Latitude: 42.931179 | Longitude: 19.853992 | Country: Montenegro | Year: 2018 |
| F | 6.84925 | km2 | Surface area of the drainage basin |
| Fm | 1.99876 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 4.85049 | km2 | Surface area of greater portion of the drainage basin |
| O | 11.19337 | km | The length of the watershed |
| Lv | 1.63664 | km | Natural length of the main watercourse |
| Lb | 4.36078 | km | Surface area of greater portion of the drainage basin |
| Liz | ["3.97953 ","3.98426 ","3.79276 ","3.54904 ","2.24257 ","2.09055 ","0.20457 "] | km | Contour line length |
| f | ["1.39718 ","0.95068 ","1.26481 ","1.04352 ","0.86878 ","0.72280 ","0.59109 ","0.01039 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 649 | m | Lowest altitude in the drainage basin |
| Hmax | 1318 | m | Highest altitude in the draigane basin |
| ΣL | 2.33664 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 1.39107 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.3868 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1983 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.4149 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.598511436 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.308099763 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.093388801 | 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 |
| 9.72 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 75.23 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 15.05 % | 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 |
| 9.34 % | Plough-lands |
| 1.37 % | Orchards and vineyards |
| 10.63 % | Mountain pastures |
| 18.81 % | Meadows |
| 35.91 % | Degraded forests |
| 23.94 % | Well-constituted forests |
| 2.73 % | Depth erosion |
| 2.43 % | 80% of the river basin under rill and gully erosion |
| 2.13 % | 50% of the river basin under rill and gully erosion |
| 1.82 % | 100% of the river basin under surface erosion |
| 18.81 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.91 % | 50% of the river basin under surface erosion |
| 0.61 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 9.34 % | The river basin mostly under plough-land |
| 61.22 % | The river basin under forests and perennial vegetation |
| A | 1.3336513527715 | / | Coefficient of the river basin form |
| m | 0.17641142986201 | / | Coefficient of the watershed development |
| B | 1.5706479116121 | km | Average river basin width |
| a | 0.83271307077417 | / | (A)symmetry of the river basin |
| G | 0.34115268095047 | / | Density of the river network of the basin |
| K | 1.1765331723062 | / | Coefficient of the river basin tortuousness |
| Hsr | 907.79901741067 | m | Average river basin altitude |
| Dsr | 258.79901741067 | m | Average elevation difference of the river basin |
| Isr | 28.971464028908 | % | Average river basin decline |
| Hleb | 669 | m | The height of the local erosion base of the river basin |
| Er | 131.63321556725 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7570833937341 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.70843 | / | Coefficient of the region's permeability |
| S2 | 0.698975473 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 186.48861443906 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 216.39433493065 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.43222360885981 | / | Coefficient of the river basin erosion |
| Wgod | 5984.610463091 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.29252577473233 | / | Coefficient of the deposit retention |
| Ggod | 1750.6528121869 | m3 god-1 | Real soil losses |
| Ggod km-2 | 255.59773875781 | m3 km-2 god-1 | Real soil losses per km2 |