Latitude: 42.833783 | Longitude: 19.836532 | Country: Montenegro | Year: 2018 |
| F | 133.88747 | km2 | Surface area of the drainage basin |
| Fm | 52.94323 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 80.94424 | km2 | Surface area of greater portion of the drainage basin |
| O | 62.49592 | km | The length of the watershed |
| Lv | 26.90531 | km | Natural length of the main watercourse |
| Lb | 21.98716 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.20982 ","6.71367 ","7.20292 ","19.79409 ","31.53289 ","41.96885 ","48.15472 ","63.55594 ","67.04959 ","73.48834 ","59.50381 ","49.90986 ","29.13672 ","16.76063 ","2.21565 "] | km | Contour line length |
| f | ["2.47489 ","1.44993 ","1.15302 ","3.48991 ","5.32819 ","8.18507 ","10.87748 ","14.87302 ","16.16024 ","17.61977 ","17.89506 ","14.90414 ","9.97085 ","6.48003 ","2.83956 ","0.18631 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 685 | m | Lowest altitude in the drainage basin |
| Hmax | 2139 | m | Highest altitude in the draigane basin |
| ΣL | 69.1736 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 22.4919 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.3166 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0501 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.6333 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.523996482 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.444460878 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.031542639 | 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 |
| 3.21 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 74.92 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 6.49 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 15.37 % | Brown forest soils and Mountain soils |
| 0 % | Epieugleysol and Marshlands |
| 0 % | Good structured Chernozems and alluvial well-structured deposits |
| 0 % | Bare, compact igneous |
| 0.01 % | Bare lands |
| 3.15 % | Plough-lands |
| 1.04 % | Orchards and vineyards |
| 24.61 % | Mountain pastures |
| 18.79 % | Meadows |
| 31.44 % | Degraded forests |
| 20.96 % | Well-constituted forests |
| 6.33 % | Depth erosion |
| 5.63 % | 80% of the river basin under rill and gully erosion |
| 4.92 % | 50% of the river basin under rill and gully erosion |
| 4.22 % | 100% of the river basin under surface erosion |
| 18.79 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 2.11 % | 50% of the river basin under surface erosion |
| 1.41 % | 20% of the river basin under surface erosion |
| 0.01 % | There are smaller slides in the watercourse beds |
| 3.15 % | The river basin mostly under plough-land |
| 53.44 % | The river basin under forests and perennial vegetation |
| A | 0.45294792737939 | / | Coefficient of the river basin form |
| m | 0.65593846742225 | / | Coefficient of the watershed development |
| B | 6.0893480558653 | km | Average river basin width |
| a | 0.41827678124025 | / | (A)symmetry of the river basin |
| G | 0.51665476986009 | / | Density of the river network of the basin |
| K | 1.196222195546 | / | Coefficient of the river basin tortuousness |
| Hsr | 1489.5333063654 | m | Average river basin altitude |
| Dsr | 804.5333063654 | m | Average elevation difference of the river basin |
| Isr | 38.778647471642 | % | Average river basin decline |
| Hleb | 1454 | m | The height of the local erosion base of the river basin |
| Er | 136.05971285542 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.2550973659666 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.79501 | / | Coefficient of the region's permeability |
| S2 | 0.7015092306 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 1453.7558754517 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 460.91745924746 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.48530582590298 | / | Coefficient of the river basin erosion |
| Wgod | 134283.62442727 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.38427221591528 | / | Coefficient of the deposit retention |
| Ggod | 51601.465919802 | m3 god-1 | Real soil losses |
| Ggod km-2 | 385.40922402822 | m3 km-2 god-1 | Real soil losses per km2 |