The Makgadikgadi Pans are one of the largest salt pan systems in the world, covering an area of over 16,000 km², with the main pans—Sua Pan, Nxai Pan, and Ntwetwe Pan—spanning more than 8,400 km². These pans are the remnants of an ancient inland lake, once covering an area roughly the size of Switzerland. The lake was gradually reduced to the pans we see today due to the natural processes of evaporation and the disruption of the water supply from the surrounding rivers, which were cut off as a result of plate tectonics.

As the vast lake evaporated, salt accumulated in the depression created by the lowest point in the region. Over time, this led to the formation of thick layers of salt, which can be up to five meters deep. This arid, saline landscape is now a striking feature of the Botswana wilderness, where the absence of permanent water sources has resulted in the area being largely uninhabited by humans.

Though the pans themselves have never been settled, the surrounding villages were granted permission to graze their herds on the fringes of the area. Despite its seemingly inhospitable appearance, the pans are home to a rich diversity of life, particularly during the rainy season when the landscape transforms into lush grasslands, drawing wildlife such as zebras, wildebeests, and a variety of migratory birds.

The Makgadikgadi Pans also hold cultural and historical significance. They are believed to have been an important site for early humans, with evidence of ancient human habitation found in the form of stone tools and archaeological remains. The area is also home to some of the largest and most iconic baobab trees, which have been landmarks for centuries, helping explorers like David Livingstone navigate the vast wilderness.

This area offers a unique opportunity to witness the extraordinary contrast of life and desolation, and it remains one of Botswana’s most intriguing natural and cultural wonders.