Achávalite: The Rare Selenium Sentinel of the Sierras

While silver and uranium minerals often steal the spotlight with their luster and glow, the world of selenides holds its own quiet, metallic mystery. Achávalite (or Achavalite) is one of the rarest of the bunch—a mineral so elusive that for decades it was known from only a single mine system in the world.

Named after the Argentine engineer and professor Luis Achával, this mineral is a masterclass in “hidden” geology.


What is Achávalite?

Achávalite is an iron selenide mineral ($FeSe$). It belongs to the nickeline group, a family of metallic minerals that share a specific hexagonal crystal structure. First discovered in 1939, it was found tucked away in the selenide-rich veins of the Mendoza Province in Argentina.

In 2015, the International Mineralogical Association (IMA) officially updated the spelling from Achavalite to Achávalite to correctly reflect the accent in Luis Achával’s name.

Quick Facts:

  • Chemical Formula: $FeSe$ (often with traces of copper)

  • Color: Dark grey to iron-black.

  • Luster: Metallic to sub-metallic.

  • Hardness: 2.5 on the Mohs scale (soft and brittle).

  • Crystal System: Hexagonal.


The “One-Mine” Wonder

For a long time, Achávalite was considered a “single-locality” mineral. Its home was the Cacheuta Mine in the Sierra de Cacheuta, Argentina.

In this remote location, Achávalite forms as tiny, dark grains or massive granular patches within calcite veins. It isn’t a mineral you find in giant, showy crystals; instead, it’s often microscopic, intergrown with other rare selenides like Berzelianite (copper selenide) and Clausthalite (lead selenide).

Today, only a handful of other sites—such as the Zapadno-Ozernoe deposit in Russia—have reported its presence, making it a true prize for specialized “rare species” collectors.


A Chemical Powerhouse

Though it might look like a simple grey stone, Achávalite is chemically significant. It is the selenium-based analogue of Troilite (iron sulfide).

Why Selenium?

Most iron in the Earth’s crust bonds with sulfur to create minerals like Pyrite (Fool’s Gold). However, in very specific geological environments where sulfur is low and selenium is high, the iron is forced to bond with selenium instead. This “chemical swap” creates Achávalite.

The Superconductor Connection

Interestingly, synthetic iron selenide ($FeSe$)—the man-made version of Achávalite—is a superstar in the world of physics. It is a superconductor, meaning it can conduct electricity with zero resistance at certain temperatures. While natural Achávalite isn’t used to build quantum computers, its existence helps geologists understand how these unique elements behave in nature.


Identification and Handling

If you happen to find a piece of Achávalite, don’t expect it to stand out. It looks remarkably like many other metallic grey minerals. Identification usually requires:

  1. Polished Section Analysis: Looking at the mineral under a reflected-light microscope.

  2. X-Ray Diffraction (XRD): Confirming the hexagonal structure.

  3. Chemical Testing: Proving the presence of selenium over sulfur.

Safety Tip: Like many selenides, Achávalite should be handled with care. While it isn’t highly toxic to touch, you should avoid inhaling dust from the mineral, as selenium can be harmful in high concentrations.


The “A-Group” Final Roundup

Now that we’ve covered five distinct “A” minerals, you can see how diverse the mineral kingdom really is:

Mineral Color Key Element Claim to Fame
Abernathyite Yellow Uranium The glowing radioactive crystal.
Abriachanite Blue Iron The “Loch Ness Blue” pigment.
Abukumalite Brown Yttrium The tech-metal workhorse.
Acanthite Black Silver The “soft” silver you can cut with a knife.
Achávalite Grey/Black Selenium The ultra-rare Argentine native.

Acanthite: The Shifting Shape of Pure Silver

If you’ve ever looked at a piece of heirloom silverware and noticed a dark, stubborn tarnish, you’ve already encountered Acanthite. While it might look like mere “dirt” to the untrained eye, to a geologist or a silver miner, this mineral is one of the most precious substances on Earth.

Acanthite is the primary ore of silver, and it possesses a “Jekyll and Hyde” personality that baffled scientists for decades.


The Mineral That Changes Its Mind

Acanthite is silver sulfide ($Ag_2S$). What makes it fascinating is its polymorphism—the ability to exist in different crystal structures depending on the temperature.

  • Argentite (The High-Temperature Form): Above $173°C$ ($343°F$), silver sulfide organizes itself into a neat, cubic (isometric) structure called Argentite.

  • Acanthite (The Low-Temperature Form): As soon as the temperature drops below that $173°C$ threshold, the atoms “slip” into a less symmetrical, monoclinic structure.

The “Fake” Cubes

Because of this shift, most “Argentite” specimens in museums are actually pseudomorphs. They have the outward shape of a cube (from their high-temperature birth), but their internal atomic structure has quietly shifted to Acanthite as they cooled.


Physical Characteristics

Acanthite is easy to overlook if you aren’t looking for its metallic “lead-grey” to “iron-black” luster.

  • Sectility: This is its coolest party trick. Acanthite is sectile, meaning you can actually cut it with a knife like lead or cold wax, rather than it shattering like most minerals.

  • Color: Deep charcoal to black.

  • Hardness: 2.0 to 2.5 on the Mohs scale (very soft).

  • Streak: A shiny, lead-grey streak when rubbed on porcelain.


From the Comstock Lode to Your Kitchen

Acanthite isn’t just a collector’s item; it has shaped the economy of entire nations.

1. The Silver King

It was the main mineral found in the Comstock Lode in Nevada during the 1850s. This deposit was so incredibly rich in silver that the U.S. government opened a branch of the Mint in nearby Carson City just to turn the local Acanthite into coins.

2. The Science of Tarnish

Ever wonder why silver tarnishes? When your sterling silver jewelry reacts with trace amounts of sulfur in the air, it creates a microscopic layer of Acanthite. You are essentially growing a silver ore deposit on your favorite necklace!


Famous Localities

If you are looking for world-class specimens, these are the legendary spots:

  • Jáchymov, Czech Republic: The type locality where it was first described in 1855.

  • Guanajuato, Mexico: Known for producing incredibly sharp, lustrous “argentite” pseudomorphs.

  • Imiter Mine, Morocco: Currently the source of some of the finest, most aesthetic silver-and-acanthite combinations in the world.

  • Fukushima, Japan: (Returning to the Abukuma region) where it is often found alongside other rare-earth minerals.


Handling and Care

Acanthite is relatively stable, but like all silver, it can lose its luster over decades if exposed to high levels of humidity or pollutants. To keep a specimen looking “fresh” and metallic, collectors often keep them in airtight containers.


The “A-Group” Quick Reference

Mineral Color Chemistry Fun Fact
Abernathyite Yellow Uranium Glows under UV light
Abriachanite Blue Iron/Magnesium Used as a historic blue paint
Abukumalite Brown Yttrium A “metamict” radioactive glass
Acanthite Black Silver You can cut it with a knife