The Ocean Column: Mining the Treasures of the Deep Sea
- Millie Webb

- Sep 24
- 4 min read
Updated: Nov 3
Polymetallic nodules on the deep seabed hold metals needed for clean energy. But as the world debates mining them, scientists warn of irreversible damage to fragile ecosystems which are still barely understood.
The World Beneath the Waves
The deep sea might look like a desolate, muddy wasteland, but in reality, it’s one of the richest and alien ecosystems on Earth. Stretching from 200 metres down to nearly 11,000 metres at its deepest point, this cold, dark realm could host as many as 10 million species, most of them still undiscovered.
Alongside this hidden biodiversity lie vast mineral riches. Over millions of years, metals such as nickel, copper, cobalt and manganese have slowly accumulated on the seabed in potato-sized lumps called polymetallic nodules. These were first discovered during the 1870s Challenger Expedition, the first major deep-sea voyage, but it wasn’t until the 1960’s when interest in using the nodules as a resource was considered.

The 19th Century Challenger Expedition revealed life in the deep sea and details of undiscovered seafloor geology, revolutionising oceanography forever. Image Credit: State Library Victoria on Wikimedia Commons.
The biggest concentration of the polymetallic nodules is found in the Clarion-Clipperton Zone (CCZ) of the Pacific Ocean, an area larger than the entire Amazon rainforest. Here, it is estimated that more than 21 billion tonnes of manganese, nickel and cobalt is scattered across the seafloor.

The Clarion-Clipperton Zone is an area rich in polymetallic nodules on the seafloor. Image Credit: US Geological Survey (Public Domain)
The nodules are now referred to as ‘battery rocks’ because the metals inside them are critical for modern technologies, from electric vehicles and renewable energy infrastructure to everyday electronic devices. Nodules can be extracted from the seafloor by deep sea mining, but since their discovery, there has been global debate about what to do with the CCZ and who can use it.

Polymetallic nodules, slow growing lumps of nickel, cobalt, manganese and copper found on the seafloor. Image Credit: Geomar Biddatenbank on Wikimedia Commons
Who Owns the Seabed?
Our oceans cover 71% of the Earth: this means that the seabed beneath it is larger than all land combined. So, how can an area of this size be managed? The United Nations attempted to answer this in 1982, when 169 states and the EU signed the UN Convention on the Law of the Sea (UNCLOS), which set rules for the use of the oceans. The treaty agreed that the seabed in international waters belongs to everyone and not one individual country.
The International Seabed Authority (ISA) was created under UNCLOS to regulate and authorise all deep-sea mining activity. In 2000, the ISA and its member states began developing a set of rules for deep sea mining, with the CCZ at the heart of the conversation. More than two decades later, the negotiations are still ongoing and as of this year, no deep-sea mining regulations have been agreed.
Amid this indecision, the United States has never ratified UNCLOS. In March, The Metals Company announced plans to apply for mining rights in the CCZ under US law. A month later, President Trump signed an executive order in support of deep-sea mining in international waters, widely criticised as a violation of international law. Because the US is outside UNCLOS, this move risks undermining international governance of the seabed and raises concerns of a scramble for resources in the deep.
The Deep Sea Under Threat
This political uncertainty only sharpens the question: if mining does go ahead, what would it mean for the deep sea?
Nodules are found across abyssal plains, about 4,000 metres below the surface. These are the largest habitats on Earth, covering more than half the planet’s surface, and are home to diverse marine life. Far from being barren, they are alive with sea cucumbers, urchins, worms, and shrimp, which together form seafloor communities.





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