Latitude: 42.999431 | Longitude: 19.747604 | Country: Montenegro | Year: 2018 |
| F | 12.9164 | km2 | Surface area of the drainage basin |
| Fm | 4.01929 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 8.89711 | km2 | Surface area of greater portion of the drainage basin |
| O | 16.30059 | km | The length of the watershed |
| Lv | 3.82415 | km | Natural length of the main watercourse |
| Lb | 6.60463 | km | Surface area of greater portion of the drainage basin |
| Liz | ["4.61578 ","8.13069 ","9.28506 ","7.10253 ","6.31298 ","4.30832 ","1.23246 "] | km | Contour line length |
| f | ["1.33140 ","1.68526 ","2.49675 ","2.67643 ","2.18208 ","1.74259 ","0.69747 ","0.10442 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 578 | m | Lowest altitude in the drainage basin |
| Hmax | 1264 | m | Highest altitude in the draigane basin |
| ΣL | 3.82415 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 3.45558 | 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 | 0.1342 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.8658 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.572645755 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.372279326 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.055074919 | 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 | 893.3 | mm | Average annual quantity of precipitation |
| 8 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 92 % | 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 |
| 5.51 % | Plough-lands |
| 8.67 % | Orchards and vineyards |
| 9.24 % | Mountain pastures |
| 19.32 % | Meadows |
| 37.22 % | Degraded forests |
| 20.04 % | Well-constituted forests |
| 2.38 % | Depth erosion |
| 2.11 % | 80% of the river basin under rill and gully erosion |
| 1.85 % | 50% of the river basin under rill and gully erosion |
| 1.58 % | 100% of the river basin under surface erosion |
| 19.32 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.79 % | 50% of the river basin under surface erosion |
| 0.53 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 5.51 % | The river basin mostly under plough-land |
| 65.93 % | The river basin under forests and perennial vegetation |
| A | 0.83119518062837 | / | Coefficient of the river basin form |
| m | 0.30016444214948 | / | Coefficient of the watershed development |
| B | 1.9556583790462 | km | Average river basin width |
| a | 0.75529094794215 | / | (A)symmetry of the river basin |
| G | 0.29606933820569 | / | Density of the river network of the basin |
| K | 1.1066593741138 | / | Coefficient of the river basin tortuousness |
| Hsr | 840.83591712861 | m | Average river basin altitude |
| Dsr | 262.83591712861 | m | Average elevation difference of the river basin |
| Isr | 31.733160942678 | % | Average river basin decline |
| Hleb | 686 | m | The height of the local erosion base of the river basin |
| Er | 115.18312883334 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.7251111879185 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.95974 | / | Coefficient of the region's permeability |
| S2 | 0.6964858328 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 258.08490296955 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 247.37088988456 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.46203968971942 | / | Coefficient of the river basin erosion |
| Wgod | 11327.269025408 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.29945776319159 | / | Coefficient of the deposit retention |
| Ggod | 3392.0386454182 | m3 god-1 | Real soil losses |
| Ggod km-2 | 262.6148652425 | m3 km-2 god-1 | Real soil losses per km2 |