Lochinvar National Park

Lore & Background

Lochinvar National Park protects a large portion of the southern Kafue Flats floodplain, including the Chunga Lagoon, and drier woodland dominated by termite mounds. The park also contains hot springs, echoing rocks, remains of a Neolithic settlement, and an Iron Age village on Sebanzi Hill, which is known for its caves, ancient baobab, and wildlife. The northern boundary is marked by the Kafue River, while wooded hills lie to the south.

Reader's Guide

Lochinvar National Park is significant for its conservation of the Kafue lechwe and its rich birdlife, with over 400 species recorded. The park is very similar to Blue Lagoon National Park on the opposite side of the Kafue River. Antelope and birds thrive here due to the absence of larger predators, which were killed off by ranchers in the area. The southern area, a stretch of woodland dominated by Faidherbia albida and Combretum trees, is spared from flooding and hosts species such as bushbuck, kudu, baboon, bushpig, and vervet monkey. The marshes support large numbers of waterfowl, including migratory species. As of 2026, no accommodation is available in or near the park, but visitors may camp with their own gear. The old colonial-style farmhouse that once served as the lodge has been closed for many years.

Did You Know?

• The park was originally a ranch named after a loch in Galloway, Scotland.
• It is home to hot springs, echoing rocks, and remains of a Neolithic settlement.
• The park's northern boundary is marked by the Kafue River.
• No accommodation is available in or near the park as of 2026, but camping is permitted.

Geography & Landscape

Lochinvar National Park stretches across 428 square kilometres of Zambian terrain, positioned to the south-west of the capital city of Lusaka. Its northern edge is defined by the Kafue River, which also serves as a natural dividing line with Blue Lagoon National Park on the opposite, northern bank of the flats. South of the river, the landscape transitions into wooded hills, creating a varied topography within a single protected area. The park encompasses a significant stretch of the southern Kafue Flats floodplain, including the Chunga Lagoon, where seasonal inundation shapes the ecosystem. In contrast, the drier southern reaches are dominated by woodland of Faidherbia albida and Combretum trees, a zone that escapes the periodic flooding that reshapes the rest of the park. This interplay between wet and dry habitats, framed by the river to the north and forested highlands to the south, gives Lochinvar a distinctly layered character that sets it apart from more uniform savanna parks elsewhere in the country.

Wildlife & Ecology

The park's fauna is shaped as much by what is absent as by what is present. Because ranchers in the surrounding region eliminated larger predators over the decades, antelope and bird populations have flourished without the usual predation pressure. The Kafue lechwe, a wetland specialist, is the park's signature mammal, sharing the floodplain with blue wildebeest, kudu, and oribi. In the drier southern woodland, where Faidherbia albida and Combretum trees form the canopy, visitors encounter bushbuck, kudu, baboons, bushpig, and vervet monkeys. The birdlife is extraordinary: more than four hundred species have been documented, and the marshes support dense congregations of waterfowl, including migratory arrivals that follow seasonal routes across the continent. The absence of apex carnivores has created an ecosystem where grazing and browsing species thrive in numbers that would be unusual in a wild, unmanaged landscape, making Lochinvar a compelling case study in how human land-use history can reshape a natural community.

History & Heritage

Before it became a protected area, the land that is now Lochinvar National Park operated as a cattle ranch, a name borrowed from a loch in Galloway, Scotland, a nod to the colonial-era pastoral culture that shaped much of southern Zambia. The park was formally designated in 1972, transitioning from private grazing land to a national conservation zone. Yet the human story here stretches far deeper than the colonial period. Archaeological remains on the park's grounds include a Neolithic settlement and an Iron Age village situated on Sebanzi Hill, a site also noted for its caves and a remarkable ancient baobab tree. These layers of occupation suggest that the floodplain and its surrounding woodlands have sustained human communities for millennia. The old colonial-style farmhouse, once the operational lodge for park visitors, has long since closed its doors, leaving the landscape to tell its own layered story through rock, river, and root.

Visitor Experience & Current Status

Lochinvar occupies a deliberately quiet niche among Zambia's national parks. The colonial-era farmhouse that once served as the park's lodge shut down years ago, and as of 2026 there is no formal accommodation available within or in the immediate vicinity of the park. Visitors who wish to experience the floodplain, the hot springs, or the echoing rocks must bring their own camping gear and be prepared for a self-sufficient stay. This lack of infrastructure means the park remains largely untouched by the tourism machinery that has reshaped many of its counterparts. The result is a raw, unmediated encounter with the Kafue Flats: the lagoon at Chunga, the termite-mound-dotted woodlands, the caves of Sebanzi Hill, and the ancient baobab all exist without interpretive signage or guided circuits. For the independent traveller, this absence of commercial framing is the park's greatest asset, offering a landscape that still feels genuinely wild and unscripted.