Latitude: 42.678026 | Longitude: 19.924543 | Country: Montenegro | Year: 2018 |
| F | 11.49594 | km2 | Surface area of the drainage basin |
| Fm | 5.44077 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 6.05517 | km2 | Surface area of greater portion of the drainage basin |
| O | 14.1326 | km | The length of the watershed |
| Lv | 3.72568 | km | Natural length of the main watercourse |
| Lb | 5.58109 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.80685 ","4.10299 ","4.70407 ","5.32706 ","5.34557 ","4.95016 ","4.80633 ","4.44049 ","3.29382 ","2.93046 ","2.65587 ","0.39185 "] | km | Contour line length |
| f | ["0.96358 ","0.78701 ","1.08552 ","1.26289 ","1.36072 ","1.31207 ","1.09857 ","1.18937 ","0.77843 ","0.66581 ","0.64353 ","0.3243 ","0.02649 "] | km2 | The area between the two neighboring contour lines |
| h0 | 900 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 849 | m | Lowest altitude in the drainage basin |
| Hmax | 2003 | m | Highest altitude in the draigane basin |
| ΣL | 3.72568 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 3.19774 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.1331 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1086 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.7583 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.450957516 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.512015243 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.037027241 | 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 | 1182.3 | mm | Average annual quantity of precipitation |
| 8.49 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 74.26 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 17.25 % | 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 |
| 3.7 % | Plough-lands |
| 3.02 % | Orchards and vineyards |
| 19.94 % | Mountain pastures |
| 28.24 % | Meadows |
| 13.04 % | Degraded forests |
| 32.06 % | Well-constituted forests |
| 5.13 % | Depth erosion |
| 4.56 % | 80% of the river basin under rill and gully erosion |
| 3.99 % | 50% of the river basin under rill and gully erosion |
| 3.42 % | 100% of the river basin under surface erosion |
| 28.24 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.71 % | 50% of the river basin under surface erosion |
| 1.14 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 3.7 % | The river basin mostly under plough-land |
| 48.12 % | The river basin under forests and perennial vegetation |
| A | 0.73969235146336 | / | Coefficient of the river basin form |
| m | 0.30997621732387 | / | Coefficient of the watershed development |
| B | 2.059801938331 | km | Average river basin width |
| a | 0.10688991069891 | / | (A)symmetry of the river basin |
| G | 0.32408659057024 | / | Density of the river network of the basin |
| K | 1.1650978503568 | / | Coefficient of the river basin tortuousness |
| Hsr | 1341.0461819564 | m | Average river basin altitude |
| Dsr | 492.0461819564 | m | Average elevation difference of the river basin |
| Isr | 39.801460341651 | % | Average river basin decline |
| Hleb | 1154 | m | The height of the local erosion base of the river basin |
| Er | 199.48939536053 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.1134000606982 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.88756 | / | Coefficient of the region's permeability |
| S2 | 0.717213945 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 333.13838718121 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 174.6519722035 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.95393920141695 | / | Temperature coefficient of the region |
| Z | 0.44158900886332 | / | Coefficient of the river basin erosion |
| Wgod | 11952.813129977 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.38424665261268 | / | Coefficient of the deposit retention |
| Ggod | 4592.8284344986 | m3 god-1 | Real soil losses |
| Ggod km-2 | 399.51743263262 | m3 km-2 god-1 | Real soil losses per km2 |