Latitude: 42.655985 | Longitude: 19.90641 | Country: Montenegro | Year: 2018 |
| F | 8.37729 | km2 | Surface area of the drainage basin |
| Fm | 3.21016 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 5.16713 | km2 | Surface area of greater portion of the drainage basin |
| O | 14.87242 | km | The length of the watershed |
| Lv | 5.49795 | km | Natural length of the main watercourse |
| Lb | 6.40713 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.63084 ","3.34422 ","3.84844 ","4.23396 ","3.89224 ","2.95327 ","2.6569 ","2.9065 ","3.0454 ","3.16974 ","1.95251 ","1.25336 ","0.25212 ","0.10000 "] | km | Contour line length |
| f | ["1.36782 ","0.66695 ","0.77565 ","0.8747 ","0.9344 ","0.78505 ","0.55176 ","0.58917 ","0.46316 ","0.49859 ","0.45822 ","0.29376 ","0.09634 ","0.02062 ","0.10000 "] | km2 | The area between the two neighboring contour lines |
| h0 | 900 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 845 | m | Lowest altitude in the drainage basin |
| Hmax | 2211 | m | Highest altitude in the draigane basin |
| ΣL | 5.49795 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 4.35858 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.1357 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1629 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.7014 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.583741637 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.408709233 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.007549130 | 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 | 1182.3 | mm | Average annual quantity of precipitation |
| 15.55 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 62.38 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 22.07 % | 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 |
| 0.74 % | Plough-lands |
| 0.61 % | Orchards and vineyards |
| 24.01 % | Mountain pastures |
| 15.45 % | Meadows |
| 17.99 % | Degraded forests |
| 41.2 % | Well-constituted forests |
| 6.3 % | Depth erosion |
| 5.6 % | 80% of the river basin under rill and gully erosion |
| 4.9 % | 50% of the river basin under rill and gully erosion |
| 4.2 % | 100% of the river basin under surface erosion |
| 15.76 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 2.1 % | 50% of the river basin under surface erosion |
| 1.4 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 0.75 % | The river basin mostly under plough-land |
| 58.99 % | The river basin under forests and perennial vegetation |
| A | 0.52749150137779 | / | Coefficient of the river basin form |
| m | 0.53585104128542 | / | Coefficient of the watershed development |
| B | 1.307494931428 | km | Average river basin width |
| a | 0.46720836929365 | / | (A)symmetry of the river basin |
| G | 0.65629218995642 | / | Density of the river network of the basin |
| K | 1.2614085321366 | / | Coefficient of the river basin tortuousness |
| Hsr | 1325.9790994462 | m | Average river basin altitude |
| Dsr | 480.9790994462 | m | Average elevation difference of the river basin |
| Isr | 43.259216285935 | % | Average river basin decline |
| Hleb | 1366 | m | The height of the local erosion base of the river basin |
| Er | 255.57886620057 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.1022813277418 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.86971 | / | Coefficient of the region's permeability |
| S2 | 0.6847614986 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 281.16702059095 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 97.361239418983 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.95393920141695 | / | Temperature coefficient of the region |
| Z | 0.41670376056399 | / | Coefficient of the river basin erosion |
| Wgod | 7984.411986772 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.34515141916523 | / | Coefficient of the deposit retention |
| Ggod | 2755.8311284342 | m3 god-1 | Real soil losses |
| Ggod km-2 | 328.96451339684 | m3 km-2 god-1 | Real soil losses per km2 |