Oued es Segui

From Wikipedia, the free encyclopedia

Oued es Segui is a wadi in Tunisia and is nearby to , Henchir el Haramine and . Oued es Segui is also close to river and .[1]

The Wadi is located at 35.788333n and 9.928889e and flows near Kairouan.

The Segui Formation is a Miocene-Pliocene era geological structure first proposed by Burollet in 1956[2][better source needed] and it sits near the Oued es Segui in the tribal area of Tunisia.[3]

References[]

  1. ^ Oued es Segui at mapcarta.com.
  2. ^ Burollet (1956) In the Gafsa-Metlaoui Basin in Southwestern Tunisia
  3. ^ "Bled Segui".


Retrieved from ""