Latitude: 43.133479 | Longitude: 19.779412 | Country: Montenegro | Year: 2018 |
| F | 208.3548 | km2 | Surface area of the drainage basin |
| Fm | 60.80527 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 147.54953 | km2 | Surface area of greater portion of the drainage basin |
| O | 77.39176 | km | The length of the watershed |
| Lv | 20.19917 | km | Natural length of the main watercourse |
| Lb | 30.99341 | km | Surface area of greater portion of the drainage basin |
| Liz | ["26.51452 ","41.17613 ","41.07684 ","45.57509 ","56.40767 ","88.75072 ","118.59031 ","39.30942 ","30.28807 ","23.72393 "] | km | Contour line length |
| f | ["6.23615 ","11.18257 ","13.47651 ","11.78466 ","12.85439 ","21.73429 ","58.83183 ","39.38577 ","13.62419 ","13.51338 ","5.57253 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 535 | m | Lowest altitude in the drainage basin |
| Hmax | 1503 | m | Highest altitude in the draigane basin |
| ΣL | 45.63539 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 9.85582 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.4971 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.3062 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.1967 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.596205635 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.355037885 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.048756480 | 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 | 873.7 | mm | Average annual quantity of precipitation |
| 2.41 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 52.74 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 44.85 % | 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 |
| 4.88 % | Plough-lands |
| 2.27 % | Orchards and vineyards |
| 10.46 % | Mountain pastures |
| 22.78 % | Meadows |
| 38.75 % | Degraded forests |
| 20.87 % | Well-constituted forests |
| 2.69 % | Depth erosion |
| 2.39 % | 80% of the river basin under rill and gully erosion |
| 2.09 % | 50% of the river basin under rill and gully erosion |
| 1.79 % | 100% of the river basin under surface erosion |
| 22.78 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.9 % | 50% of the river basin under surface erosion |
| 0.6 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 4.88 % | The river basin mostly under plough-land |
| 61.89 % | The river basin under forests and perennial vegetation |
| A | 0.74712937214747 | / | Coefficient of the river basin form |
| m | 0.39475427079801 | / | Coefficient of the watershed development |
| B | 6.7225516650152 | km | Average river basin width |
| a | 0.83265909880646 | / | (A)symmetry of the river basin |
| G | 0.21902730342665 | / | Density of the river network of the basin |
| K | 2.0494662037253 | / | Coefficient of the river basin tortuousness |
| Hsr | 1100.0837629851 | m | Average river basin altitude |
| Dsr | 565.0837629851 | m | Average elevation difference of the river basin |
| Isr | 24.545280454302 | % | Average river basin decline |
| Hleb | 968 | m | The height of the local erosion base of the river basin |
| Er | 81.100700817794 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.6050764747116 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.60988 | / | Coefficient of the region's permeability |
| S2 | 0.690510169 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 1519.8742977367 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 767.56238013145 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.37005031851576 | / | Coefficient of the river basin erosion |
| Wgod | 128092.73222197 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.4379643540408 | / | Coefficient of the deposit retention |
| Ggod | 56100.050724915 | m3 god-1 | Real soil losses |
| Ggod km-2 | 269.25249970202 | m3 km-2 god-1 | Real soil losses per km2 |