Latitude: 42.929765 | Longitude: 19.849683 | Country: Montenegro | Year: 2018 |
| F | 2.37591 | km2 | Surface area of the drainage basin |
| Fm | 0.61772 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 1.75819 | km2 | Surface area of greater portion of the drainage basin |
| O | 7.62522 | km | The length of the watershed |
| Lv | 2.22005 | km | Natural length of the main watercourse |
| Lb | 2.99791 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.21619 ","0.41679 ","0.80423 ","1.98632 ","3.82004 ","0.97984 "] | km | Contour line length |
| f | ["0.02119 ","0.02951 ","0.08112 ","0.59 ","0.60163 ","0.85699 ","0.19547 "] | km2 | The area between the two neighboring contour lines |
| h0 | 600 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 545 | m | Lowest altitude in the drainage basin |
| Hmax | 1123 | m | Highest altitude in the draigane basin |
| ΣL | 4.58 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 1.81702 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.715 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1217 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.1633 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.598511530 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.308099654 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.093388816 | 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 |
| 15.09 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 84.91 % | 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 |
| 9.34 % | Plough-lands |
| 1.37 % | Orchards and vineyards |
| 10.63 % | Mountain pastures |
| 18.81 % | Meadows |
| 35.91 % | Degraded forests |
| 23.94 % | Well-constituted forests |
| 2.73 % | Depth erosion |
| 2.43 % | 80% of the river basin under rill and gully erosion |
| 2.13 % | 50% of the river basin under rill and gully erosion |
| 1.82 % | 100% of the river basin under surface erosion |
| 18.81 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.91 % | 50% of the river basin under surface erosion |
| 0.61 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 9.34 % | The river basin mostly under plough-land |
| 61.22 % | The river basin under forests and perennial vegetation |
| A | 0.66976775297854 | / | Coefficient of the river basin form |
| m | 0.40629626598175 | / | Coefficient of the watershed development |
| B | 0.79252212374621 | km | Average river basin width |
| a | 0.96002794718655 | / | (A)symmetry of the river basin |
| G | 1.9276824458839 | / | Density of the river network of the basin |
| K | 1.2218082354625 | / | Coefficient of the river basin tortuousness |
| Hsr | 960.60275010417 | m | Average river basin altitude |
| Dsr | 415.60275010417 | m | Average elevation difference of the river basin |
| Isr | 34.611622494118 | % | Average river basin decline |
| Hleb | 578 | m | The height of the local erosion base of the river basin |
| Er | 148.19053617049 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3826455788623 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.53449 | / | Coefficient of the region's permeability |
| S2 | 0.6989754572 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 139.188610894 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 48.154881096734 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.48998004464068 | / | Coefficient of the river basin erosion |
| Wgod | 2417.4496485715 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.29135495489714 | / | Coefficient of the deposit retention |
| Ggod | 704.33593332567 | m3 god-1 | Real soil losses |
| Ggod km-2 | 296.44891150156 | m3 km-2 god-1 | Real soil losses per km2 |