Latitude: 42.639204 | Longitude: 19.935218 | Country: Montenegro | Year: 2018 |
| F | 1.71344 | km2 | Surface area of the drainage basin |
| Fm | 0.76431 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 0.94913 | km2 | Surface area of greater portion of the drainage basin |
| O | 6.45006 | km | The length of the watershed |
| Lv | 1.42343 | km | Natural length of the main watercourse |
| Lb | 2.6646 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.261558 ","0.905049 ","1.0548 ","1.212138 ","1.34163 ","1.354167 ","1.24047 ","1.091133 ","1.089738 ","1.064502 ","1.049994 ","1.293858 ","1.194219 ","1.08999 ","0.854883 ","0.534033 ","0.368307 ","0.244101 "] | km | Contour line length |
| f | ["0.0138288 ","0.0788018 ","0.1011102 ","0.1186542 ","0.1418914 ","0.1085062 ","0.1267812 ","0.1081794 ","0.103157 ","0.0776494 ","0.0957524 ","0.1020734 ","0.1109314 ","0.0946086 ","0.1132362 ","0.056373 ","0.0948408 ","0.0520902 ","0.0 | km2 | The area between the two neighboring contour lines |
| h0 | 900 | m | Altitude of the first contour line |
| Δh | 50 | m | Equidistance |
| Hmin | 870 | m | Lowest altitude in the drainage basin |
| Hmax | 1778 | m | Highest altitude in the draigane basin |
| ΣL | 1.42343 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 1.24777 | 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 | 0.156 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.844 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.562633764 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.387425290 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.049940946 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 89.4 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 8.1 | °C | Average annual air temperature |
| Hgod | 1182.3 | mm | Average annual quantity of precipitation |
| 15.76 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 84.24 % | 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 |
| 4.99 % | Plough-lands |
| 1.5 % | Orchards and vineyards |
| 9.13 % | Mountain pastures |
| 28.11 % | Meadows |
| 12.51 % | Degraded forests |
| 43.76 % | Well-constituted forests |
| 2.35 % | Depth erosion |
| 2.09 % | 80% of the river basin under rill and gully erosion |
| 1.83 % | 50% of the river basin under rill and gully erosion |
| 1.57 % | 100% of the river basin under surface erosion |
| 28.11 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.78 % | 50% of the river basin under surface erosion |
| 0.52 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 4.99 % | The river basin mostly under plough-land |
| 57.76 % | The river basin under forests and perennial vegetation |
| A | 0.88361331431823 | / | Coefficient of the river basin form |
| m | 0.30675858943571 | / | Coefficient of the watershed development |
| B | 0.64303835472491 | km | Average river basin width |
| a | 0.21572976001494 | / | (A)symmetry of the river basin |
| G | 0.83074400037352 | / | Density of the river network of the basin |
| K | 1.1407791500036 | / | Coefficient of the river basin tortuousness |
| Hsr | 1382.1793204314 | m | Average river basin altitude |
| Dsr | 512.1793204314 | m | Average elevation difference of the river basin |
| Isr | 50.321487767299 | % | Average river basin decline |
| Hleb | 908 | m | The height of the local erosion base of the river basin |
| Er | 252.62059314954 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.1331697855215 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.9532 | / | Coefficient of the region's permeability |
| S2 | 0.6974614364 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 131.21847069973 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 87.348699391567 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.95393920141695 | / | Temperature coefficient of the region |
| Z | 0.40347490283018 | / | Coefficient of the river basin erosion |
| Wgod | 1555.9367842345 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.31821919146491 | / | Coefficient of the deposit retention |
| Ggod | 495.12894544961 | m3 god-1 | Real soil losses |
| Ggod km-2 | 288.96777561491 | m3 km-2 god-1 | Real soil losses per km2 |