Latitude: 43.009608 | Longitude: 19.739122 | Country: Montenegro | Year: 2018 |
| F | 1.55807 | km2 | Surface area of the drainage basin |
| Fm | 0.71461 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 0.84346 | km2 | Surface area of greater portion of the drainage basin |
| O | 6.60901 | km | The length of the watershed |
| Lv | 2.43468 | km | Natural length of the main watercourse |
| Lb | 3.02977 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.25 ","1.25458 ","2.36614 ","2.96405 ","2.02494 ","1.79414 ","1.77331 ","0.18047 "] | km | Contour line length |
| f | ["0.08060 ","0.07773 ","0.20672 ","0.25671 ","0.28424 ","0.18212 ","0.22623 ","0.24325 ","0.01236 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 50 | m | Equidistance |
| Hmin | 551 | m | Lowest altitude in the drainage basin |
| Hmax | 983 | m | Highest altitude in the draigane basin |
| ΣL | 3.02207 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.2963 | 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 | 0.077 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.923 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.572645755 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.372279326 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.055074919 | 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 | 893.3 | mm | Average annual quantity of precipitation |
| 8.25 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 91.75 % | 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 |
| 5.51 % | Plough-lands |
| 8.67 % | Orchards and vineyards |
| 9.24 % | Mountain pastures |
| 19.32 % | Meadows |
| 37.22 % | Degraded forests |
| 20.04 % | Well-constituted forests |
| 2.38 % | Depth erosion |
| 2.11 % | 80% of the river basin under rill and gully erosion |
| 1.85 % | 50% of the river basin under rill and gully erosion |
| 1.58 % | 100% of the river basin under surface erosion |
| 19.32 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.79 % | 50% of the river basin under surface erosion |
| 0.53 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 5.51 % | The river basin mostly under plough-land |
| 65.93 % | The river basin under forests and perennial vegetation |
| A | 0.52933319779191 | / | Coefficient of the river basin form |
| m | 0.55022899638651 | / | Coefficient of the watershed development |
| B | 0.51425355720071 | km | Average river basin width |
| a | 0.16539693338553 | / | (A)symmetry of the river basin |
| G | 1.9396240220273 | / | Density of the river network of the basin |
| K | 1.0602621608675 | / | Coefficient of the river basin tortuousness |
| Hsr | 786.90671150847 | m | Average river basin altitude |
| Dsr | 235.90671150847 | m | Average elevation difference of the river basin |
| Isr | 40.459125713222 | % | Average river basin decline |
| Hleb | 432 | m | The height of the local erosion base of the river basin |
| Er | 123.07989944145 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7437961156615 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.9769 | / | Coefficient of the region's permeability |
| S2 | 0.6964858328 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 84.920615373418 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 53.333534639835 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.5036205052634 | / | Coefficient of the river basin erosion |
| Wgod | 1554.9157981503 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.20083238005273 | / | Coefficient of the deposit retention |
| Ggod | 312.27744052413 | m3 god-1 | Real soil losses |
| Ggod km-2 | 200.42580918965 | m3 km-2 god-1 | Real soil losses per km2 |