No. Ol Doinyo Lengai is associate with an area of rifting in Africa, which is a developing divergent plate boundary.
Ol Doinyo Lengai is on the continental crust of the African Plate.
it is on a convergent boundary if I remember right but I'll post another answer if I'm wrong
The myth of ol doinyo lengai is the myth of the Maasi People which clearly states: Ol Doinyo Lengai is translated in the language of Maa as the Mountain of God. Yes, God. Not Gods. The Maasians believe that when Ol doinyo lengai the God,God, is on the summit.
Ol Doinyo Lengai is a volcano in Tanzania notable for the fact that it erupts unique carbonatite lava.
No. Ol Doinyo Lengai is associate with an area of rifting in Africa, which is a developing divergent plate boundary.
Ol Doinyo Lengai is on the continental crust of the African Plate.
it is on a convergent boundary if I remember right but I'll post another answer if I'm wrong
The myth of ol doinyo lengai is the myth of the Maasi People which clearly states: Ol Doinyo Lengai is translated in the language of Maa as the Mountain of God. Yes, God. Not Gods. The Maasians believe that when Ol doinyo lengai the God,God, is on the summit.
Ol Doinyo Lengai is a volcano in Tanzania notable for the fact that it erupts unique carbonatite lava.
Ol Doinyo Lengai is not associated with a subduction zone. It is associated with the East African Rift, which is a continental rift.
* Ol Doinyo Lengai Volcano in Tanzania
Ol Doinyo Lengai is a unique volcano in that it erupts carbonatite lava, which cools to form carbonatite. It is unusual in that all other currently active volcanoes erupt silicate based material while this is carbonate based.
This type of lava can be found at Mt. Ol Doinyo Lengai, Northern Tanzania.
The tours up the mountain help the surrounding areas economony
Villarrica volcano is a Stratovolcano situated on the continental side of a subduction zone (a destructive plate boundary), it also sits on an ancient North West-West trending fracture in the crust called the sinistral Gastre Fault Zone.
The East Pacific Rise is representative of a divergent boundary where the Pacific Plate and the Nazca Plate (west of South America) are moving apart—a process known as rifting. Volcanoes occur along both subduction and rift zones but are generally absent along strike-slip plate margins.