Situated on the Zambia–Zimbabwe border along the Zambezi River, Victoria Falls is experienced from the Zambian side within Mosi-oa-Tunya National Park, where walkways trace the cliff edge above a vast basalt gorge. Knife Edge Bridge pushes visitors into the spray line for a close view of the Main Falls, a continuous curtain of water, and the Eastern Cataract, where the flow breaks into narrower channels across the far side. Rainbow Falls, the highest section of the cascade, often reveals shifting arcs of colour in fine mist when light breaks through the spray. The Boiling Pot viewpoint looks directly into a deep whirlpool where the river is forced into the Batoka Gorge. Upstream, boat access reaches Livingstone Island, a rocky outcrop on the lip of the falls, and the seasonal Devil’s Pool, a natural rock pool at the edge of Victoria Falls that becomes safely accessible during low water when river levels drop and currents weaken. Activities extend beyond the rim, including white-water rafting through gorge rapids, kayaking, ziplining across the chasm, bungee jumping from the bridge, bridge swings, sunset cruises, game viewing along the riverbanks, and visits to the local market.
From its source in the North-Western Province of Zambia, the Zambezi flows into Angola before re-entering Zambia and meandering down to the breathtaking spectacle of one of the world’s largest waterfalls, the Victoria Falls. This section of the river above the falls forms a natural border between Zimbabwe and Zambia, and it is here that most water-based activities take place. While the Zimbabwean banks are home to the Zambezi National Park, the Zambian banks are dotted with lodges blending into the natural landscape. The ideal way to appreciate the beauty of the Upper Zambezi is on a guided canoe trip, during which you can camp overnight on the river banks. Exhilarating wildlife encounters can be experienced as your canoe slips silently past a group of hippos, a crocodile lazing in the sun, or a herd of elephants drinking at the water’s edge.
As previously described