Latitude: 42.968747 | Longitude: 19.836161 | Country: Montenegro | Year: 2018 |
| F | 29.5919 | km2 | Surface area of the drainage basin |
| Fm | 9.73523 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 19.85667 | km2 | Surface area of greater portion of the drainage basin |
| O | 27.49582 | km | The length of the watershed |
| Lv | 11.33772 | km | Natural length of the main watercourse |
| Lb | 12.40093 | km | Surface area of greater portion of the drainage basin |
| Liz | ["10.42299 ","17.33215 ","19.26944 ","16.25709 ","11.98655 ","9.71556 ","5.71036 ","0.74851 "] | km | Contour line length |
| f | ["2.98664 ","4.35729 ","5.20436 ","5.85422 ","3.92314 ","3.46386 ","2.40854 ","1.35322 ","0.04063 "] | km2 | The area between the two neighboring contour lines |
| h0 | 700 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 622 | m | Lowest altitude in the drainage basin |
| Hmax | 1476 | m | Highest altitude in the draigane basin |
| ΣL | 11.33772 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 10.43256 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.2021 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.0383 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.7596 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.532023983 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.314555218 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.153420799 | 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 | 983.7 | mm | Average annual quantity of precipitation |
| 3.71 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 82.79 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 13.49 % | 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 |
| 15.34 % | Plough-lands |
| 1.94 % | Orchards and vineyards |
| 17.99 % | Mountain pastures |
| 11.52 % | Meadows |
| 31.92 % | Degraded forests |
| 21.28 % | Well-constituted forests |
| 4.63 % | Depth erosion |
| 4.11 % | 80% of the river basin under rill and gully erosion |
| 3.6 % | 50% of the river basin under rill and gully erosion |
| 3.08 % | 100% of the river basin under surface erosion |
| 11.52 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 1.54 % | 50% of the river basin under surface erosion |
| 1.03 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 15.34 % | The river basin mostly under plough-land |
| 55.15 % | The river basin under forests and perennial vegetation |
| A | 0.47290680136747 | / | Coefficient of the river basin form |
| m | 0.58794184371746 | / | Coefficient of the watershed development |
| B | 2.3862645785437 | km | Average river basin width |
| a | 0.68406827544024 | / | (A)symmetry of the river basin |
| G | 0.3831359257094 | / | Density of the river network of the basin |
| K | 1.0867629805148 | / | Coefficient of the river basin tortuousness |
| Hsr | 953.84329765916 | m | Average river basin altitude |
| Dsr | 331.84329765916 | m | Average elevation difference of the river basin |
| Isr | 30.901243245618 | % | Average river basin decline |
| Hleb | 854 | m | The height of the local erosion base of the river basin |
| Er | 116.55067292076 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.6583702814239 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.86725 | / | Coefficient of the region's permeability |
| S2 | 0.7242793632 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 438.93726385624 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 216.22700768523 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.99498743710662 | / | Temperature coefficient of the region |
| Z | 0.47618773455425 | / | Coefficient of the river basin erosion |
| Wgod | 29899.938795429 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.28312736497123 | / | Coefficient of the deposit retention |
| Ggod | 8465.4908839509 | m3 god-1 | Real soil losses |
| Ggod km-2 | 286.07459757403 | m3 km-2 god-1 | Real soil losses per km2 |