| 2.2 % | Depth erosion |
| 1.95 % | 80% of the river basin under rill and gully erosion |
| 1.71 % | 50% of the river basin under rill and gully erosion |
| 1.47 % | 100% of the river basin under surface erosion |
| 22.28 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.73 % | 50% of the river basin under surface erosion |
| 0.49 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 8.38 % | The river basin mostly under plough-land |
| 60.79 % | The river basin under forests and perennial vegetation |
| A | 0.50911408457341 | / | Coefficient of the river basin form |
| m | 0.49228737901982 | / | Coefficient of the watershed development |
| B | 1.653660825854 | km | Average river basin width |
| a | 0.50373116625794 | / | (A)symmetry of the river basin |
| G | 0.51254001374981 | / | Density of the river network of the basin |
| K | 1.1035147508102 | / | Coefficient of the river basin tortuousness |
| Hsr | 793.32751841862 | m | Average river basin altitude |
| Dsr | 200.32751841862 | m | Average elevation difference of the river basin |
| Isr | 27.046707076493 | % | Average river basin decline |
| Hleb | 433 | m | The height of the local erosion base of the river basin |
| Er | 74.694752899571 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7023202673314 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.97198 | / | Coefficient of the region's permeability |
| S2 | 0.7051089164 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 213.4595869098 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 126.79016925308 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.45732226310679 | / | Coefficient of the river basin erosion |
| Wgod | 11024.410407001 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.22116296110144 | / | Coefficient of the deposit retention |
| Ggod | 2438.1912500099 | m3 god-1 | Real soil losses |
| Ggod km-2 | 210.3178111765 | m3 km-2 god-1 | Real soil losses per km2 |