The Tundavala Gap is the edge where the high plateau of Angola stops and falls 1,200 metres to the coastal plain, a fissure in the escarpment fifteen kilometres from the city of Lubango in Huíla province, unfenced, with the morning cloud of the dry season often filling the lowland below so that the rim stands above a white sea, and it is walked out to along the split between two walls of stone until the rock simply ends. The escarpment is the boundary between the provinces of Huíla and Namibe, the great step of southern Africa where the plateau of 2,200 metres drops to the desert coast, and the stone underfoot is roughly 1.79 billion years old while the cliff is young, cut back by the rivers of the plain; the gap is a slot cut back into the clifftop between two walls of stone, followed out over broken ground to a point with nothing beneath it, and from the rim the land opens across some 10,000 square kilometres of the plain, ridge stacking behind ridge into the haze, with the road to Namibe winding down the face at the Leba pass to the south. The name does not describe the view but comes from the Nyaneka word for the place.
In the cacimbo, the dry season of May to September, fog off the cold Atlantic pushes inland and fills the plain 1,200 metres below the rim, burning away toward midday on many mornings, and the grassland of the plateau goes copper in the late afternoon light. Birders travel a long way for the Angola cave-chat, a cliff-crevice nester recorded at only about eight sites on Earth, which breeds in the crevices of these cliffs from September to November, and the rocks hold the rock hyrax and the baboons. Lubango below the plateau is the city of the Christ statue and the Portuguese settlers, and the gap is its Sunday outing, with picnics at the edge and no rail. Tundavala is the place where a country's tableland ends, and the drop is the whole view.