Latitude: 42.985615 | Longitude: 19.754802 | Country: Montenegro | Year: 2018 |
| F | 3.90474 | km2 | Surface area of the drainage basin |
| Fm | 1.50083 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 2.40391 | km2 | Surface area of greater portion of the drainage basin |
| O | 10.66291 | km | The length of the watershed |
| Lv | 3.80992 | km | Natural length of the main watercourse |
| Lb | 4.23154 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.15032 ","0.73023 ","1.30891 ","4.32289 ","6.92308 ","6.65907 ","5.67712 ","3.12694 ","0.24539 "] | km | Contour line length |
| f | ["0.00514 ","0.0268 ","0.11623 ","0.36052 ","0.95916 ","1.00387 ","0.80403 ","0.4995 ","0.22348 ","0.07525 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 50 | m | Equidistance |
| Hmin | 592 | m | Lowest altitude in the drainage basin |
| Hmax | 1006 | m | Highest altitude in the draigane basin |
| ΣL | 8.13186 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.91368 | 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 | 0.1157 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.8843 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.676996973 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.261297321 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.061705706 | 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 | 983.7 | mm | Average annual quantity of precipitation |
| 11.39 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 0 % | Serpentines, red sand stones, flishe deposits |
| 19.69 % | Podzols and parapodzols, decomposed schist |
| 0 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 39.38 % | Brown forest soils and Mountain soils |
| 0 % | Epieugleysol and Marshlands |
| 0 % | Good structured Chernozems and alluvial well-structured deposits |
| 29.54 % | Bare, compact igneous |
| 0 % | Bare lands |
| 6.17 % | Plough-lands |
| 5.86 % | Orchards and vineyards |
| 3.9 % | Mountain pastures |
| 16.37 % | Meadows |
| 44 % | Degraded forests |
| 23.69 % | Well-constituted forests |
| 1 % | Depth erosion |
| 0.89 % | 80% of the river basin under rill and gully erosion |
| 0.78 % | 50% of the river basin under rill and gully erosion |
| 0.67 % | 100% of the river basin under surface erosion |
| 16.37 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.33 % | 50% of the river basin under surface erosion |
| 0.22 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 6.17 % | The river basin mostly under plough-land |
| 73.57 % | The river basin under forests and perennial vegetation |
| A | 0.54575094752646 | / | Coefficient of the river basin form |
| m | 0.54389474634674 | / | Coefficient of the watershed development |
| B | 0.92277043345921 | km | Average river basin width |
| a | 0.46255576555673 | / | (A)symmetry of the river basin |
| G | 2.0825611948555 | / | Density of the river network of the basin |
| K | 1.307597265314 | / | Coefficient of the river basin tortuousness |
| Hsr | 868.20631847447 | m | Average river basin altitude |
| Dsr | 276.20631847447 | m | Average elevation difference of the river basin |
| Isr | 37.318681909679 | % | Average river basin decline |
| Hleb | 414 | m | The height of the local erosion base of the river basin |
| Er | 93.745933511616 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.725283370609 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.96529 | / | Coefficient of the region's permeability |
| S2 | 0.6769417466 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 145.46629139839 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 89.500694691916 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.30893212066687 | / | Coefficient of the river basin erosion |
| Wgod | 2061.6591279934 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.24853840637952 | / | Coefficient of the deposit retention |
| Ggod | 512.40147416926 | m3 god-1 | Real soil losses |
| Ggod km-2 | 131.22550391813 | m3 km-2 god-1 | Real soil losses per km2 |