Kilimanjaro is a massive stratovolcano located near the border of Kenya and Tanzania. It formed as part of the tectonic activity associated with the East African Rift System. The mountain is famous for its disappearing glaciers and diverse ecological zones. Although there is no recorded history of an eruption, fumaroles (steam vents) in the Kibo crater indicate that heat is still present beneath the surface. It is a major destination for mountaineers and a critical water tower for the surrounding semi-arid plains of Tanzania.