Latitude: 42.662417 | Longitude: 19.885632 | Country: Montenegro | Year: 2018 |
| F | 23.81316 | km2 | Surface area of the drainage basin |
| Fm | 11.75132 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 12.06184 | km2 | Surface area of greater portion of the drainage basin |
| O | 20.12763 | km | The length of the watershed |
| Lv | 6.21857 | km | Natural length of the main watercourse |
| Lb | 7.29624 | km | Surface area of greater portion of the drainage basin |
| Liz | ["3.66252 ","6.85066 ","7.65354 ","9.41269 ","9.90799 ","9.82903 ","12.1316 ","14.00802 ","15.05212 ","14.57022 ","12.36504 ","7.36179 ","2.99289 ","0.00001 "] | km | Contour line length |
| f | ["0.45239 ","1.1597 ","1.31044 ","1.72803 ","1.58075 ","1.49243 ","1.63147 ","2.16386 ","2.58594 ","3.24771 ","2.91651 ","2.20469 ","0.9558 ","0.39092 ","0.00001 "] | km2 | The area between the two neighboring contour lines |
| h0 | 900 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 830 | m | Lowest altitude in the drainage basin |
| Hmax | 2211 | m | Highest altitude in the draigane basin |
| ΣL | 8.68633 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 5.92688 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.2947 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0405 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.6648 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.680741123 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.298309852 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.020949025 | 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 | 1183.7 | mm | Average annual quantity of precipitation |
| 2.19 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 65.57 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 32.24 % | 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 |
| 2.09 % | Plough-lands |
| 2.38 % | Orchards and vineyards |
| 17.81 % | Mountain pastures |
| 9.64 % | Meadows |
| 17.23 % | Degraded forests |
| 50.85 % | Well-constituted forests |
| 4.58 % | Depth erosion |
| 4.07 % | 80% of the river basin under rill and gully erosion |
| 3.56 % | 50% of the river basin under rill and gully erosion |
| 3.05 % | 100% of the river basin under surface erosion |
| 9.64 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.53 % | 50% of the river basin under surface erosion |
| 1.02 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 2.09 % | The river basin mostly under plough-land |
| 70.45 % | The river basin under forests and perennial vegetation |
| A | 0.63115601335998 | / | Coefficient of the river basin form |
| m | 0.35948194298402 | / | Coefficient of the watershed development |
| B | 3.2637577711259 | km | Average river basin width |
| a | 0.026079697108658 | / | (A)symmetry of the river basin |
| G | 0.36477015230234 | / | Density of the river network of the basin |
| K | 1.049214763923 | / | Coefficient of the river basin tortuousness |
| Hsr | 1554.2428600404 | m | Average river basin altitude |
| Dsr | 724.2428600404 | m | Average elevation difference of the river basin |
| Isr | 52.827142638776 | % | Average river basin decline |
| Hleb | 1381 | m | The height of the local erosion base of the river basin |
| Er | 198.99380136113 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3480171403329 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.81103 | / | Coefficient of the region's permeability |
| S2 | 0.6680415804 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 581.70142502842 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 268.14683809524 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.32719744107024 | / | Coefficient of the river basin erosion |
| Wgod | 16573.84977357 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.47082104556721 | / | Coefficient of the deposit retention |
| Ggod | 7803.317279466 | m3 god-1 | Real soil losses |
| Ggod km-2 | 327.68928103057 | m3 km-2 god-1 | Real soil losses per km2 |