Latitude: 42.73322 | Longitude: 19.819346 | Country: Montenegro | Year: 2018 |
| F | 12.61614 | km2 | Surface area of the drainage basin |
| Fm | 5.11513 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 7.50101 | km2 | Surface area of greater portion of the drainage basin |
| O | 20.72708 | km | The length of the watershed |
| Lv | 1.23533 | km | Natural length of the main watercourse |
| Lb | 7.30658 | km | Surface area of greater portion of the drainage basin |
| Liz | ["10.37621 ","9.57327 ","9.01633 ","8.24128 ","7.30547 ","7.26588 ","5.03096 ","3.59283 ","0.36841 "] | km | Contour line length |
| f | ["2.16541 ","1.92023 ","1.58165 ","1.46163 ","1.31788 ","1.30616 ","1.14610 ","0.93213 ","0.49041 ","0.29454 "] | km2 | The area between the two neighboring contour lines |
| h0 | 800 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 726 | m | Lowest altitude in the drainage basin |
| Hmax | 1601 | m | Highest altitude in the draigane basin |
| ΣL | 1.23533 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 1.20294 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.691 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.087 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.222 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.499253578 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.484862241 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.015884181 | 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 |
| 23.37 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 53.32 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 23.31 % | 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 |
| 8.04 % | Degraded forests |
| 37.06 % | 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 | 3.2718225899152 | / | Coefficient of the river basin form |
| m | 0.098110345826308 | / | Coefficient of the watershed development |
| B | 1.7266819770672 | km | Average river basin width |
| a | 0.37822662082063 | / | (A)symmetry of the river basin |
| G | 0.097916636942837 | / | Density of the river network of the basin |
| K | 1.0269256987048 | / | Coefficient of the river basin tortuousness |
| Hsr | 1078.0091692071 | m | Average river basin altitude |
| Dsr | 352.0091692071 | m | Average elevation difference of the river basin |
| Isr | 48.168964516881 | % | Average river basin decline |
| Hleb | 875 | m | The height of the local erosion base of the river basin |
| Er | 147.7837067373 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3957048369087 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.5593 | / | Coefficient of the region's permeability |
| S2 | 0.7033261206 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 295.1819106165 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 530.24262386875 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.48168342602173 | / | Coefficient of the river basin erosion |
| Wgod | 15684.135105938 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.48082851234902 | / | Coefficient of the deposit retention |
| Ggod | 7541.3793504691 | m3 god-1 | Real soil losses |
| Ggod km-2 | 597.75647309471 | m3 km-2 god-1 | Real soil losses per km2 |