Latitude: 42.930473 | Longitude: 19.861783 | Country: Montenegro | Year: 2018 |
| F | 207.80982 | km2 | Surface area of the drainage basin |
| Fm | 87.90757 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 119.90225 | km2 | Surface area of greater portion of the drainage basin |
| O | 70.78064 | km | The length of the watershed |
| Lv | 26.82035 | km | Natural length of the main watercourse |
| Lb | 26.83658 | km | Surface area of greater portion of the drainage basin |
| Liz | ["19.71679 ","59.22214 ","70.36777 ","66.38101 ","66.86189 ","85.90636 ","75.20515 ","57.83770 ","51.75069 ","15.78357 ","3.37545 "] | km | Contour line length |
| f | ["3.23978 ","12.59470 ","22.48905 ","21.76435 ","18.73432 ","21.47152 ","29.89405 ","24.17672 ","28.32979 ","20.96133 ","3.66651 ","0.48771 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 635 | m | Lowest altitude in the drainage basin |
| Hmax | 1758 | m | Highest altitude in the draigane basin |
| ΣL | 45.62923 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 20.9632 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.4405 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1875 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.372 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.500071451 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.372352518 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.127576031 | 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 | 983.7 | mm | Average annual quantity of precipitation |
| 3.22 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 71.48 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 25.29 % | 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 |
| 12.76 % | Plough-lands |
| 0.9 % | Orchards and vineyards |
| 21.09 % | Mountain pastures |
| 15.25 % | Meadows |
| 30 % | Degraded forests |
| 20 % | Well-constituted forests |
| 5.42 % | Depth erosion |
| 4.82 % | 80% of the river basin under rill and gully erosion |
| 4.22 % | 50% of the river basin under rill and gully erosion |
| 3.61 % | 100% of the river basin under surface erosion |
| 15.25 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.81 % | 50% of the river basin under surface erosion |
| 1.2 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 12.76 % | The river basin mostly under plough-land |
| 50.91 % | The river basin under forests and perennial vegetation |
| A | 0.51461762430393 | / | Coefficient of the river basin form |
| m | 0.52483945507354 | / | Coefficient of the watershed development |
| B | 7.7435284227722 | km | Average river basin width |
| a | 0.3079226958572 | / | (A)symmetry of the river basin |
| G | 0.21957205872177 | / | Density of the river network of the basin |
| K | 1.2794015226683 | / | Coefficient of the river basin tortuousness |
| Hsr | 1184.8865984293 | m | Average river basin altitude |
| Dsr | 549.8865984293 | m | Average elevation difference of the river basin |
| Isr | 27.544825360034 | % | Average river basin decline |
| Hleb | 1123 | m | The height of the local erosion base of the river basin |
| Er | 94.148491743606 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.5727138788396 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.67945 | / | Coefficient of the region's permeability |
| S2 | 0.725500916 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 1497.3354345252 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 597.37761593297 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.46009704229773 | / | Coefficient of the river basin erosion |
| Wgod | 199420.76123502 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.33887216207105 | / | Coefficient of the deposit retention |
| Ggod | 67578.144521565 | m3 god-1 | Real soil losses |
| Ggod km-2 | 325.19225762077 | m3 km-2 god-1 | Real soil losses per km2 |