It is a confined river, locally meandering in its narrow alluvial plain, with a slope gradient of 25 metres per kilometre. With its tributaries, the river has cut a deep gorge.
The runoff footprint or annual total runoff volume is 41 million m³ at the bridge in Abiy Addi and 79 million m³ at the confluence with Giba River at Barashuwa. Peak discharges up to 543 m³ per second occur in the second part of the rainy season when there are strong rains and the soils are saturated with water in many places. The percentage of total rainfall that directly leaves the catchment as storm runoff is 23%. This is high, in comparison to other rivers of the Giba River basin, and has been explained by the fact that the larger part of the Tanqwa basin is composed of impervious rocks, particularly Ashangi Basalts, Alaji Basalts and Precambrian basement rocks. The total amount of sediment that is transported by this river amounts to 596,000 tonnes per year. Median sediment concentration in the river water is 3.95 grammes per litre, but may go up to 68 g/L. The highest sediment concentrations occur at the beginning of the rainy season, when loose soil and dust is washed away by overland flow and ends up in the river. As such water contains many nutrients, farmers estimate that it strengthens their cattle, which they will bring to the river. All in all, average sediment yield is 3627 tonnes per km² and per year. All measurements were done at purposively installed stations, in the years 2006-2007.
Flash floods
Runoff mostly occurs in the form of high runoff discharge events that occur in a very short period. These are related to the steep topography, often little vegetation cover and intense convective rainfall. The peaks of such flash floods have often a 50 to 100 times larger discharge than the preceding baseflow. These flash floods mostly occur during the evening or night, because the convective rain showers occur in the afternoon.
Changes over time
Evidence given by Italian aerial photographs of the catchment, taken in the 1930s show that 63% of the catchment was covered with woody vegetation. This vegetation could slow down runoff and the runoff coefficient was smaller. As a consequence, discharges in the river were less and the river was narrower than today. Up to the 1980s, there was strong pressure on the environment, and much vegetation disappeared. This river had its greatest discharges and width in that period. The magnitude of floods in this river has however been decreased in recent years due to interventions in the catchment. On other steep slopes, exclosures have been established; the dense vegetation largely contributes to enhanced infiltration, less flooding and better baseflow. Physical conservation structures such as stone bunds and check dams also intercept runoff.
The valley bottoms in the gorges of this river have been identified as a transhumance destination zone. Transhumance takes place in the summer rainy season, when the lands near the villages are occupied by crops. Young shepherds will take the village cattle down to the gorge and overnight in small caves. The gorges are particularly attractive as a transhumance destination zone, because there is water and good growth of semi-natural vegetation.
Boulders and pebbles encountered in the river bed can originate from any location higher up in the catchment. In the uppermost stretches of the river, only rock fragments of the upper lithological units will be present in the river bed, whereas more downstream one may find a more comprehensive mix of all lithologies crossed by the river. From upstream to downstream, the following lithological units occur in the catchment.
Trekking routes have been established across and along this river. The tracks are not marked on the ground but can be followed using downloaded.GPX files.
In the rainy season, flash floods may occur and it is advised not to follow the river bed. Frequently, it is then also impossible to wade across the river.
