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India’s Second Mineral Exploration Contract

Kartavya Desk Staff

Source: IE

Context: India has secured a second exploration contract from the International Seabed Authority (ISA) for Polymetallic Sulphides (PMS) in the Carlsberg Ridge, Indian Ocean.

• This makes India the first country with two PMS contracts, commanding the largest allocated area for PMS exploration globally.

About India’s Second Mineral Exploration Contract:

What it is?

• Signed with ISA under UNCLOS framework for a 10,000 sq. km area in Carlsberg Ridge.

• Exploration will be carried out by the National Centre for Polar and Ocean Research (NCPOR) from 2026.

• To secure strategic minerals critical for India’s energy transition, high-tech manufacturing, and resource security.

• To strengthen India’s role in the Blue Economy and Deep Ocean Mission.

Features:

• Builds on India’s first PMS contract (2016) in Central & Southwest Indian Ridge.

• Exploration plan: Reconnaissance surveys (ship-mounted tools). Near-seabed surveys (AUVs, ROVs). Resource evaluation of deposits.

Reconnaissance surveys (ship-mounted tools).

Near-seabed surveys (AUVs, ROVs).

Resource evaluation of deposits.

• Supported by India’s Samudrayaan mission and deep-sea technology development.

About Carlsberg Ridge:

What it is?

• A major mid-ocean ridge system in the Indian Ocean formed by seafloor spreading.

Located in:

• Extends from the triple junction of African, Indian & Australian plates (near 2°N, 66°E) towards the Gulf of Aden.

• Separates Arabian Sea (NE) from Somali Basin (SW).

Features:

• Formed ~40 million years ago, with a spreading rate of 2.4–3.3 cm/year.

Depth: 1,800–3,600 m below sea surface.

• Has median valley, rugged topography, typical of slow-spreading ridges.

• Known for hydrothermal vent systems, rich in PMS deposits.

• Closer to India (~2°N) than earlier exploration sites (~26°S).

• Lies in a seismically active zone, linked to the East African Rift System.

About Polymetallic Sulphides (PMS):

What it is?

Mineral deposits formed on ocean floors near hydrothermal vents.

• Created when cold seawater interacts with magma, ejects hot mineral-rich fluids, depositing solids on seabed.

Found in: Along mid-ocean ridges and hydrothermal vent fields at depths of 2,000–5,000 m.

Composition: Rich in copper, zinc, lead, silver, gold, and trace amounts of rare/precious metals.

Applications:

• Electronics & high-tech industries (copper, rare metals).

• Green energy systems (zinc, silver for solar & batteries).

• Strategic use in aerospace, defence, and clean-tech manufacturing.

AI-assisted content, editorially reviewed by Kartavya Desk Staff.

About Kartavya Desk Staff

Articles in our archive published before our editorial team was expanded. Legacy content is periodically reviewed and updated by our current editors.

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