Etosha Pan

Etosha Pan is a vast salt pan in northern Namibia forming the central feature of Etosha National Park and recognised as one of the region’s major natural landmarks. The pan is an extensive, flat saline depression that can appear as a white, shimmering plain in dry conditions.

The pan and its bordering grasslands attract migratory birds and concentration of large mammals when seasonal rains bring water, and the park’s permanent waterholes provide predictable wildlife viewing points. Many visitors base themselves at park camps to observe elephants, lions, giraffe and other species that come to drink at these waterholes.

The Etosha Pan formed through long-term climatic and geological processes that left a saline depression in the landscape; it is largely dry most of the year but can hold shallow water after rains. The wider area has been managed as a protected national park since the 20th century to conserve its distinctive ecosystems and resident wildlife.

Geographically the pan lies in northern Namibia within Etosha National Park and is accessible from regional towns and park entrances; park camps and roads are arranged around the pan to facilitate wildlife observation.

• Scale: One of the largest salt pans in Africa, largely contained within Etosha National Park and visible as a bright expanse from satellite imagery.
• Viewing tip: Best wildlife viewing typically occurs in the dry season at permanent waterholes where animals gather, while the pan itself may hold shallow seasonal water after rains.

What to See #

• Central pan: The broad, pale salt flat that forms the central floor of the park and fills seasonally with shallow water, visible as a white expanse from roads and lookout points.
• Waterholes and camps: Park waterholes and camps such as Okaukuejo and Namutoni, which provide permanent or seasonal water sources attracting game and offering concentrated wildlife viewing.