Latitude: 43.061861 | Longitude: 19.765378 | Country: Montenegro | Year: 2018 |
| F | 3.04722 | km2 | Surface area of the drainage basin |
| Fm | 1.33162 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 1.7156 | km2 | Surface area of greater portion of the drainage basin |
| O | 7.42855 | km | The length of the watershed |
| Lv | 1.17361 | km | Natural length of the main watercourse |
| Lb | 2.98208 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.23821 ","1.87280 ","1.39779 "] | km | Contour line length |
| f | ["1.47046 ","0.66148 ","0.66309 ","0.25219 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 553 | m | Lowest altitude in the drainage basin |
| Hmax | 828 | m | Highest altitude in the draigane basin |
| ΣL | 1.17361 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 1.08767 | 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 | 0.4242 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.5758 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.570047170 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.280760474 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.149192356 | 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 |
| 39.92 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 60.08 % | 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 |
| 14.92 % | Plough-lands |
| 5.88 % | Orchards and vineyards |
| 5.91 % | Mountain pastures |
| 16.29 % | Meadows |
| 37.05 % | Degraded forests |
| 19.95 % | Well-constituted forests |
| 1.52 % | Depth erosion |
| 1.35 % | 80% of the river basin under rill and gully erosion |
| 1.18 % | 50% of the river basin under rill and gully erosion |
| 1.01 % | 100% of the river basin under surface erosion |
| 16.29 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.51 % | 50% of the river basin under surface erosion |
| 0.34 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 14.92 % | The river basin mostly under plough-land |
| 62.89 % | The river basin under forests and perennial vegetation |
| A | 1.2342833223984 | / | Coefficient of the river basin form |
| m | 0.18965616489762 | / | Coefficient of the watershed development |
| B | 1.0218438137139 | km | Average river basin width |
| a | 0.25201987385223 | / | (A)symmetry of the river basin |
| G | 0.38514121067727 | / | Density of the river network of the basin |
| K | 1.0790129359089 | / | Coefficient of the river basin tortuousness |
| Hsr | 649.86523782333 | m | Average river basin altitude |
| Dsr | 96.86523782333 | m | Average elevation difference of the river basin |
| Isr | 18.078117103458 | % | Average river basin decline |
| Hleb | 275 | m | The height of the local erosion base of the river basin |
| Er | 66.253201413827 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7663493042462 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.87274 | / | Coefficient of the region's permeability |
| S2 | 0.7158290372 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 76.10012692368 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 103.65041044256 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.48634368558007 | / | Coefficient of the river basin erosion |
| Wgod | 2822.5948071498 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.15183520732756 | / | Coefficient of the deposit retention |
| Ggod | 428.56926774527 | m3 god-1 | Real soil losses |
| Ggod km-2 | 140.64270638328 | m3 km-2 god-1 | Real soil losses per km2 |