Latitude: 42.65296 | Longitude: 19.92774 | Country: Montenegro | Year: 2018 |
| F | 32.25843 | km2 | Surface area of the drainage basin |
| Fm | 12.33498 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 19.92345 | km2 | Surface area of greater portion of the drainage basin |
| O | 24.31217 | km | The length of the watershed |
| Lv | 6.90844 | km | Natural length of the main watercourse |
| Lb | 8.88564 | km | Surface area of greater portion of the drainage basin |
| Liz | ["3.38501 ","8.76982 ","10.84120 ","13.73594 ","14.56722 ","14.59249 ","14.88688 ","14.90037 ","13.29120 ","12.03854 ","8.57967 ","2.07198 "] | km | Contour line length |
| f | ["0.47946 ","1.80118 ","2.25785 ","2.94814 ","3.19298 ","3.39597 ","3.09540 ","3.54191 ","3.63426 ","3.33728 ","2.75455 ","1.48562 ","0.33383 "] | km2 | The area between the two neighboring contour lines |
| h0 | 900 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 879 | m | Lowest altitude in the drainage basin |
| Hmax | 2077 | m | Highest altitude in the draigane basin |
| ΣL | 10.18487 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 5.4377 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.1344 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0804 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.7852 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.39 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.59 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.02 | 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 |
| 3.73 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 83.66 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 12.61 % | 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 |
| 1.99 % | Plough-lands |
| 1 % | Orchards and vineyards |
| 44.82 % | Mountain pastures |
| 12.95 % | Meadows |
| 9.06 % | Degraded forests |
| 30.18 % | Well-constituted forests |
| 2 % | Depth erosion |
| 12 % | 80% of the river basin under rill and gully erosion |
| 11 % | 50% of the river basin under rill and gully erosion |
| 10 % | 100% of the river basin under surface erosion |
| 16 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 5 % | 50% of the river basin under surface erosion |
| 3 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 2 % | The river basin mostly under plough-land |
| 39 % | The river basin under forests and perennial vegetation |
| A | 0.68624365992901 | / | Coefficient of the river basin form |
| m | 0.34312585559727 | / | Coefficient of the watershed development |
| B | 3.6304002863046 | km | Average river basin width |
| a | 0.47047980946376 | / | (A)symmetry of the river basin |
| G | 0.31572739280864 | / | Density of the river network of the basin |
| K | 1.2704709711827 | / | Coefficient of the river basin tortuousness |
| Hsr | 1455.8345562695 | m | Average river basin altitude |
| Dsr | 576.8345562695 | m | Average elevation difference of the river basin |
| Isr | 40.814236774697 | % | Average river basin decline |
| Hleb | 1198 | m | The height of the local erosion base of the river basin |
| Er | 160.00963652762 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.0946746295478 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.89524 | / | Coefficient of the region's permeability |
| S2 | 0.726 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 604.22229997006 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 295.00966672736 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.95393920141695 | / | Temperature coefficient of the region |
| Z | 0.50461483704605 | / | Coefficient of the river basin erosion |
| Wgod | 40971.466483167 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.44295943001821 | / | Coefficient of the deposit retention |
| Ggod | 18148.697440394 | m3 god-1 | Real soil losses |
| Ggod km-2 | 562.60324635743 | m3 km-2 god-1 | Real soil losses per km2 |