Latitude: 42.672351 | Longitude: 19.866152 | Country: Montenegro | Year: 2018 |
| F | 6.90446 | km2 | Surface area of the drainage basin |
| Fm | 3.14642 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 3.75804 | km2 | Surface area of greater portion of the drainage basin |
| O | 11.50498 | km | The length of the watershed |
| Lv | 1.27037 | km | Natural length of the main watercourse |
| Lb | 5.07595 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.65353 ","2.85988 ","2.69617 ","2.63675 ","2.49850 ","2.48061 ","2.40735 ","2.49351 ","2.47841 ","2.29500 ","2.21177 ","1.38448 ","0.88421 "] | km | Contour line length |
| f | ["0.95194 ","0.71860 ","0.65874 ","0.69487 ","0.60179 ","0.49996 ","0.48542 ","0.45687 ","0.56179 ","0.50261 ","0.33114 ","0.25706 ","0.12930 ","0.05438 "] | km2 | The area between the two neighboring contour lines |
| h0 | 900 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 810 | m | Lowest altitude in the drainage basin |
| Hmax | 2126 | m | Highest altitude in the draigane basin |
| ΣL | 1.27037 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 1.17921 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.327 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1602 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.5128 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.680741123 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.298309852 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.020949025 | 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 |
| 11.24 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 52.23 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 36.53 % | 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 |
| 2.09 % | Plough-lands |
| 2.38 % | Orchards and vineyards |
| 17.81 % | Mountain pastures |
| 9.64 % | Meadows |
| 17.23 % | Degraded forests |
| 50.85 % | Well-constituted forests |
| 4.58 % | Depth erosion |
| 4.07 % | 80% of the river basin under rill and gully erosion |
| 3.56 % | 50% of the river basin under rill and gully erosion |
| 3.05 % | 100% of the river basin under surface erosion |
| 9.64 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.53 % | 50% of the river basin under surface erosion |
| 1.02 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 2.09 % | The river basin mostly under plough-land |
| 70.45 % | The river basin under forests and perennial vegetation |
| A | 1.7659981737604 | / | Coefficient of the river basin form |
| m | 0.13638306247806 | / | Coefficient of the watershed development |
| B | 1.3602301047095 | km | Average river basin width |
| a | 0.17716664301046 | / | (A)symmetry of the river basin |
| G | 0.18399266561034 | / | Density of the river network of the basin |
| K | 1.0773059929953 | / | Coefficient of the river basin tortuousness |
| Hsr | 1321.8867427721 | m | Average river basin altitude |
| Dsr | 511.8867427721 | m | Average elevation difference of the river basin |
| Isr | 43.421455117417 | % | Average river basin decline |
| Hleb | 1316 | m | The height of the local erosion base of the river basin |
| Er | 258.41849156576 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3951648113995 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.75574 | / | Coefficient of the region's permeability |
| S2 | 0.6680415804 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 263.33058351586 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 327.56158937589 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.32607973066115 | / | Coefficient of the river basin erosion |
| Wgod | 4780.8700990263 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.43064726833478 | / | Coefficient of the deposit retention |
| Ggod | 2058.8686484091 | m3 god-1 | Real soil losses |
| Ggod km-2 | 298.19401494239 | m3 km-2 god-1 | Real soil losses per km2 |