Latitude: 43.126851 | Longitude: 19.766691 | Country: Montenegro | Year: 2018 |
| F | 11.4021 | km2 | Surface area of the drainage basin |
| Fm | 5.6707 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 5.7314 | km2 | Surface area of greater portion of the drainage basin |
| O | 14.58839 | km | The length of the watershed |
| Lv | 5.20805 | km | Natural length of the main watercourse |
| Lb | 6.52291 | km | Surface area of greater portion of the drainage basin |
| Liz | ["4.66683 ","6.71907 ","7.60343 ","6.77277 ","5.69539 ","3.50497 ","2.04705 "] | km | Contour line length |
| f | ["0.84581 ","1.59509 ","2.10808 ","2.21129 ","2.09680 ","1.37155 ","0.81267 ","0.36081 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 537 | m | Lowest altitude in the drainage basin |
| Hmax | 1212 | m | Highest altitude in the draigane basin |
| ΣL | 5.20805 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 4.07012 | 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 | 0.0766 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.9234 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.512796530 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.401242996 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.085960473 | 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 | 873.7 | mm | Average annual quantity of precipitation |
| 3.91 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 96.09 % | 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 |
| 8.6 % | Plough-lands |
| 4.48 % | Orchards and vineyards |
| 10.59 % | Mountain pastures |
| 25.06 % | Meadows |
| 33.33 % | Degraded forests |
| 17.95 % | Well-constituted forests |
| 2.72 % | Depth erosion |
| 2.42 % | 80% of the river basin under rill and gully erosion |
| 2.12 % | 50% of the river basin under rill and gully erosion |
| 1.81 % | 100% of the river basin under surface erosion |
| 25.06 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.91 % | 50% of the river basin under surface erosion |
| 0.6 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 8.6 % | The river basin mostly under plough-land |
| 55.76 % | The river basin under forests and perennial vegetation |
| A | 0.54621903591555 | / | Coefficient of the river basin form |
| m | 0.4350886861393 | / | Coefficient of the watershed development |
| B | 1.7480081742658 | km | Average river basin width |
| a | 0.010647161487796 | / | (A)symmetry of the river basin |
| G | 0.45676235079503 | / | Density of the river network of the basin |
| K | 1.2795814374023 | / | Coefficient of the river basin tortuousness |
| Hsr | 857.74575253681 | m | Average river basin altitude |
| Dsr | 320.74575253681 | m | Average elevation difference of the river basin |
| Isr | 32.458503258172 | % | Average river basin decline |
| Hleb | 675 | m | The height of the local erosion base of the river basin |
| Er | 116.92508350443 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.709670871128 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.97702 | / | Coefficient of the region's permeability |
| S2 | 0.7146327878 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 267.86895367866 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 174.65785292733 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.47755619836772 | / | Coefficient of the river basin erosion |
| Wgod | 10276.645623896 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.28447270568727 | / | Coefficient of the deposit retention |
| Ggod | 2923.4251860189 | m3 god-1 | Real soil losses |
| Ggod km-2 | 256.39357539566 | m3 km-2 god-1 | Real soil losses per km2 |