Latitude: 43.014343 | Longitude: 19.730621 | Country: Montenegro | Year: 2018 |
| F | 3.11484 | km2 | Surface area of the drainage basin |
| Fm | 1.10431 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 2.01053 | km2 | Surface area of greater portion of the drainage basin |
| O | 9.04999 | km | The length of the watershed |
| Lv | 3.05494 | km | Natural length of the main watercourse |
| Lb | 3.79687 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.96111 ","2.67691 ","3.95387 ","4.51106 ","3.04726 ","2.8391 ","1.99244 ","1.14 "] | km | Contour line length |
| f | ["2.80222 ","0.24287 ","0.46999 ","0.5509 ","0.42817 ","0.38134 ","0.36028 ","0.23723 ","0.90068 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 50 | m | Equidistance |
| Hmin | 552 | m | Lowest altitude in the drainage basin |
| Hmax | 983 | m | Highest altitude in the draigane basin |
| ΣL | 4.6904 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.80611 | 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 | 0.0855 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.9145 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.449512057 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.409614519 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.140873424 | 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 |
| 18.55 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 81.45 % | 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 |
| 14.09 % | Plough-lands |
| 11 % | Orchards and vineyards |
| 6.52 % | Mountain pastures |
| 23.44 % | Meadows |
| 29.22 % | Degraded forests |
| 15.73 % | Well-constituted forests |
| 1.68 % | Depth erosion |
| 1.49 % | 80% of the river basin under rill and gully erosion |
| 1.3 % | 50% of the river basin under rill and gully erosion |
| 1.12 % | 100% of the river basin under surface erosion |
| 23.44 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.56 % | 50% of the river basin under surface erosion |
| 0.37 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 14.09 % | The river basin mostly under plough-land |
| 55.95 % | The river basin under forests and perennial vegetation |
| A | 0.57767028157672 | / | Coefficient of the river basin form |
| m | 0.48829230623438 | / | Coefficient of the watershed development |
| B | 0.82037046303929 | km | Average river basin width |
| a | 0.58187258414557 | / | (A)symmetry of the river basin |
| G | 1.5058237341244 | / | Density of the river network of the basin |
| K | 1.0886743570281 | / | Coefficient of the river basin tortuousness |
| Hsr | 1455.6591799258 | m | Average river basin altitude |
| Dsr | 903.6591799258 | m | Average elevation difference of the river basin |
| Isr | 33.905032040169 | % | Average river basin decline |
| Hleb | 431 | m | The height of the local erosion base of the river basin |
| Er | 103.26864096877 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7349314679035 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.97435 | / | Coefficient of the region's permeability |
| S2 | 0.7382722734 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 235.00099738342 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 169.4195809817 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.56141518924913 | / | Coefficient of the river basin erosion |
| Wgod | 3658.6998684316 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.4381083166953 | / | Coefficient of the deposit retention |
| Ggod | 1602.9068406519 | m3 god-1 | Real soil losses |
| Ggod km-2 | 514.60326715077 | m3 km-2 god-1 | Real soil losses per km2 |