Latitude: 42.713853 | Longitude: 19.841359 | Country: Montenegro | Year: 2018 |
| F | 13.1774 | km2 | Surface area of the drainage basin |
| Fm | 5.03959 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 8.13781 | km2 | Surface area of greater portion of the drainage basin |
| O | 17.67563 | km | The length of the watershed |
| Lv | 4.29066 | km | Natural length of the main watercourse |
| Lb | 7.73623 | km | Surface area of greater portion of the drainage basin |
| Liz | ["2.74605 ","4.20528 ","5.27618 ","5.71525 ","6.62818 ","7.15637 ","7.99406 ","8.38899 ","5.47760 ","3.73894 ","2.56524 ","1.73568 "] | km | Contour line length |
| f | ["0.34733 ","0.85915 ","0.85252 ","1.06944 ","1.28883 ","1.26091 ","1.48741 ","1.50505 ","1.80966 ","1.01645 ","0.81578 ","0.45640 ","0.40846 "] | km2 | The area between the two neighboring contour lines |
| h0 | 800 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 775 | m | Lowest altitude in the drainage basin |
| Hmax | 1988 | m | Highest altitude in the draigane basin |
| ΣL | 4.29066 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 3.86715 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.1694 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0949 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.7357 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.554404007 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.419556599 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.026039393 | 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 | 1183.7 | mm | Average annual quantity of precipitation |
| 7.82 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 79.28 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 12.9 % | 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 |
| 2.6 % | Plough-lands |
| 1.69 % | Orchards and vineyards |
| 25.37 % | Mountain pastures |
| 14.9 % | Meadows |
| 12.18 % | Degraded forests |
| 43.26 % | Well-constituted forests |
| 6.52 % | Depth erosion |
| 5.8 % | 80% of the river basin under rill and gully erosion |
| 5.07 % | 50% of the river basin under rill and gully erosion |
| 4.35 % | 100% of the river basin under surface erosion |
| 14.9 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 2.17 % | 50% of the river basin under surface erosion |
| 1.45 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 2.6 % | The river basin mostly under plough-land |
| 57.13 % | The river basin under forests and perennial vegetation |
| A | 0.80331414048188 | / | Coefficient of the river basin form |
| m | 0.33342971790941 | / | Coefficient of the watershed development |
| B | 1.7033361210822 | km | Average river basin width |
| a | 0.47023236753836 | / | (A)symmetry of the river basin |
| G | 0.32560747947243 | / | Density of the river network of the basin |
| K | 1.109514758931 | / | Coefficient of the river basin tortuousness |
| Hsr | 1345.7389633008 | m | Average river basin altitude |
| Dsr | 570.7389633008 | m | Average elevation difference of the river basin |
| Isr | 46.767814591649 | % | Average river basin decline |
| Hleb | 1213 | m | The height of the local erosion base of the river basin |
| Er | 202.65321400665 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.3625870161202 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.86989 | / | Coefficient of the region's permeability |
| S2 | 0.6943270764 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 384.13433479227 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 253.95760641893 | m3 s-1 | Maximal outflow from the river basin |
| T | 1 | / | Temperature coefficient of the region |
| Z | 0.40600096959969 | / | Coefficient of the river basin erosion |
| Wgod | 12676.864712869 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.44451244148543 | / | Coefficient of the deposit retention |
| Ggod | 5635.0240838979 | m3 god-1 | Real soil losses |
| Ggod km-2 | 427.62791475541 | m3 km-2 god-1 | Real soil losses per km2 |