EARTHCACHE: Waterberg Plateau, Namibia.
Rising up to 200 meters above the surrounding landscape, the Waterberg Plateau in Namibia tells a story that began nearly 130 million years ago during the breakup of Gondwana. As Africa and South America separated, powerful tectonic forces reshaped the region, uplifting rock layers and leaving behind the dramatic plateau seen today.
The plateau’s striking red cliffs are composed of porous sandstone from the Etjo Formation—ancient petrified desert dunes deposited ~190 million years ago. Beneath it lies the older Omingonde Formation, made up of conglomerate, sandstone, and mudstone from an even older lake-filled environment.
But the geology here does more than shape the landscape; it controls water. Rainfall is absorbed into the sandstone like a giant sponge, then redirected along the underlying impermeable rock layer to emerge as springs at the plateau’s edge, giving Waterberg (“water mountain”) its name.
Namibia is also a fitting backdrop to GSA’s 2026 Thompson Field Forum, where participants are currently exploring the southern region’s extraordinary geologic history, landscapes, and field relationships firsthand.
🧭 Explore this EarthCache at:
geosociety.co/GCAZ4DK
📍Location: Waterberg Plateau, Namibia
📊 Difficulty: 2/5 | Terrain: 3/5
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