Latitude: 42.955017 | Longitude: 19.852923 | Country: Montenegro | Year: 2018 |
| F | 3.5542 | km2 | Surface area of the drainage basin |
| Fm | 1.7589 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 1.7953 | km2 | Surface area of greater portion of the drainage basin |
| O | 10.56262 | km | The length of the watershed |
| Lv | 3.377 | km | Natural length of the main watercourse |
| Lb | 3.13813 | km | Surface area of greater portion of the drainage basin |
| Liz | ["3.77434 ","1.43496 ","1.25747 "] | km | Contour line length |
| f | ["2.12629 ","0.88502 ","0.32976 ","0.21313 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 674 | m | Lowest altitude in the drainage basin |
| Hmax | 973 | m | Highest altitude in the draigane basin |
| ΣL | 6.70854 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.80589 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.3788 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.6212 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.385405455 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.491927055 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.122667490 | 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 |
| 94.45 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 0 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 5.55 % | 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 |
| 12.27 % | Plough-lands |
| 5.45 % | Orchards and vineyards |
| 15.82 % | Mountain pastures |
| 27.92 % | Meadows |
| 23.12 % | Degraded forests |
| 15.42 % | Well-constituted forests |
| 4.07 % | Depth erosion |
| 3.62 % | 80% of the river basin under rill and gully erosion |
| 3.16 % | 50% of the river basin under rill and gully erosion |
| 2.71 % | 100% of the river basin under surface erosion |
| 27.92 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.36 % | 50% of the river basin under surface erosion |
| 0.9 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 12.27 % | The river basin mostly under plough-land |
| 43.99 % | The river basin under forests and perennial vegetation |
| A | 0.60992327509624 | / | Coefficient of the river basin form |
| m | 0.50530686364689 | / | Coefficient of the watershed development |
| B | 1.1325853294797 | km | Average river basin width |
| a | 0.020482809070958 | / | (A)symmetry of the river basin |
| G | 1.8874964830342 | / | Density of the river network of the basin |
| K | 1.203539696852 | / | Coefficient of the river basin tortuousness |
| Hsr | 732.7720654437 | m | Average river basin altitude |
| Dsr | 58.7720654437 | m | Average elevation difference of the river basin |
| Isr | 18.194727364808 | % | Average river basin decline |
| Hleb | 299 | m | The height of the local erosion base of the river basin |
| Er | 69.316376183872 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3706506762654 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.58636 | / | Coefficient of the region's permeability |
| S2 | 0.747452407 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 64.018561242033 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 23.456098777095 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.762027362184 | / | Coefficient of the river basin erosion |
| Wgod | 7013.8677652118 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.11779926299468 | / | Coefficient of the deposit retention |
| Ggod | 826.2284534841 | m3 god-1 | Real soil losses |
| Ggod km-2 | 232.46537996851 | m3 km-2 god-1 | Real soil losses per km2 |