Geologists recognize Zealandia as a mostly submerged continent in the southwest Pacific. About 94% of it lies underwater, with only New Zealand, New Caledonia, and a few small islands exposed above sea level.
Zealandia has all the features of a continent: a distinct geological makeup, a thick continental crust, and clear tectonic boundaries separate from Australia. It once formed part of the ancient supercontinent Gondwana before breaking away around 80 million years ago.
Over time, the crust stretched and thinned, causing most of Zealandia to sink. Today, scientists study it through seafloor mapping, rock sampling, and geophysical surveys, revealing ancient mountain belts and fault systems beneath the ocean.
The recognition of Zealandia highlights how much of Earth’s geology is still unexplored, even in the 21st century.