Latitude: 42.965474 | Longitude: 19.803427 | Country: Montenegro | Year: 2018 |
| F | 58.97254 | km2 | Surface area of the drainage basin |
| Fm | 25.51797 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 33.45457 | km2 | Surface area of greater portion of the drainage basin |
| O | 37.66755 | km | The length of the watershed |
| Lv | 9.41475 | km | Natural length of the main watercourse |
| Lb | 16.0797 | km | Surface area of greater portion of the drainage basin |
| Liz | ["1.40702 ","16.45055 ","21.79096 ","22.40950 ","26.94811 ","28.15199 ","23.96819 ","15.93641 ","11.26803 ","6.98885 ","5.34400 ","4.48934 ","3.41206 ","1.31015 ","0.21999 "] | km | Contour line length |
| f | ["0.33128 ","5.37975 ","6.12391 ","6.57640 ","6.53720 ","7.93210 ","8.39302 ","6.34801 ","4.06150 ","2.32883 ","1.54674 ","1.47398 ","1.11295 ","0.58720 ","0.23234 ","0.00731 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 595 | m | Lowest altitude in the drainage basin |
| Hmax | 2005 | m | Highest altitude in the draigane basin |
| ΣL | 23.8826 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 8.76356 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.2614 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0426 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.696 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.552755275527553 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.422842284228423 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.0244024402440244 | 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 |
| 3.96 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 88.03 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 3.62 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 4.4 % | 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 |
| 2.44 % | Plough-lands |
| 0.24 % | Orchards and vineyards |
| 30.17 % | Mountain pastures |
| 11.87 % | Meadows |
| 33.16 % | Degraded forests |
| 22.11 % | Well-constituted forests |
| 7.76 % | Depth erosion |
| 6.9 % | 80% of the river basin under rill and gully erosion |
| 6.03 % | 50% of the river basin under rill and gully erosion |
| 5.17 % | 100% of the river basin under surface erosion |
| 11.87 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 2.59 % | 50% of the river basin under surface erosion |
| 1.72 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 2.44 % | The river basin mostly under plough-land |
| 55.51 % | The river basin under forests and perennial vegetation |
| A | 0.78017708914204 | / | Coefficient of the river basin form |
| m | 0.3458429630334 | / | Coefficient of the watershed development |
| B | 3.6675149411992 | km | Average river basin width |
| a | 0.26916256277922 | / | (A)symmetry of the river basin |
| G | 0.40497831702687 | / | Density of the river network of the basin |
| K | 1.0743065603476 | / | Coefficient of the river basin tortuousness |
| Hsr | 1071.5954675685 | m | Average river basin altitude |
| Dsr | 476.5954675685 | m | Average elevation difference of the river basin |
| Isr | 32.234519659489 | % | Average river basin decline |
| Hleb | 1410 | m | The height of the local erosion base of the river basin |
| Er | 161.95963209215 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.6724978593604 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.83038 | / | Coefficient of the region's permeability |
| S2 | 0.69432943294329 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 742.59047145485 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 558.66387773268 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.48471752753156 | / | Coefficient of the river basin erosion |
| Wgod | 61194.594504557 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.43647244733383 | / | Coefficient of the deposit retention |
| Ggod | 26709.754427005 | m3 god-1 | Real soil losses |
| Ggod km-2 | 452.91850117029 | m3 km-2 god-1 | Real soil losses per km2 |