May Ayni

The May Ayni is a river of the Nile basin. Rising in the mountains of Dogu’a Tembien in northern Ethiopia, it flows southwestward to empty finally in the Giba and Tekezé River.^[1]

The river in the radial drainage network of Dogu’a Tembien

May Ayni
May Ayni River in Dogu’a Tembien
Etymology	"Spring" in Tigrinya language
Location
Country	Ethiopia
Region	Tigray Region
District (woreda)	Dogu’a Tembien
Physical characteristics
Source
• location	Ra’isot in Ayninbirkekin municipality
• elevation	2,298 m (7,539 ft)
Mouth	Afedena River
• location	Near Afedena in Addi Azmera municipality
• coordinates	13.647°N 39.303°E / 13.647; 39.303
• elevation	1,995 m (6,545 ft)
Length	6 km (3.7 mi)
Width
• average	5 m (16 ft)
Basin features
Progression	Afedena→ Hurura→ Giba→ Tekezé→ Atbarah→ Nile→ Mediterranean Sea
River system	Seasonal river
Topography	Mountains and deep gorges

Characteristics

It is a confined ephemeral river, locally meandering in its narrow alluvial plain, with an average slope gradient of 51 metres per kilometre. With its tributaries, the river has cut a deep gorge.^[2]

Flash floods and flood buffering

Runoff mostly happens in the form of high runoff discharge events that occur in a very short period (called flash floods). These are related to the steep topography, often little vegetation cover and intense convective rainfall. The peaks of such flash floods often have a 50 to 100 times larger discharge than the preceding baseflow.^[2] The magnitude of floods in this river has, however, been decreased due to interventions in the catchment. On steep slopes, exclosures have been established; the dense vegetation largely contributes to enhanced infiltration, less flooding and better baseflow.^[3] Physical conservation structures such as stone bunds^[4][5] and check dams also intercept runoff.^[6][7]

Boulders and pebbles in the river bed

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.^[8]

• Amba Aradam Formation
• Mekelle Dolerite
• Antalo Limestone
• Quaternary freshwater tufa^[9]

See also

• List of Ethiopian rivers