Latitude: 42.79676 | Longitude: 19.844666 | Country: Montenegro | Year: 2018 |
| F | 8.37511 | km2 | Surface area of the drainage basin |
| Fm | 3.36772 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 5.00739 | km2 | Surface area of greater portion of the drainage basin |
| O | 14.48935 | km | The length of the watershed |
| Lv | 4.68168 | km | Natural length of the main watercourse |
| Lb | 5.80048 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.89220 ","2.41157 ","3.55199 ","3.82108 ","4.29406 ","2.07612 "] | km | Contour line length |
| f | ["0.20124 ","0.77035 ","1.03434 ","1.42206 ","1.30556 ","2.06744 ","1.57411 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 698 | m | Lowest altitude in the drainage basin |
| Hmax | 1280 | m | Highest altitude in the draigane basin |
| ΣL | 5.34878 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 4.29355 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.5403 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.3185 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.1412 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.684040325 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.288509487 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.027450188 | 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 |
| 13.92 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 17.4 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 68.68 % | 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 |
| 2.75 % | Plough-lands |
| 2.05 % | Orchards and vineyards |
| 13.08 % | Mountain pastures |
| 13.72 % | Meadows |
| 11.04 % | Degraded forests |
| 57.36 % | Well-constituted forests |
| 3.36 % | Depth erosion |
| 2.99 % | 80% of the river basin under rill and gully erosion |
| 2.62 % | 50% of the river basin under rill and gully erosion |
| 2.24 % | 100% of the river basin under surface erosion |
| 13.72 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.12 % | 50% of the river basin under surface erosion |
| 0.75 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 2.75 % | The river basin mostly under plough-land |
| 70.45 % | The river basin under forests and perennial vegetation |
| A | 0.60350627338904 | / | Coefficient of the river basin form |
| m | 0.45635365557466 | / | Coefficient of the watershed development |
| B | 1.4438649904835 | km | Average river basin width |
| a | 0.39155784222536 | / | (A)symmetry of the river basin |
| G | 0.63865191024357 | / | Density of the river network of the basin |
| K | 1.0903983882801 | / | Coefficient of the river basin tortuousness |
| Hsr | 1032.6868136657 | m | Average river basin altitude |
| Dsr | 334.6868136657 | m | Average elevation difference of the river basin |
| Isr | 22.742411741458 | % | Average river basin decline |
| Hleb | 582 | m | The height of the local erosion base of the river basin |
| Er | 108.89939875984 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3594016937901 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.58027 | / | Coefficient of the region's permeability |
| S2 | 0.6686819726 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 234.5114556383 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 74.652334102262 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.21490374154398 | / | Coefficient of the river basin erosion |
| Wgod | 2475.2344871205 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.29998393264781 | / | Coefficient of the deposit retention |
| Ggod | 742.53057567188 | m3 god-1 | Real soil losses |
| Ggod km-2 | 88.659202765323 | m3 km-2 god-1 | Real soil losses per km2 |