Latitude: 42.617437 | Longitude: 19.937493 | Country: Montenegro | Year: 2018 |
| F | 69.57222 | km2 | Surface area of the drainage basin |
| Fm | 33.70013 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 35.87209 | km2 | Surface area of greater portion of the drainage basin |
| O | 39.89908 | km | The length of the watershed |
| Lv | 14.54081 | km | Natural length of the main watercourse |
| Lb | 16.2095 | km | Surface area of greater portion of the drainage basin |
| Liz | ["10.20105 ","20.72815 ","26.40122 ","28.32701 ","31.82954 ","32.87518 ","32.29958 ","29.51557 ","27.32305 ","19.02231 ","12.12301 ","2.52508 "] | km | Contour line length |
| f | ["5.34923 ","4.65281 ","5.91714 ","6.33132 ","6.56607 ","6.79885 ","7.37212 ","7.49663 ","6.74740 ","6.14937 ","4.05821 ","1.83075 ","0.30230 "] | km2 | The area between the two neighboring contour lines |
| h0 | 1000 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 907 | m | Lowest altitude in the drainage basin |
| Hmax | 2149 | m | Highest altitude in the draigane basin |
| ΣL | 37.50148 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 12.11945 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.0325 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0645 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.903 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.504824965 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.469212049 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.025962986 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 89.4 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 8.1 | °C | Average annual air temperature |
| Hgod | 1345.4 | mm | Average annual quantity of precipitation |
| 11.06 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 88.61 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 0.33 % | 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 |
| 2.6 % | Plough-lands |
| 0.48 % | Orchards and vineyards |
| 35.48 % | Mountain pastures |
| 10.96 % | Meadows |
| 25.24 % | Degraded forests |
| 25.24 % | Well-constituted forests |
| 9.12 % | Depth erosion |
| 8.11 % | 80% of the river basin under rill and gully erosion |
| 7.1 % | 50% of the river basin under rill and gully erosion |
| 6.08 % | 100% of the river basin under surface erosion |
| 10.96 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 3.04 % | 50% of the river basin under surface erosion |
| 2.03 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 2.6 % | The river basin mostly under plough-land |
| 50.96 % | The river basin under forests and perennial vegetation |
| A | 0.53506789511726 | / | Coefficient of the river basin form |
| m | 0.49177419582941 | / | Coefficient of the watershed development |
| B | 4.2920645300595 | km | Average river basin width |
| a | 0.062437564878625 | / | (A)symmetry of the river basin |
| G | 0.53902951494145 | / | Density of the river network of the basin |
| K | 1.1997912446522 | / | Coefficient of the river basin tortuousness |
| Hsr | 1476.4028322655 | m | Average river basin altitude |
| Dsr | 569.4028322655 | m | Average elevation difference of the river basin |
| Isr | 39.264342865586 | % | Average river basin decline |
| Hleb | 1242 | m | The height of the local erosion base of the river basin |
| Er | 136.88717401773 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.0628969455629 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.96115 | / | Coefficient of the region's permeability |
| S2 | 0.7042276042 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 881.61149438756 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 339.37630041292 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.95393920141695 | / | Temperature coefficient of the region |
| Z | 0.553755238131 | / | Coefficient of the river basin erosion |
| Wgod | 115593.82236054 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.38844752171698 | / | Coefficient of the deposit retention |
| Ggod | 44902.133821746 | m3 god-1 | Real soil losses |
| Ggod km-2 | 645.40320578739 | m3 km-2 god-1 | Real soil losses per km2 |