Latitude: 42.619435 | Longitude: 19.940214 | Country: Montenegro | Year: 2018 |
| F | 88.70148 | km2 | Surface area of the drainage basin |
| Fm | 41.3019 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 47.39958 | km2 | Surface area of greater portion of the drainage basin |
| O | 40.01784 | km | The length of the watershed |
| Lv | 16.33554 | km | Natural length of the main watercourse |
| Lb | 16.65007 | km | Surface area of greater portion of the drainage basin |
| Liz | ["9.03277 ","12.68366 ","19.31676 ","22.54119 ","28.49542 ","25.49528 ","36.24810 ","39.65107 ","37.47339 ","40.42133 ","29.72351 ","22.40549 ","13.09430 ","1.06107 ","0.1 "] | km | Contour line length |
| f | ["1.80258 ","2.43246 ","3.78096 ","4.73565 ","6.11416 ","6.65865 ","8.33182 ","8.98081 ","10.71202 ","10.17923 ","10.26820 ","7.46545 ","4.46962 ","2.71639 ","0.05349 ","0.1 "] | km2 | The area between the two neighboring contour lines |
| h0 | 1000 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 906 | m | Lowest altitude in the drainage basin |
| Hmax | 2426 | m | Highest altitude in the draigane basin |
| ΣL | 36.61443 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 12.68833 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.0041 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.2417 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.7542 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.489992714 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.494120993 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.015886293 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 89.4 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 8.1 | °C | Average annual air temperature |
| Hgod | 1345.4 | mm | Average annual quantity of precipitation |
| 8.59 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 85.54 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 0 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 5.87 % | 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 |
| 0.15 % | Orchards and vineyards |
| 40.96 % | Mountain pastures |
| 8.3 % | Meadows |
| 10 % | Degraded forests |
| 39 % | Well-constituted forests |
| 10.53 % | Depth erosion |
| 9.36 % | 80% of the river basin under rill and gully erosion |
| 8.19 % | 50% of the river basin under rill and gully erosion |
| 7.02 % | 100% of the river basin under surface erosion |
| 8.3 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 3.51 % | 50% of the river basin under surface erosion |
| 2.34 % | 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 |
| 49.15 % | The river basin under forests and perennial vegetation |
| A | 0.47769946998997 | / | Coefficient of the river basin form |
| m | 0.48928638406835 | / | Coefficient of the watershed development |
| B | 5.3273938187647 | km | Average river basin width |
| a | 0.13748767213354 | / | (A)symmetry of the river basin |
| G | 0.41278262775322 | / | Density of the river network of the basin |
| K | 1.2874460232355 | / | Coefficient of the river basin tortuousness |
| Hsr | 1681.7617839071 | m | Average river basin altitude |
| Dsr | 775.7617839071 | m | Average elevation difference of the river basin |
| Isr | 38.076404136662 | % | Average river basin decline |
| Hleb | 1520 | m | The height of the local erosion base of the river basin |
| Er | 157.65617973967 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.056769018737 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.92503 | / | Coefficient of the region's permeability |
| S2 | 0.7051787158 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 1161.9277534439 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 382.62114821943 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.95393920141695 | / | Temperature coefficient of the region |
| Z | 0.45396633067502 | / | Coefficient of the river basin erosion |
| Wgod | 109392.69555868 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.42313483470199 | / | Coefficient of the deposit retention |
| Ggod | 46287.860152827 | m3 god-1 | Real soil losses |
| Ggod km-2 | 521.83864522697 | m3 km-2 god-1 | Real soil losses per km2 |