Tat Ali is a low Holocene shield volcano located in the northern part of the Afar Region of Ethiopia. This elevation is characterized as having an elongated summit depression that has produced a variety of rock types, ranging from basalts to pantellerites.
The Tat Ali volcano is a low-lying shield volcano located in the northern Afar Region of Ethiopia. Its distinctive elongated summit depression has resulted in the formation of a range of rocks, including basalts and pantellerites.