Latitude: 42.922158 | Longitude: 19.860094 | Country: Montenegro | Year: 2018 |
| F | 77.74127 | km2 | Surface area of the drainage basin |
| Fm | 32.42818 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 45.31309 | km2 | Surface area of greater portion of the drainage basin |
| O | 47.69818 | km | The length of the watershed |
| Lv | 18.63097 | km | Natural length of the main watercourse |
| Lb | 16.9459 | km | Surface area of greater portion of the drainage basin |
| Liz | ["5.10930 ","7.81371 ","19.51511 ","29.49667 ","35.41558 ","34.12410 ","34.91699 ","38.16232 ","37.39740 ","35.58561 ","19.90150 ","21.86124 ","5.85499 "] | km | Contour line length |
| f | ["1.89333 ","2.81206 ","3.89692 ","4.81249 ","6.64300 ","7.76400 ","7.31605 ","7.67770 ","8.51072 ","8.20787 ","8.21651 ","5.50208 ","3.77999 ","0.70854 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 681 | m | Lowest altitude in the drainage basin |
| Hmax | 1963 | m | Highest altitude in the draigane basin |
| ΣL | 32.92231 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 12.67805 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.7834 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1577 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.0589 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.494437420 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.477727166 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.027835414 | 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 | 944.3 | mm | Average annual quantity of precipitation |
| 5.87 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 84.72 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 9.41 % | 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 |
| 2.78 % | Plough-lands |
| 1.03 % | Orchards and vineyards |
| 34.42 % | Mountain pastures |
| 12.32 % | Meadows |
| 29.67 % | Degraded forests |
| 19.78 % | Well-constituted forests |
| 8.85 % | Depth erosion |
| 7.87 % | 80% of the river basin under rill and gully erosion |
| 6.88 % | 50% of the river basin under rill and gully erosion |
| 5.9 % | 100% of the river basin under surface erosion |
| 12.32 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 2.95 % | 50% of the river basin under surface erosion |
| 1.97 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 2.78 % | The river basin mostly under plough-land |
| 50.48 % | The river basin under forests and perennial vegetation |
| A | 0.49923031919433 | / | Coefficient of the river basin form |
| m | 0.59608023138098 | / | Coefficient of the watershed development |
| B | 4.5876152933748 | km | Average river basin width |
| a | 0.33148184998779 | / | (A)symmetry of the river basin |
| G | 0.42348562095783 | / | Density of the river network of the basin |
| K | 1.4695453953881 | / | Coefficient of the river basin tortuousness |
| Hsr | 1329.0816431864 | m | Average river basin altitude |
| Dsr | 648.0816431864 | m | Average elevation difference of the river basin |
| Isr | 41.825213300477 | % | Average river basin decline |
| Hleb | 1282 | m | The height of the local erosion base of the river basin |
| Er | 137.42800585229 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.2851355546211 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.48265 | / | Coefficient of the region's permeability |
| S2 | 0.7066795988 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 994.23758624287 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 217.56795692625 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.56758334561869 | / | Coefficient of the river basin erosion |
| Wgod | 98617.947375407 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.38838254028279 | / | Coefficient of the deposit retention |
| Ggod | 38301.488919135 | m3 god-1 | Real soil losses |
| Ggod km-2 | 492.67897114538 | m3 km-2 god-1 | Real soil losses per km2 |