Latitude: 37.94 | Longitude: 57.35 | Country: Iran, Islamic Republic of | Year: 2019 |
| F | 35.46 | km2 | Surface area of the drainage basin |
| Fm | 16.96 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 18.5 | km2 | Surface area of greater portion of the drainage basin |
| O | 28.64 | km | The length of the watershed |
| Lv | 11.14 | km | Natural length of the main watercourse |
| Lb | 3.95 | km | Surface area of greater portion of the drainage basin |
| Liz | ["3.56 ","11.85 ","26.37 ","19.28 ","22.56 ","23.11 "] | km | Contour line length |
| f | ["0.81 ","6.35 ","7.47 ","6.06 ","5.91 ","8.79 ","0.07 "] | km2 | The area between the two neighboring contour lines |
| h0 | 1200 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 1156 | m | Lowest altitude in the drainage basin |
| Hmax | 1767 | m | Highest altitude in the draigane basin |
| ΣL | 72.53 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 10.16 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.12 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.58 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.3 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.31820 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.65340 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.02840 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 34.52 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 11 | °C | Average annual air temperature |
| Hgod | 315.2 | mm | Average annual quantity of precipitation |
| 0 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 38.5 % | Decomposed limestone and marls |
| 41.63 % | 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 |
| 19.87 % | Epieugleysol and Marshlands |
| 0 % | Good structured Chernozems and alluvial well-structured deposits |
| 0 % | Bare, compact igneous |
| 0 % | Bare lands |
| 2.84 % | Plough-lands |
| 1.32 % | Orchards and vineyards |
| 64.02 % | Mountain pastures |
| 0 % | Meadows |
| 31.82 % | Degraded forests |
| 0 % | Well-constituted forests |
| 0 % | Depth erosion |
| 13.29 % | 80% of the river basin under rill and gully erosion |
| 36.62 % | 50% of the river basin under rill and gully erosion |
| 0 % | 100% of the river basin under surface erosion |
| 0 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0 % | 50% of the river basin under surface erosion |
| 50.09 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 0 % | The river basin mostly under plough-land |
| 0 % | The river basin under forests and perennial vegetation |
| A | 0.50132854578097 | / | Coefficient of the river basin form |
| m | 0.52772891836289 | / | Coefficient of the watershed development |
| B | 8.9772151898734 | km | Average river basin width |
| a | 0.086858432036097 | / | (A)symmetry of the river basin |
| G | 2.0454032712916 | / | Density of the river network of the basin |
| K | 1.0964566929134 | / | Coefficient of the river basin tortuousness |
| Hsr | 1453.709108855 | m | Average river basin altitude |
| Dsr | 297.709108855 | m | Average elevation difference of the river basin |
| Isr | 30.098702763677 | % | Average river basin decline |
| Hleb | 611 | m | The height of the local erosion base of the river basin |
| Er | 79.699694141038 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 0.45701928433154 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.754 | / | Coefficient of the region's permeability |
| S2 | 0.74204 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 455.10848080427 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 58.340554315277 | m3 s-1 | Maximal outflow from the river basin |
| T | 1.0954451150103 | / | Temperature coefficient of the region |
| Z | 0.70435094003744 | / | Coefficient of the river basin erosion |
| Wgod | 22737.833585677 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.27625336759509 | / | Coefficient of the deposit retention |
| Ggod | 6281.4030998599 | m3 god-1 | Real soil losses |
| Ggod km-2 | 177.14052735081 | m3 km-2 god-1 | Real soil losses per km2 |