The Jebel Sirwa, or Siroua, Adrar Sirwa or Adrar n'Siroua, link between the High Atlas and the Anti-Atlas, is a high and very vast dismantled volcano from which singularly emerge dykes and bases black lava. Siroua is in fact an ancient stratovolcano of late Miocene-early Pliocene age.
The Jebel Sirwa, or Siroua, Adrar Sirwa or Adrar n'Siroua, link between the High Atlas and the Anti-Atlas, is a high and very vast dismantled volcano from which singularly emerge dykes and bases black lava. Siroua is in fact an ancient stratovolcano of late Miocene-early Pliocene age.
The Jebel Sirwa, or Siroua, Adrar Sirwa or Adrar n'Siroua, link between the High Atlas and the Anti-Atlas, is a high and very vast dismantled volcano from which singularly emerge dykes and bases black lava. Siroua is in fact an ancient stratovolcano of late Miocene-early Pliocene age.
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The Jebel Sirwa, or Siroua, Adrar Sirwa or Adrar n'Siroua, link between the High Atlas and the Anti-Atlas, is a high and very vast dismantled volcano from which singularly emerge dykes and bases black lava. Siroua is in fact an ancient stratovolcano of late Miocene-early Pliocene age.
