Deep Sea Mining Map: Track ISA Concessions, Hydrothermal Vents, and Ocean Biodiversity

Deep-sea mining is reshaping the ocean floor — and most of it happens out of sight. Abyssal Claims is an independent transparency platform mapping every active International Seabed Authority (ISA) exploration contract, every documented hydrothermal vent field, and the biodiversity at risk, alongside 30+ ocean and land environmental data layers on an interactive 3D globe. Built for researchers, journalists, policymakers, and the public.

Ocean Data Layers

Land Data Layers

What Is Deep-Sea Mining?

Deep-sea mining is the extraction of metals — polymetallic nodules, seafloor massive sulphides, and cobalt-rich crusts — from the ocean floor at depths of 1,000 to 6,000 metres. The International Seabed Authority (ISA) regulates mining in international waters and has issued exploration contracts across the Pacific (Clarion-Clipperton Zone), Indian, and Atlantic Oceans. Commercial extraction could begin within years, despite incomplete environmental impact data and unresolved questions about damage to hydrothermal vent ecosystems and deep-sea biodiversity.

This map tracks every active ISA concession alongside the vents, species observations, and ocean monitoring data those concessions overlap — connecting policy, ecology, and infrastructure in one view.

Frequently Asked Questions

What is deep sea mining?

Deep-sea mining is the industrial extraction of mineral deposits — polymetallic nodules, seafloor massive sulphides, and cobalt-rich crusts — from the ocean floor, typically at depths of 1,000 to 6,000 metres. The metals (nickel, cobalt, manganese, copper, rare earth elements) are used in batteries and electronics. Mining is regulated by the International Seabed Authority (ISA) in international waters and by national agencies within Exclusive Economic Zones.

Where is deep sea mining happening?

Most active deep-sea mining exploration is concentrated in the Clarion-Clipperton Zone (CCZ) of the Pacific Ocean between Hawaii and Mexico, with additional contracts in the Indian Ocean, Mid-Atlantic Ridge, and Western Pacific. The interactive map shows every active ISA exploration and exploitation contract alongside national leasing zones from BOEM, NOPTA, NSTA, and other registries. As of 2026, no commercial-scale deep-sea mining has begun, but tests of nodule-collector vehicles started in 2022.

Is deep sea mining legal?

Deep-sea mining in international waters is legal under exploration contracts issued by the International Seabed Authority, but commercial exploitation requires a separate Mining Code the ISA has been negotiating since 2014. Within national waters, individual countries (e.g., Norway, Cook Islands, Papua New Guinea) set their own rules. Several countries — including France, Germany, Spain, Chile, and Palau — have called for a moratorium or precautionary pause until environmental impacts are better understood.

How does deep sea mining damage ecosystems?

Deep-sea mining disturbs the seafloor at depths where ecosystems recover slowly — sediment plumes can travel hundreds of kilometres and smother filter-feeding life, while light and noise pollution affects species adapted to total darkness. Hydrothermal vents host species found nowhere else on Earth, and even small-scale disturbance can extirpate entire populations. Recovery timescales for polymetallic nodule fields are estimated in millions of years.

Who regulates deep sea mining?

The International Seabed Authority (ISA), based in Kingston, Jamaica, regulates deep-sea mining in "the Area" — the seabed beyond national jurisdiction, roughly 54% of Earth's seafloor. The ISA has 168 member states and operates under the UN Convention on the Law of the Sea (UNCLOS). Within national EEZs, regulation is handled by domestic agencies such as BOEM (USA), NOPTA (Australia), NSTA (UK), Sodir (Norway), CNH (Mexico), and others — all surfaced as separate layers on this map.

What metals are in deep-sea mining nodules?

Polymetallic nodules contain primarily manganese (~28%), iron (~6%), nickel (~1.3%), copper (~1.1%), and cobalt (~0.2%), plus trace rare earth elements. Seafloor massive sulphides are richer in copper, zinc, gold, and silver. Cobalt-rich crusts grow on seamount surfaces and contain up to 1.5% cobalt with significant tellurium and platinum-group metals. Demand is driven by battery metals for EVs and grid storage.

Data Sources