Lake Katwe
Lake Katwe is a saline crater lake in western Uganda where local miners still extract salt by hand from shallow evaporation pans.
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Overview and significance
The Katwe craters or Katwe-Kikorongo explosion craters are a group of volcanic craters within Queen Elizabeth National Park in Toro, Uganda. The volcanic field is roughly 210 km2 (81 sq mi) in size. The individual craters vary widely in size, but the largest are up to 3 km (1.9 mi) in diameter and 100 m (330 ft) deep. The unusual formations were formed individually by a series of violent volcanic explosions over the last 1 million years. These maar craters are a result of magma coming in contact with groundwater driving large steam explosions. The explosive events created large, low lying craters with few other signs of volcanic activity.
History and heritage
The falls and surrounding river landscape form part of the wider living environment of Uganda, where water, local livelihoods and visitor access meet. Respect for local knowledge and safety practices is essential.
Features and attractions
Flowing water, rock, spray and changing river levels define the scenery. Appearance and intensity can shift with rainfall, season and upstream conditions.
Activities and experiences
Visitors may photograph the falls, walk to marked viewpoints or arrange specialist activities such as rafting or guided river experiences through licensed operators where available.
Visitor information
Do not enter fast water independently. Confirm access routes, operator credentials, safety equipment and weather or water levels before any adventure activity, and follow posted restrictions.
This editorial information is a starting guide. Verify current visitor rules, fees and access with the official operator.