Latitude: 42.801003 | Longitude: 19.84483 | Country: Montenegro | Year: 2018 |
| F | 17.6299 | km2 | Surface area of the drainage basin |
| Fm | 7.71132 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 9.91858 | km2 | Surface area of greater portion of the drainage basin |
| O | 21.51861 | km | The length of the watershed |
| Lv | 7.31913 | km | Natural length of the main watercourse |
| Lb | 8.29074 | km | Surface area of greater portion of the drainage basin |
| Liz | ["1.39164 ","7.37748 ","7.37178 ","7.98934 ","4.29275 ","3.63637 ","3.65955 ","3.93973 ","5.37646 ","7.42631 ","7.76852 ","4.28908 "] | km | Contour line length |
| f | ["0.44559 ","2.95570 ","2.12800 ","1.89432 ","1.32803 ","0.62144 ","0.55537 ","0.62253 ","0.76737 ","1.49231 ","2.02380 ","2.20315 ","0.59230 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 692 | m | Lowest altitude in the drainage basin |
| Hmax | 1838 | m | Highest altitude in the draigane basin |
| ΣL | 7.31913 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 6.92495 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.2258 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.2585 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.5157 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.474821939 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.484920589 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.040257472 | 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 | 944.3 | mm | Average annual quantity of precipitation |
| 12.22 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 73.57 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 1.41 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 12.8 % | 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 |
| 4.03 % | Plough-lands |
| 5.9 % | Orchards and vineyards |
| 27.19 % | Mountain pastures |
| 15.4 % | Meadows |
| 28.49 % | Degraded forests |
| 18.99 % | Well-constituted forests |
| 6.99 % | Depth erosion |
| 6.22 % | 80% of the river basin under rill and gully erosion |
| 5.44 % | 50% of the river basin under rill and gully erosion |
| 4.66 % | 100% of the river basin under surface erosion |
| 15.4 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 2.33 % | 50% of the river basin under surface erosion |
| 1.55 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 4.03 % | The river basin mostly under plough-land |
| 53.38 % | The river basin under forests and perennial vegetation |
| A | 0.57330979911547 | / | Coefficient of the river basin form |
| m | 0.49173328302508 | / | Coefficient of the watershed development |
| B | 2.1264567457187 | km | Average river basin width |
| a | 0.25039960521614 | / | (A)symmetry of the river basin |
| G | 0.4151543684309 | / | Density of the river network of the basin |
| K | 1.0569217106261 | / | Coefficient of the river basin tortuousness |
| Hsr | 1218.212714763 | m | Average river basin altitude |
| Dsr | 526.212714763 | m | Average elevation difference of the river basin |
| Isr | 36.596356190336 | % | Average river basin decline |
| Hleb | 1146 | m | The height of the local erosion base of the river basin |
| Er | 178.02142894264 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.340714077213 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.78697 | / | Coefficient of the region's permeability |
| S2 | 0.7130871066 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 426.63363830669 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 184.02693378103 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.55016088165538 | / | Coefficient of the river basin erosion |
| Wgod | 21342.4499804 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.38859007104188 | / | Coefficient of the deposit retention |
| Ggod | 8293.4641540913 | m3 god-1 | Real soil losses |
| Ggod km-2 | 470.4203741423 | m3 km-2 god-1 | Real soil losses per km2 |