Latitude: 43.089306 | Longitude: 19.769829 | Country: Montenegro | Year: 2018 |
| F | 5.87915 | km2 | Surface area of the drainage basin |
| Fm | 2.42407 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 3.45508 | km2 | Surface area of greater portion of the drainage basin |
| O | 10.54637 | km | The length of the watershed |
| Lv | 3.23573 | km | Natural length of the main watercourse |
| Lb | 4.4447 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.10637 ","2.85357 ","2.62383 ","2.31367 ","2.20655 ","1.85235 ","1.02699 "] | km | Contour line length |
| f | ["0.76484 ","0.92509 ","1.08386 ","0.83106 ","0.85554 ","0.78880 ","0.44418 ","0.18577 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 540 | m | Lowest altitude in the drainage basin |
| Hmax | 1278 | m | Highest altitude in the draigane basin |
| ΣL | 3.23573 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.96758 | 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 | 0.0739 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.9261 | 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 |
| 6.79 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 93.21 % | 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 |
| 52.81 % | The river basin under forests and perennial vegetation |
| A | 0.63557285373007 | / | Coefficient of the river basin form |
| m | 0.37645240241989 | / | Coefficient of the watershed development |
| B | 1.3227326928702 | km | Average river basin width |
| a | 0.35073437486712 | / | (A)symmetry of the river basin |
| G | 0.55037377852241 | / | Density of the river network of the basin |
| K | 1.0903598218077 | / | Coefficient of the river basin tortuousness |
| Hsr | 840.00958131703 | m | Average river basin altitude |
| Dsr | 300.00958131703 | m | Average elevation difference of the river basin |
| Isr | 25.485537875373 | % | Average river basin decline |
| Hleb | 738 | m | The height of the local erosion base of the river basin |
| Er | 150.86130281993 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7325213778223 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.97783 | / | Coefficient of the region's permeability |
| S2 | 0.7529320954 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 186.02629409468 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 150.81253629141 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.48819516971446 | / | Coefficient of the river basin erosion |
| Wgod | 5476.8968765415 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.26878260620301 | / | Coefficient of the deposit retention |
| Ggod | 1472.094616382 | m3 god-1 | Real soil losses |
| Ggod km-2 | 250.39242345951 | m3 km-2 god-1 | Real soil losses per km2 |