Latitude: 42.728154 | Longitude: 19.836015 | Country: Montenegro | Year: 2018 |
| F | 4.43397 | km2 | Surface area of the drainage basin |
| Fm | 1.85186 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 2.58211 | km2 | Surface area of greater portion of the drainage basin |
| O | 9.6491 | km | The length of the watershed |
| Lv | 0.65491 | km | Natural length of the main watercourse |
| Lb | 3.62389 | km | Surface area of greater portion of the drainage basin |
| Liz | ["4.02329 ","3.79075 ","3.40498 ","2.87883 ","2.31531 ","1.93894 ","1.49808 ","0.52992 "] | km | Contour line length |
| f | ["0.84366 ","0.57276 ","0.74182 ","0.63388 ","0.58726 ","0.45977 ","0.37590 ","0.18269 ","0.03624 "] | km2 | The area between the two neighboring contour lines |
| h0 | 800 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 741 | m | Lowest altitude in the drainage basin |
| Hmax | 1503 | m | Highest altitude in the draigane basin |
| ΣL | 0.65491 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 0.61386 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.5726 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.3987 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.0287 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.499253578 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.484862241 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.015884181 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 115 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 9.0 | °C | Average annual air temperature |
| Hgod | 1183.7 | mm | Average annual quantity of precipitation |
| 15.94 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 13.43 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 70.63 % | 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 |
| 1.59 % | Plough-lands |
| 0.57 % | Orchards and vineyards |
| 34.19 % | Mountain pastures |
| 13.73 % | Meadows |
| 9.97 % | Degraded forests |
| 39.96 % | Well-constituted forests |
| 8.79 % | Depth erosion |
| 7.81 % | 80% of the river basin under rill and gully erosion |
| 6.84 % | 50% of the river basin under rill and gully erosion |
| 5.86 % | 100% of the river basin under surface erosion |
| 13.73 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 2.93 % | 50% of the river basin under surface erosion |
| 1.95 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 1.59 % | The river basin mostly under plough-land |
| 50.5 % | The river basin under forests and perennial vegetation |
| A | 2.8730275915775 | / | Coefficient of the river basin form |
| m | 0.087736501854513 | / | Coefficient of the watershed development |
| B | 1.2235387939479 | km | Average river basin width |
| a | 0.32938878702382 | / | (A)symmetry of the river basin |
| G | 0.14770284868865 | / | Density of the river network of the basin |
| K | 1.0668719251947 | / | Coefficient of the river basin tortuousness |
| Hsr | 1033.8433480605 | m | Average river basin altitude |
| Dsr | 292.8433480605 | m | Average elevation difference of the river basin |
| Isr | 45.963549595509 | % | Average river basin decline |
| Hleb | 762 | m | The height of the local erosion base of the river basin |
| Er | 167.15020403232 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.4061303540943 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.53683 | / | Coefficient of the region's permeability |
| S2 | 0.7033261206 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 159.61127192149 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 243.45711055629 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.42936865571343 | / | Coefficient of the river basin erosion |
| Wgod | 4639.0577267313 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.3155304634884 | / | Coefficient of the deposit retention |
| Ggod | 1463.764034665 | m3 god-1 | Real soil losses |
| Ggod km-2 | 330.12492972775 | m3 km-2 god-1 | Real soil losses per km2 |