NOAAA map of Zealandia, outlined in grey.

• Scientists confirmed the existence of an eighth continent, called Zealandia, under New Zealand and the surrounding ocean in 2017.
• Because 94% of Zealandia’s 2 million square miles are underwater, mapping the continent is challenging.
• Researchers just released maps that show Zealandia in unprecedented detail, revealing its shape and how it was formed millions of years ago.

About 3,500 feet under the south Pacific waves sits a lost eighth continent.

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Scientists confirmed that the submerged land mass, named Zealandia, was its own continent in 2017. But they hadn’t been able to map its full breadth until now.

On Monday, researchers from GNS Science in New Zealand announced that they’d mapped the shape and size of the continent in unprecedented detail. They put their maps on an interactive website so that users could virtually explore the continent.

“We’ve made these maps to provide an accurate, complete, and up-to-date picture of the geology of the New Zealand and southwest Pacific area – better than we have had before,” Nick Mortimer, who led the work, said in a statement.

Mortimer and his colleagues mapped the bathymetry surrounding Zealandia – the shape and depth of the ocean floor – as well as its tectonic profile, showing where Zealandia falls across tectonic-plate boundaries.

The maps reveal new information about how Zealandia formed before it became submerged underwater millions of years ago.

An underwater continent nearly 2 million square miles in size

Zealandia’s area is nearly 2 million square miles (5 million square kilometers) – about half the size of Australia.

But only 6% of the continent is above sea level. That part underpins New Zealand’s north and south islands and the island of New Caledonia. The rest is underwater, which makes Zealandia challenging to survey.

To better understand the submerged continent, Mortimer and his team mapped both Zealandia and the ocean floor around it. The bathymetric map they created (below) shows how high the continent’s mountains and ridge rise toward the water’s surface.

A bathymetric map of Zealandia, which shows the shape of the continent under the water.

It also depicts coastlines, territorial limits, and the names of major undersea features. The map is part of a global initiative to map the planet’s entire ocean floor by 2030.

The second map the GNS scientists made (below) reveals the types of crust that make up the underwater continent, how old that crust is, and major faults. The continental crust – the older, thicker kind of Earth’s crust that forms landmasses – is shown in red, orange, yellow, and brown. The oceanic crust, which is generally younger, is in blue. Red triangles show where volcanoes are.

A tectonic map of Zealandia, which shows the types and age of the crust, major faults, and volcanoes that make up the continent.

This map also reveals where Zealandia sits across various tectonic plates, which of those plates are being pushed under the other in a process known as subduction, and how quickly that movement is happening.

Studying the tectonic machinations that underpin Zealandia today can reveal clues about how the continent formed in the first place.

Zealandia’s 85 million-year-old origins

The concept of Zealandia is 25 years old. Geophysicist Bruce Luyendyk coined the term in 1995.

Luyendyk previously told Business Insider that he never intended for the term to describe a new continent. Rather, the name originally referred to New Zealand and a collection of submerged chunks of crust that broke off the ancient supercontinent Gondwana about 85 million years ago.

“The reason I came up with this term is out of convenience,” Luyendyk said. “They’re pieces of the same thing when you look at Gondwana. So I thought, ‘Why do you keep naming this collection of pieces as different things?'”

Gondwana formed when Earth’s ancient supercontinent, Pangea, split into two fragments. Laurasia in the north became Europe, Asia, and North America. Gondwana in the south dispersed to form modern-day Africa, Antarctica, South America, and Australia.

Geologic forces continued to rearrange these land masses, and Zealandia was forced under the waves about 30 million to 50 million years after it broke off Gondwana as the largest tectonic plate – the Pacific Plate – slowly subducted beneath it.

These maps show Zealandia is a continent like the other 7

Until 2017, Zealandia was classified as a “microcontinent,” like the island of Madagascar. But according to Mortimer, Zealandia ticks all the boxes for continent status: It has clearly defined boundaries, occupies an area greater than 386,000 square miles (1 million square kilometers), is elevated above the surrounding ocean crust, and has a continental crust thicker than that oceanic crust.

These new maps therefore offer further evidence that the underwater land mass should be considered the eighth continent, Mortimer added.

“If we could pull the plug on the world’s oceans, it would be quite clear that Zealandia stands out,” he told Science News in 2017, adding, “If it wasn’t for the ocean level, long ago we’d have recognised Zealandia for what it was – a continent.”