The Kunene Region in north-western Namibia hosts a lesser-known but geologically significant resource: chromium, a critical metal used in stainless-steel and alloy production.
While copper and cobalt dominate current exploration headlines, geological surveys have confirmed chromite—the principal chromium ore—in Kunene’s layered mafic and ultramafic rocks.
Chromium in Kunene occurs mainly within the Kunene Anorthosite Complex and associated mafic–ultramafic satellite intrusions of the Kaoko Belt.
These rocks are ancient, igneous in origin, and display similarities to major global chrome-bearing systems such as South Africa’s Bushveld Complex and Zimbabwe’s Great Dyke.
The most clearly documented locality is the Ombuku peridotite-gabbronorite body near Epupa, which contains massive chromitite seams recorded in geological literature. Chromite is also listed among the recognised commodities for the Kunene Region in Namibia’s mineral database.
Early mapping by the Geological Survey of Namibia in the 1960s and 1970s identified small chromite showings in the Kaoko Belt, particularly around Ombuku. At that time, Kunene’s isolation and lack of infrastructure prevented detailed evaluation.
Modern geochemical surveys confirm that the area’s high magnesium and iron oxide content provides favourable conditions for chromite formation.
The Epembe area, often mentioned in connection with critical-metal exploration, is primarily a niobium–tantalum–rare-earth carbonatite and not a chrome target. However, it lies within the broader magmatic province that hosts the chromite occurrences.
The chrome-prospective ultramafic terrain around Opuwo, Etanga, and Epupa now falls under several exploration licences.
Aldoro Resources Limited originally held ground in north-western Namibia through its subsidiary Gunex Pty Ltd, focusing on nickel and PGE mineralisation in mafic intrusions that also contain accessory chromite. In September 2025, Sultan Resources Limited announced the acquisition of Gunex and its Namibian assets, thereby inheriting these licences. Sultan’s technical reports acknowledge the presence of chromite and magnetite mineralisation within Kunene’s layered gabbros.
Namibia Critical Metals Inc. also operates across the Kaoko Belt and lists chromium among minor associated minerals encountered during regional exploration for cobalt and rare earths.
No exploration company has yet declared a JORC- or NI 43-101-compliant chromium resource, and no active chrome-focused drilling has been reported publicly. Existing references remain geological rather than economic.
Ombuku in the Epupa District is the best-documented occurrence, containing a massive chromitite layer within ultramafic rocks. The Etanga–Opuwo corridor hosts ultramafic satellites that include magnetite- and chromite-bearing gabbros, though work remains at the reconnaissance stage.
The Sesfontein area contains minor chromite and iron-oxide showings, which are noted in the layered mafic bodies of the Kunene Complex.
Chromium is indispensable to stainless-steel and heat-resistant alloy production. Global demand is projected to rise in line with construction, manufacturing, and renewable-energy infrastructure growth. If Kunene’s chromite occurrences can be delineated at scale, Namibia would gain entry into the ferrochrome value chain that South Africa and Zimbabwe currently dominate.
Kunene’s terrain remains remote, with few paved roads north of Opuwo and limited energy infrastructure. Opuwo functions as the logistical centre for exploration campaigns. Improved road links, airborne magnetic surveys, and future geophysical data will be necessary before any detailed chrome assessment can proceed.
The magmatic layering of the Kunene Anorthosite Complex hosts alternating seams rich in magnetite, ilmenite, and chromite. Petrological studies show Cr₂O₃ enrichment consistent with primary chromite segregation. These findings suggest potential for stratiform chromite mineralisation typical of large igneous provinces.
At present, chromium in Kunene remains at an early exploration stage, with no defined resource or operational mine. However, the geological evidence—especially the chromitite at Ombuku—demonstrates that the region holds genuine potential for future chrome development once systematic drilling and evaluation begins.
With its established mining legislation and emerging infrastructure, Namibia could eventually extend its mineral portfolio beyond copper, cobalt, and rare earths to include chrome, adding another critical metal to its resource base.
