Rock Identifier
Patronite (Vanadium sulfide (VS4))
mineral

Patronite

Vanadium sulfide (VS4)

A rare greenish-black vanadium sulfide that was historically one of the world's most important ores of vanadium.

Mohs hardness
2-2.5
Color
Greenish-black to black
Type
mineral

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Overview

Patronite is a rare vanadium sulfide (VS4), notable as one of the few minerals mined directly and importantly as an ore of vanadium. It is greenish-black to black, soft, and usually massive rather than well-crystallized, with a dull to slightly metallic appearance.

It was named after Antenor Rizo Patron, who was connected to the famous Peruvian deposit where it was discovered. For decades the Minasragra deposit in Peru was a leading source of the world's vanadium, with patronite as a principal ore mineral.

Because it is fine-grained and intimately mixed with carbonaceous material and other vanadium minerals, patronite is more important economically and scientifically than as a display specimen.

Formation & geology

Patronite formed in an unusual sedimentary-to-low-grade setting at Minasragra, near Cerro de Pasco, Peru, associated with vanadium-rich carbonaceous shales and asphaltite. There, vanadium concentrated in organic-rich black rock and combined with sulfur to produce patronite alongside other vanadium minerals.

It is associated with carbonaceous matter, pyrite, and secondary vanadium oxides and oxysalts that form on weathering. Comparable vanadium concentrations in organic-rich sediments occur elsewhere, but the Peruvian deposit remains the type and classic locality.

How to identify it

Patronite is hard to identify by eye because it is typically a soft (Mohs about 2-2.5), greenish-black to black massive material mixed with carbon-rich rock rather than forming distinct crystals. It has a relatively low to moderate density and dull luster.

Its greenish-black tint, softness, and association with vanadium-rich black shale and asphaltite are clues, but reliable identification usually requires chemical analysis. On weathering it is often accompanied by brightly colored secondary vanadium minerals, which can hint at its presence.

Uses & significance

Patronite's significance is as a vanadium ore. Vanadium is used mainly to strengthen and toughen steel (ferrovanadium alloys for tools, springs, and structural steel) and increasingly in vanadium redox flow batteries for grid energy storage, as well as in catalysts.

The Minasragra deposit made Peru a major early supplier of vanadium, giving patronite considerable historical economic importance. It has no gemstone or metaphysical use and is essentially never seen as a decorative specimen.

Frequently asked questions

What is patronite used for?

It is an ore of vanadium, a metal used to strengthen steel alloys, in catalysts, and in vanadium flow batteries.

Where is patronite found?

Its classic and economically important source is the Minasragra deposit near Cerro de Pasco, Peru.

Is patronite a common mineral?

No, it is rare; its importance comes from being a concentrated vanadium ore rather than from being widespread.

Why is vanadium important?

Vanadium greatly improves the strength and toughness of steel and is increasingly used in large-scale battery storage.