Occurrence of Attributes in Original Text
The text related to the cultural heritage 'Lower Valley of the Awash' has mentioned 'River' in the following places:
| Occurrence Sentence | Text Source |
|---|---|
| Major river in Ethiopia | WIKI |
| Lower Valley of the AwashUNESCO World Heritage SiteAwash River in 2005LocationEthiopiaCriteriaCultural:xc2xa0(ii)(iii)(iv)Reference10Inscription1980 (4th session)Coordinates11xc2xb06xe2x80xb20.216xe2x80xb3N 40xc2xb034xe2x80xb245.804xe2x80xb3Exefxbbxbf / xefxbbxbf11.10006000xc2xb0N 40.57939000xc2xb0Exefxbbxbf / 11.10006000; 40.57939000Location of Awash River in Ethiopia | WIKI |
| The Awash (sometimes spelled Hawash; Oromiffa: Awaash, Amharic: xe1x8axa0xe1x8bx8bxe1x88xbd, Afar: We'ayot, Somali: Webiga Hawiye) is a major river of Ethiopia. | WIKI |
| According to Huntingford, in the 16th century the Awash river was called the great Dir river and lay in the country of the Muslims. | WIKI |
| It is then joined on its left bank by its chief affluent, the Germama (or Kasam) River, before turning northeast at approximately 11xc2xb0 N 40xc2xb0 30' E as far north as 12xc2xb0 before turning completely east to reach lake Gargori. | WIKI |
| The first European to trace the course of the Awash to its end in the Aussa oasis was Wilfred Thesiger in 1933/1934, who started at the city of Awash, followed the river's course to its final end in Lake Abhebad, and continued his expedition east to Tadjoura. | WIKI |
| Nesbitt had followed parts of the course of the Awash in 1928, he turned away from the river at Asaita and proceeded north through the Afar Depression to the Red Sea. | WIKI |
| [11] Recharge from river channel losses and via infiltration from lakes plays a role in the Main Ethiopian Rift (MER) and in southern Afar. | WIKI |