Latitude: 42.983814 | Longitude: 19.76365 | Country: Montenegro | Year: 2018 |
| F | 8.75632 | km2 | Surface area of the drainage basin |
| Fm | 3.20485 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 5.55147 | km2 | Surface area of greater portion of the drainage basin |
| O | 14.52221 | km | The length of the watershed |
| Lv | 1.35435 | km | Natural length of the main watercourse |
| Lb | 6.00371 | km | Surface area of greater portion of the drainage basin |
| Liz | ["8.13329 ","9.01899 ","9.60111 ","5.81637 ","1.53708 "] | km | Contour line length |
| f | ["1.71501 ","1.88908 ","2.36487 ","1.68284 ","0.96118 ","0.14334 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 586 | m | Lowest altitude in the drainage basin |
| Hmax | 1018 | m | Highest altitude in the draigane basin |
| ΣL | 1.35435 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 1.27769 | 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 | 0.0753 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.9247 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.569872890 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.360011498 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.070115612 | 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 |
| 19.42 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 80.58 % | 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 |
| 7.01 % | Plough-lands |
| 11.11 % | Orchards and vineyards |
| 7.43 % | Mountain pastures |
| 17.45 % | Meadows |
| 37.04 % | Degraded forests |
| 19.95 % | Well-constituted forests |
| 1.91 % | Depth erosion |
| 1.7 % | 80% of the river basin under rill and gully erosion |
| 1.49 % | 50% of the river basin under rill and gully erosion |
| 1.27 % | 100% of the river basin under surface erosion |
| 17.45 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.64 % | 50% of the river basin under surface erosion |
| 0.42 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 7.01 % | The river basin mostly under plough-land |
| 68.11 % | The river basin under forests and perennial vegetation |
| A | 2.090915162255 | / | Coefficient of the river basin form |
| m | 0.12911157167461 | / | Coefficient of the watershed development |
| B | 1.4584848368759 | km | Average river basin width |
| a | 0.53598315273996 | / | (A)symmetry of the river basin |
| G | 0.15467114038774 | / | Density of the river network of the basin |
| K | 1.0599989042726 | / | Coefficient of the river basin tortuousness |
| Hsr | 743.088476666 | m | Average river basin altitude |
| Dsr | 157.088476666 | m | Average elevation difference of the river basin |
| Isr | 38.951111882617 | % | Average river basin decline |
| Hleb | 432 | m | The height of the local erosion base of the river basin |
| Er | 79.938034920789 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7625464499834 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.97741 | / | Coefficient of the region's permeability |
| S2 | 0.7000485444 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 164.27916164688 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 414.25179211989 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.53881613106985 | / | Coefficient of the river basin erosion |
| Wgod | 9670.4639924939 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.26604569682508 | / | Coefficient of the deposit retention |
| Ggod | 2572.7853315048 | m3 god-1 | Real soil losses |
| Ggod km-2 | 293.82038704671 | m3 km-2 god-1 | Real soil losses per km2 |