Raymond’s Geology Blog

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October 27, 2025

News and notes

A path in the Bush, Fall 2025

This week, before going on to discuss the geology and mineral resources of Mauritius, we will first look at some news items I thought were interesting. If you enjoy my blogs, bookmark the site and check Monday mornings rather than relying on social media postings which can get lost in the shuffle.

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October 27, 2025

Geology and Mineral Resources – Mauritius

Introduction

Figure 1a – Mauritius
Credit: CIA World Factbook, public domain

Figure 1b – Location of Mauritius
Credit: CIA World Factbook, public domain

A former British and French colony, the Republic of Mauritius is an island country of 1,310,504 people in the Indian Ocean, east of Madagascar. The country has an total area of 2,040 square kilometres and includes the main island of Mauritius together with Agalega, Cargados Carajos Shoals (Saint Brandon), and Rodrigues Island. Mauritius, together with its smaller territories, is part of a larger geographic entity, the Mascarene Islands, which also includes the French Department of Réunion.

Figure 2 – Chagos Archipelago and Mauritius
Credit: Yashveer Poonit, WikiForMen, Creative Commons
 Attribution-Share Alike 3.0 Unported license

Mauritius also claims the Chagos Archipelago and has been in a territorial dispute with the United Kingdom over the Archipelago since 1965. The Chagos Archipelago includes the strategic naval base of Diego Garcia and, until very recently, the U.K. has been loathe to give up ownership of the islands. However, as of October 20, 2025, the U.K. government has ceded the Chagos Archipelago to the Republic of Mauritius.

Mauritius enjoys a moderately high standard of living with a per capita GDP (PPP) of $33,954 and a very high Human Development Index of 0.806. Mauritius has a diversified economy, based on tourism, textiles, sugar, and financial services. For more details on the country, check out the CIA World Factbook on Mauritius as well as the Wikipedia article.

Geology

Figure 3 – Track of the Réunion Hotspot Chain, Credit: Figure 1 in Torsvik et al, 2013

Mauritius is a volcanic island that owes it origin to the Réunion Hotspot and the tectonic forces that drove the Indian subcontinent northeastward from Gondwana towards the Eurasian Plate during the Late Cretaceous Epoch and into the Eocene Epoch. These same tectonic movements are responsible for the volcanic rocks underlying the Chagos Archipeligo, the Maldive Islands and the Deccan Traps in India. Overall, the volcanic rocks originating in the Réunion Hotspot form part of the Deccan Large Igneous Province.

Figure 4 – Geology of Mauritius
Credit: Figure 1 in Paul, White, & Blichert-Toft, 2005

Recent studies divide the volcanic rocks of Mauritius into three categories:

  • The Older Series, dated at 8.9 million years ago (Mya) to 4.7 Mya.

  • An Intermediate Series, dated at 3.5 to 1.9 Mya and,

  • A Younger Series, dated at 113 ± 7 thousand years ago (Kya) to 14 ± 3 Kya.

The Older Series volcanic rocks in Mauritius were extruded in two phases: a shield-building phase consisting of picrobasalt flows and agglomerate; and a second stage composed of feldsparphyric basalt, hawaiite, mugearite, and trachytic intrusive rocks. The Intermediate Series consists of olivine-phyric alkali basalt, basanite, and nephelinite while the Younger Series consists predominantly of potassium-poor alkaline olivine basalts with subordinate basanite.

Mineral Resources

Figure 5 – Salt Production, Tamarin, Mauritius
Credit: Arne Müseler, Creative Commons
 Attribution-Share Alike 3.0 Germany license


The mineral industry of Mauritius is limited to locally produced building materials – crushed stone, sand and gravel – and sea salt. Sea salt is produced at evaporation ponds near the west coast town of Tamarin.

The most recent complete USGS report on the mineral industry in Mauritius is from 2014. The most recent production statistics on the Mauritian mineral industry are from 2022.

While there are few potential mineral deposits to develop onshore Mauritius, there are at least two possible offshore development possibilities: petroleum and polymetallic nodules.

In 2012, the Mauritian government passed a bill to regulate petroleum exploration in their economic zone. However, although Mauritius and the Seychelles have an agreement to regulate their Joint Management Area on the Mascarene Plateau, there has been little actual petroleum exploration. The story about polymetallic nodules is similar. While there has been some discussion on deep-sea mining and the Mauritanian government has reiterated its claim to the resources within their economic zone, there is no publicly available information on deep-sea mining near Mauritius. As I discussed in my posting on the Marshall Islands, there is little to stop pirate operators from simply dredging up polymetallic nodules and disappearing.

Figure 6, below, links to an interactive mineral occurrence map for Mauritius.

Figure 6 – Interactive Mineral Occurrence Map of Mauritius
Credit: ©Mindat.org

Summary

Figure 7 – Blue Bay, Mauritius
Credit: Z thomas, Creative Commons
 Attribution-Share Alike 4.0 International license

That winds it up for this look at the geology and mineral industry of Mauritius. The potential for future development seems to be limited. There could be petroleum and/or natural gas offshore of Mauritius, but so far there seems to little interest. Polymetallic nodules from deep-sea mining are another possibility, but it is entirely possible that the extraction of these nodules will do little for the inhabitants of Mauritius.

Standard Caveat

J. Robert Oppenheimer on freedom and scientific inquiry

The purpose of my weblog postings is to spark people's curiosity in geology. Don't entirely believe me until you've done your own research and checked the evidence. If I have sparked your curiosity in the subject of this posting, follow up with some of the links provided here. If you want to, go out into the field and examine some rocks on your own with the help of a good field guide. Follow the evidence and make up your own mind.

In science, the only authority is the evidence.