Lebombo Mountains, Mountain range between South Africa, Mozambique and Eswatini.
The Lebombo Mountains are a ridge system spanning three countries, formed primarily of basalt and rhyolite rock. The range rises in varying heights across the landscape, with the tallest peak reaching approximately 776 meters above sea level.
The mountains formed as part of a rifted volcanic margin linked to the breakup of the Gondwana supercontinent. This volcanic origin shaped the geological character of the region that persists today.
The mountains take their name from the Zulu word Ubombo, describing how the ridge resembles a large protruding nose. This name reflects how local people have long understood and talked about this landform.
Several rivers flow through the range from west to east, providing water resources across the region. The terrain varies from steep to rolling, so visitors should plan for diverse conditions depending on the season and chosen route.
The valleys support tropical forests with African mahogany trees, while the well-drained slopes host ironwood and ebony species. This mix of tree types reflects how elevation and soil conditions create distinct growing zones across the range.
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