Latitude: 43.038387 | Longitude: 19.743472 | Country: Montenegro | Year: 2018 |
| F | 50.00087 | km2 | Surface area of the drainage basin |
| Fm | 21.30989 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 28.69098 | km2 | Surface area of greater portion of the drainage basin |
| O | 36.85641 | km | The length of the watershed |
| Lv | 15.49564 | km | Natural length of the main watercourse |
| Lb | 15.97933 | km | Surface area of greater portion of the drainage basin |
| Liz | ["4.01904 ","12.39459 ","27.80832 ","37.80433 ","40.80435 ","28.20570 ","14.65344 ","4.51312 ","2.27256 ","0.35564 "] | km | Contour line length |
| f | ["1.01231 ","2.88213 ","6.47270 ","8.58959 ","10.72667 ","10.17325 ","5.68381 ","3.16581 ","0.90257 ","0.38062 ","0.01141 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 572 | m | Lowest altitude in the drainage basin |
| Hmax | 1503 | m | Highest altitude in the draigane basin |
| ΣL | 21.13298 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 13.62535 | km | The shortest distance between the fountain - head and mouth |
| fp | 0 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0246 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.9754 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.556605141 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.407351930 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.036042929 | 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 | 893.3 | mm | Average annual quantity of precipitation |
| 0.73 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 1.03 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 98.23 % | 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 |
| 3.6 % | Plough-lands |
| 3.11 % | Orchards and vineyards |
| 18.4 % | Mountain pastures |
| 19.23 % | Meadows |
| 36.18 % | Degraded forests |
| 19.48 % | Well-constituted forests |
| 4.73 % | Depth erosion |
| 4.2 % | 80% of the river basin under rill and gully erosion |
| 3.68 % | 50% of the river basin under rill and gully erosion |
| 3.15 % | 100% of the river basin under surface erosion |
| 19.23 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.58 % | 50% of the river basin under surface erosion |
| 1.05 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 3.6 % | The river basin mostly under plough-land |
| 58.77 % | The river basin under forests and perennial vegetation |
| A | 0.46380788079744 | / | Coefficient of the river basin form |
| m | 0.61818121763477 | / | Coefficient of the watershed development |
| B | 3.1290967768987 | km | Average river basin width |
| a | 0.29523846285075 | / | (A)symmetry of the river basin |
| G | 0.42265224585092 | / | Density of the river network of the basin |
| K | 1.1372654647404 | / | Coefficient of the river basin tortuousness |
| Hsr | 955.49673985673 | m | Average river basin altitude |
| Dsr | 383.49673985673 | m | Average elevation difference of the river basin |
| Isr | 34.565616558272 | % | Average river basin decline |
| Hleb | 931 | m | The height of the local erosion base of the river basin |
| Er | 111.44367319391 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.6314539156074 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.99262 | / | Coefficient of the region's permeability |
| S2 | 0.6958875576 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 613.36518311582 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 320.59308252475 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.38998746060057 | / | Coefficient of the river basin erosion |
| Wgod | 34003.085683756 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.2949181023796 | / | Coefficient of the deposit retention |
| Ggod | 10028.125504904 | m3 god-1 | Real soil losses |
| Ggod km-2 | 200.55902037113 | m3 km-2 god-1 | Real soil losses per km2 |