Queen Elizabeth National Park

Ecosystem Overview and Rift Valley Landscape

Spanning 1,978 square kilometres across western Uganda, Queen Elizabeth National Park was founded in 1952 and designated a UNESCO Man and the Biosphere Reserve in 1979. Situated on the floor of the Western Albertine Rift Valley, the park encompasses an extraordinary mosaic of habitats: open savannas, moist deciduous woodlands, humid riverine forests, freshwater lakes, and dozens of extinct volcanic explosion craters.

To the north, the snow-draped peaks of the Rwenzori Mountains (Mountains of the Moon) frame the skyline on clear mornings, while the park borders the Democratic Republic of Congo's Virunga National Park to the west across Lake Edward.

The Kazinga Channel: Aquatic Life Corridor

The ecological centerpiece of the park is the 32-kilometre natural Kazinga Channel, which connects Lake George in the east with Lake Edward in the west. Scheduled two-hour boat safaris depart from the Mweya Peninsula, offering front-row views of one of the world's highest concentrations of hippopotamuses.

Along the channel banks, herds of African elephants bathe and drink alongside water buffaloes, Nile monitor lizards, and waterbucks. Birdlife is extraordinarily prolific, featuring yellow-billed storks, pink-backed pelicans, African skimmers, and pied kingfishers hovering above the shallows.

Tree-Climbing Lions of the Ishasha Sector

In the southern Ishasha sector of the park, visitors encounter a rare behavioral phenomenon: tree-climbing lions. Prides regularly scale the horizontal branches of large sycamore fig trees and albizia trees during the midday heat.

Wildlife biologists suggest this behavior serves multiple practical purposes: escaping ground heat and irritating biting tsetse flies, while gaining an elevated vantage point across the savanna to monitor grazing herds of Uganda kob and topi antelopes.

Kyambura Gorge: The Valley of Apes

On the eastern edge of the park lies the dramatic Kyambura Gorge, an underground sunken forest carved 100 metres deep into the savanna floor by the Kyambura River. Known colloquially as the 'Valley of Apes,' this isolated subterranean riverine rainforest shelters an isolated troop of habituated eastern chimpanzees, black-and-white colobus monkeys, and colorful forest birds.

Katwe Explosion Craters and Salt Mining

In the northern sector, the scenic 27-kilometre Crater Drive winds through extinct volcanic calderas formed thousands of years ago. At Lake Katwe, visitors observe traditional salt extraction techniques that have operated continuously since the 16th century, where local workers evaporate saline brine in shallow evaporation pans.

Seasons, Access and Travel Logistics

Queen Elizabeth National Park is productive year-round. Drier months from January to February and June to August provide optimal game drive track conditions and high wildlife concentrations along the Kazinga Channel. The green seasons from March to May and September to November produce lush emerald scenery and migratory bird arrivals.

The park is located approximately 410 kilometres southwest of Kampala, taking about six to seven hours via Mbarara or Fort Portal. Scheduled light aircraft flights land at Kasese Airstrip (60 minutes from Mweya) or Mweya's private runway.

Frequently Asked Questions

Why do lions climb trees in the Ishasha sector?

Lions in Ishasha climb large sycamore fig trees to rest away from ground flies and midday heat, while enjoying cooling breezes and an elevated view of grazing antelope herds.

What is the recommended time for Kazinga Channel boat safaris?

Afternoon departures (typically 2:00 PM and 4:00 PM) generally offer the highest concentration of animals along the water's edge as elephants, buffaloes, and antelopes come down to drink and bathe.

Are chimpanzee sightings assured in Kyambura Gorge?

Because the Kyambura chimpanzee community is relatively small and roams through a dense, deep gorge corridor, sightings cannot be assured on every excursion, though the hike through the subterranean rainforest is scenic in itself.