Latitude: 42.987693 | Longitude: 19.773726 | Country: Montenegro | Year: 2018 |
| F | 4.65292 | km2 | Surface area of the drainage basin |
| Fm | 1.89696 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 2.75596 | km2 | Surface area of greater portion of the drainage basin |
| O | 11.07977 | km | The length of the watershed |
| Lv | 4.76456 | km | Natural length of the main watercourse |
| Lb | 3.96822 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.79468 ","1.50078 ","3.04743 ","4.27864 ","4.16313 ","2.95749 ","1.17954 ","0.28877 "] | km | Contour line length |
| f | ["0.24581 ","0.22639 ","0.46940 ","0.88665 ","1.03811 ","0.98855 ","0.55123 ","0.22046 ","0.02633 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 670 | m | Lowest altitude in the drainage basin |
| Hmax | 1474 | m | Highest altitude in the draigane basin |
| ΣL | 4.76456 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 4.19401 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.2051 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.1695 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.6254 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.508302294 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.415338468 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.076359238 | 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 |
| 0 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 98.9 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 1.1 % | 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 |
| 7.64 % | Plough-lands |
| 0.98 % | Orchards and vineyards |
| 11.29 % | Mountain pastures |
| 29.26 % | Meadows |
| 30.5 % | Degraded forests |
| 20.33 % | Well-constituted forests |
| 2.9 % | Depth erosion |
| 2.58 % | 80% of the river basin under rill and gully erosion |
| 2.26 % | 50% of the river basin under rill and gully erosion |
| 1.94 % | 100% of the river basin under surface erosion |
| 29.26 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0.97 % | 50% of the river basin under surface erosion |
| 0.65 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 7.64 % | The river basin mostly under plough-land |
| 51.81 % | The river basin under forests and perennial vegetation |
| A | 0.45346373012408 | / | Coefficient of the river basin form |
| m | 0.62309616112878 | / | Coefficient of the watershed development |
| B | 1.1725458769927 | km | Average river basin width |
| a | 0.36923050471532 | / | (A)symmetry of the river basin |
| G | 1.0239935352424 | / | Density of the river network of the basin |
| K | 1.1360392559865 | / | Coefficient of the river basin tortuousness |
| Hsr | 1038.2346053661 | m | Average river basin altitude |
| Dsr | 368.2346053661 | m | Average elevation difference of the river basin |
| Isr | 39.137702775891 | % | Average river basin decline |
| Hleb | 804 | m | The height of the local erosion base of the river basin |
| Er | 174.2507996024 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3587438412877 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.82609 | / | Coefficient of the region's permeability |
| S2 | 0.7136113888 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 183.34733174824 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 66.595345477816 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.47557252773271 | / | Coefficient of the river basin erosion |
| Wgod | 4527.0009568078 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.273613271579 | / | Coefficient of the deposit retention |
| Ggod | 1238.6475422334 | m3 god-1 | Real soil losses |
| Ggod km-2 | 266.20864795299 | m3 km-2 god-1 | Real soil losses per km2 |