Latitude: 43.138682 | Longitude: 19.773887 | Country: Montenegro | Year: 2018 |
| F | 41.05907 | km2 | Surface area of the drainage basin |
| Fm | 14.85692 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 26.20215 | km2 | Surface area of greater portion of the drainage basin |
| O | 30.70126 | km | The length of the watershed |
| Lv | 6.32589 | km | Natural length of the main watercourse |
| Lb | 11.11752 | km | Surface area of greater portion of the drainage basin |
| Liz | ["12.70622 ","22.47492 ","24.16420 ","19.89668 ","16.55711 ","13.36863 ","12.14923 ","6.36042 ","2.24839 ","0.45849 "] | km | Contour line length |
| f | ["2.51322 ","5.22359 ","6.67593 ","6.59297 ","5.89601 ","4.61562 ","3.98547 ","3.40481 ","1.57289 ","0.54508 ","0.03348 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 535 | m | Lowest altitude in the drainage basin |
| Hmax | 1553 | m | Highest altitude in the draigane basin |
| ΣL | 13.88313 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 6.02786 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.1234 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0373 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.8393 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.494418976 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.373520123 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.132060901 | 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 |
| 1.19 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 94.34 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 4.46 % | 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 |
| 13.21 % | Plough-lands |
| 1 % | Orchards and vineyards |
| 20.82 % | Mountain pastures |
| 15.53 % | Meadows |
| 32.14 % | Degraded forests |
| 17.3 % | Well-constituted forests |
| 5.35 % | Depth erosion |
| 4.76 % | 80% of the river basin under rill and gully erosion |
| 4.16 % | 50% of the river basin under rill and gully erosion |
| 3.57 % | 100% of the river basin under surface erosion |
| 15.53 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.78 % | 50% of the river basin under surface erosion |
| 1.19 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 13.21 % | The river basin mostly under plough-land |
| 50.44 % | The river basin under forests and perennial vegetation |
| A | 0.94638789166426 | / | Coefficient of the river basin form |
| m | 0.27849163162698 | / | Coefficient of the watershed development |
| B | 3.6931860702747 | km | Average river basin width |
| a | 0.55262966258125 | / | (A)symmetry of the river basin |
| G | 0.33812577829941 | / | Density of the river network of the basin |
| K | 1.0494420905595 | / | Coefficient of the river basin tortuousness |
| Hsr | 917.80807675381 | m | Average river basin altitude |
| Dsr | 382.80807675381 | m | Average elevation difference of the river basin |
| Isr | 31.75529548039 | % | Average river basin decline |
| Hleb | 1018 | m | The height of the local erosion base of the river basin |
| Er | 128.01051012147 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.6986538294287 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.91477 | / | Coefficient of the region's permeability |
| S2 | 0.727528385 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 555.32164537716 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 594.12867708269 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.50667215808297 | / | Coefficient of the river basin erosion |
| Wgod | 40441.706617163 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.41997339165313 | / | Coefficient of the deposit retention |
| Ggod | 16984.440692251 | m3 god-1 | Real soil losses |
| Ggod km-2 | 413.65867985443 | m3 km-2 god-1 | Real soil losses per km2 |