Latitude: 43.070876 | Longitude: 19.789726 | Country: Montenegro | Year: 2018 |
| F | 27.41804 | km2 | Surface area of the drainage basin |
| Fm | 8.95927 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 18.45877 | km2 | Surface area of greater portion of the drainage basin |
| O | 30.97936 | km | The length of the watershed |
| Lv | 6.39141 | km | Natural length of the main watercourse |
| Lb | 12.95975 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.49506 | km | Contour line length |
| f | ["5.12456 ","6.41788 ","7.99236 ","5.26434 ","1.74621 ","0.66440 ","0.14745 ","0.05252 ","0.00833 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 550 | m | Lowest altitude in the drainage basin |
| Hmax | 1314 | m | Highest altitude in the draigane basin |
| ΣL | 8.66268 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 6.05424 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.0281 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0747 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.8972 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.625657604 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.233619677 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.140722719 | 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 |
| 15.68 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 84.32 % | 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 |
| 14.07 % | Plough-lands |
| 4.25 % | Orchards and vineyards |
| 6.76 % | Mountain pastures |
| 12.35 % | Meadows |
| 40.67 % | Degraded forests |
| 21.9 % | Well-constituted forests |
| 1.74 % | Depth erosion |
| 1.54 % | 80% of the river basin under rill and gully erosion |
| 1.35 % | 50% of the river basin under rill and gully erosion |
| 1.16 % | 100% of the river basin under surface erosion |
| 12.35 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.58 % | 50% of the river basin under surface erosion |
| 0.39 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 14.07 % | The river basin mostly under plough-land |
| 66.81 % | The river basin under forests and perennial vegetation |
| A | 0.94517097166353 | / | Coefficient of the river basin form |
| m | 0.34432895375695 | / | Coefficient of the watershed development |
| B | 2.1156303169428 | km | Average river basin width |
| a | 0.69293793429436 | / | (A)symmetry of the river basin |
| G | 0.31594818593889 | / | Density of the river network of the basin |
| K | 1.0556915484024 | / | Coefficient of the river basin tortuousness |
| Hsr | 736.37018948109 | m | Average river basin altitude |
| Dsr | 186.37018948109 | m | Average elevation difference of the river basin |
| Isr | 41.882745812611 | % | Average river basin decline |
| Hleb | 764 | m | The height of the local erosion base of the river basin |
| Er | 106.27580039673 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.6980395862509 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.96073 | / | Coefficient of the region's permeability |
| S2 | 0.703013023 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 316.63281918052 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 343.22493855429 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.53721630879217 | / | Coefficient of the river basin erosion |
| Wgod | 29484.243832512 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.29318255569147 | / | Coefficient of the deposit retention |
| Ggod | 8644.2659594463 | m3 god-1 | Real soil losses |
| Ggod km-2 | 315.27658284277 | m3 km-2 god-1 | Real soil losses per km2 |