Latitude: 42.676894 | Longitude: 19.862192 | Country: Montenegro | Year: 2018 |
| F | 14.76505 | km2 | Surface area of the drainage basin |
| Fm | 6.08231 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 8.68274 | km2 | Surface area of greater portion of the drainage basin |
| O | 17.31694 | km | The length of the watershed |
| Lv | 2.68544 | km | Natural length of the main watercourse |
| Lb | 6.41894 | km | Surface area of greater portion of the drainage basin |
| Liz | ["1.97336 ","6.38796 ","6.70489 ","6.57601 ","6.39539 ","6.10127 ","5.66343 ","5.33710 ","3.67136 ","1.05165 ","0.64204 ","0.40662 "] | km | Contour line length |
| f | ["0.33677 ","2.67540 ","1.69251 ","1.73429 ","1.84289 ","1.57783 ","1.53829 ","1.23032 ","1.34466 ","0.48165 ","0.16450 ","0.09530 ","0.05064 "] | km2 | The area between the two neighboring contour lines |
| h0 | 800 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 780 | m | Lowest altitude in the drainage basin |
| Hmax | 1988 | m | Highest altitude in the draigane basin |
| ΣL | 2.68544 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.44721 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.1962 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.156 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.6478 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.537175621 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.422613972 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.040210407 | 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 |
| 19.12 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 63.75 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 17.12 % | 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 |
| 4.02 % | Plough-lands |
| 3.23 % | Orchards and vineyards |
| 27.82 % | Mountain pastures |
| 11.21 % | Meadows |
| 11.49 % | Degraded forests |
| 42.23 % | Well-constituted forests |
| 7.15 % | Depth erosion |
| 6.36 % | 80% of the river basin under rill and gully erosion |
| 5.56 % | 50% of the river basin under rill and gully erosion |
| 4.77 % | 100% of the river basin under surface erosion |
| 11.21 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 2.38 % | 50% of the river basin under surface erosion |
| 1.59 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 4.02 % | The river basin mostly under plough-land |
| 56.94 % | The river basin under forests and perennial vegetation |
| A | 1.2574487979623 | / | Coefficient of the river basin form |
| m | 0.19714831088342 | / | Coefficient of the watershed development |
| B | 2.3002318139755 | km | Average river basin width |
| a | 0.35224127246437 | / | (A)symmetry of the river basin |
| G | 0.18187815144547 | / | Density of the river network of the basin |
| K | 1.0973475917473 | / | Coefficient of the river basin tortuousness |
| Hsr | 1175.9434245058 | m | Average river basin altitude |
| Dsr | 395.9434245058 | m | Average elevation difference of the river basin |
| Isr | 34.480804331851 | % | Average river basin decline |
| Hleb | 1208 | m | The height of the local erosion base of the river basin |
| Er | 196.15904166331 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.37751377303 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.83548 | / | Coefficient of the region's permeability |
| S2 | 0.7006069572 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 338.67530453989 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 343.38418840686 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.4198702219755 | / | Coefficient of the river basin erosion |
| Wgod | 14938.226989774 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.41283508957208 | / | Coefficient of the deposit retention |
| Ggod | 6167.0242773715 | m3 god-1 | Real soil losses |
| Ggod km-2 | 417.67716854135 | m3 km-2 god-1 | Real soil losses per km2 |