Latitude: 43.07919 | Longitude: 19.784681 | Country: Montenegro | Year: 2018 |
| F | 10.29929 | km2 | Surface area of the drainage basin |
| Fm | 3.29431 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 7.00498 | km2 | Surface area of greater portion of the drainage basin |
| O | 14.30003 | km | The length of the watershed |
| Lv | 4.003 | km | Natural length of the main watercourse |
| Lb | 5.84308 | km | Surface area of greater portion of the drainage basin |
| Liz | ["6.10853 ","7.34426 ","4.27789 ","1.76582 ","1.20790 ","0.81557 "] | km | Contour line length |
| f | ["2.68118 ","3.11941 ","2.38172 ","1.10291 ","0.50458 ","0.37513 ","0.13436 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 545 | m | Lowest altitude in the drainage basin |
| Hmax | 1185 | m | Highest altitude in the draigane basin |
| ΣL | 4.003 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 3.89458 | 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 | 0.1833 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.8167 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.390910153 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.453519217 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.155570630 | 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 | 873.7 | mm | Average annual quantity of precipitation |
| 20.42 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 79.58 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 0 % | 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 |
| 15.56 % | Plough-lands |
| 13.72 % | Orchards and vineyards |
| 6.91 % | Mountain pastures |
| 24.72 % | Meadows |
| 25.41 % | Degraded forests |
| 13.68 % | Well-constituted forests |
| 1.78 % | Depth erosion |
| 1.58 % | 80% of the river basin under rill and gully erosion |
| 1.38 % | 50% of the river basin under rill and gully erosion |
| 1.19 % | 100% of the river basin under surface erosion |
| 24.72 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.59 % | 50% of the river basin under surface erosion |
| 0.4 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 15.56 % | The river basin mostly under plough-land |
| 52.8 % | The river basin under forests and perennial vegetation |
| A | 0.69660400949288 | / | Coefficient of the river basin form |
| m | 0.3518657655853 | / | Coefficient of the watershed development |
| B | 1.7626474393642 | km | Average river basin width |
| a | 0.72056811683135 | / | (A)symmetry of the river basin |
| G | 0.38866756834694 | / | Density of the river network of the basin |
| K | 1.0278386886391 | / | Coefficient of the river basin tortuousness |
| Hsr | 710.05859141747 | m | Average river basin altitude |
| Dsr | 165.05859141747 | m | Average elevation difference of the river basin |
| Isr | 20.894615065699 | % | Average river basin decline |
| Hleb | 640 | m | The height of the local erosion base of the river basin |
| Er | 113.71775558922 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7229738266463 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.94501 | / | Coefficient of the region's permeability |
| S2 | 0.7529320954 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 182.63003916662 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 155.96569211528 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.50694235341003 | / | Coefficient of the river basin erosion |
| Wgod | 10152.545804758 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.21943022500281 | / | Coefficient of the deposit retention |
| Ggod | 2227.7754102893 | m3 god-1 | Real soil losses |
| Ggod km-2 | 216.30378504628 | m3 km-2 god-1 | Real soil losses per km2 |