Tag: Radioactive Minerals

Abukumalite: The Yttrium Star of the Japanese Highlands

While the previous minerals we’ve discussed have been neon-yellow or deep-sea blue, Abukumalite brings us into the realm of the “Earth Tones”—a mineral that looks like the soil but holds the secrets of rare-earth elements.

If you look for “Abukumalite” in a modern textbook, you might find it listed under a different name: Britholite-(Y). However, the story of its discovery in the mountains of Japan remains a classic piece of mineralogical history.

What is Abukumalite?

Abukumalite is a rare-earth silicate mineral belonging to the Apatite supergroup. It was first discovered in 1938 in the Suishoyama pegmatite, located in the Abukuma Range of the Fukushima Prefecture, Japan.

In 1966, mineralogists decided to standardize the names of rare-earth minerals. Because Abukumalite was chemically similar to Britholite but dominated by the element Yttrium, it was officially renamed Britholite-(Y). Despite the name change, seasoned collectors still use the old name to honor its Japanese heritage.

Quick Facts:

  • Chemical Formula: $(Y, Ca)_5(SiO_4, PO_4)_3(OH, F)$

  • Color: Reddish-brown, dark brown, or black.

  • Hardness: 5 on the Mohs scale (similar to a pocket knife blade).

  • Luster: Resinous to greasy (it can look a bit like hardened tree sap).

The “Metamict” State: A Mineral in Chaos

One of the most scientifically fascinating things about Abukumalite is that it is often metamict.

Because Abukumalite frequently contains trace amounts of radioactive elements like Thorium or Uranium, it undergoes a process called “self-irradiation.” Over millions of years, the radiation emitted from within the crystal actually breaks down its own internal structure.

The result? The mineral looks like a crystal on the outside, but on the inside, the atoms are in a state of chaotic disorder, more like glass than a structured crystal.

Where Does it Come From?

Abukumalite is typically found in granite pegmatites—massive, slow-cooled volcanic rocks that allow rare and “exotic” elements to concentrate into large crystals.

  1. Japan (Type Locality): The Abukuma massif remains the most famous source, specifically the Suishoyama pegmatite.

  2. Norway: Found in the high-alkaline rocks of the Drag area.

  3. Russia: Notable specimens have been found in the Kola Peninsula, a “Mecca” for rare-earth mineral hunters.

Why Is It Important?

Abukumalite isn’t just a curiosity for the shelf. It is a vital source of Yttrium and other Rare Earth Elements (REEs).

Yttrium is a “tech-metal” used in:

  • LEDs and Phosphors: Creating the red color in older television screens and modern LED bulbs.

  • Superconductors: Vital for high-tech energy and transport research.

  • Camera Lenses: Adding yttrium oxide to glass makes it heat-resistant and shock-resistant.

Safety and Identification

Like many rare-earth minerals from pegmatites, Abukumalite can be mildly radioactive. While it’s not as “hot” as pure uranium minerals, it’s best to keep it in a display case rather than carrying it in your pocket.

Visually, it can be hard to distinguish from other brown minerals like Allanite. The key is often its association—if you find a resinous brown mineral in a pegmatite known for yttrium, you might just be looking at Abukumalite.

The “A-Group” Mineral Summary

Mineral Color Key Element Claim to Fame
Abernathyite Yellow Uranium Neon fluorescence
Abriachanite Blue Iron The “Blue Earth” of Loch Ness
Abukumalite Brown Yttrium The tech-metal workhorse

Abernathyite: The Rare Yellow Treasure of the Uranium World

If you aren’t a dedicated mineral collector or a radiochemistry enthusiast, the name Abernathyite might sound like a fictional stone from a superhero movie. However, this rare secondary mineral is very real, strikingly beautiful, and carries a fascinating story that links 1950s geology with the complex world of uranium chemistry.

What is Abernathyite?

Abernathyite is a rare potassium uranyl arsenate hydrate mineral. It was first discovered in 1953 in the Fuemrol Mine in Emery County, Utah. Named after Jesse E. Abernathy, the mine operator who first found the specimens, it belongs to the autunite group—a family of minerals famous for their bright colors and radioactive properties.

Quick Facts:

  • Chemical Formula: $K(UO_2)(AsO_4) \cdot 3H_2O$

  • Color: Distinctive yellow to neon green.

  • Luster: Vitreous (glassy) to pearly.

  • Hardness: 2.5 on the Mohs scale (about the same as a fingernail).

  • Crystal System: Tetragonal.

Appearance and Characteristics

One of the most striking things about Abernathyite is its visual appeal. It typically forms in small, transparent, platy crystals. While it may look delicate, its chemical makeup is quite specific.

The Glow Factor

Like many uranium-bearing minerals, Abernathyite is fluorescent. Under ultraviolet (UV) light, it emits a moderate to strong yellow-green glow. This is a characteristic of the uranyl ion ($UO_2^{2+}$) present in its structure.

Radioactivity

Because it contains uranium, Abernathyite is radioactive. While a small thumbnail specimen in a plastic container isn’t a major health hazard, it requires careful handling. Collectors usually store it in “perky boxes” to prevent the inhalation of any radioactive dust or radon gas buildup.

Where is it Found?

Abernathyite isn’t something you’ll find in your backyard. It is a secondary mineral, meaning it forms when primary uranium ores (like uraninite) are weathered or oxidized by groundwater.

  • Utah, USA: The “type locality” remains the Fuemrol Mine.

  • France: Notable specimens have been found in the Lodève District.

  • Germany: Found in the Black Forest region.

  • South Africa: Small deposits have been identified in the Northern Cape.

Why Should You Care?

You might wonder why scientists and collectors get excited about a tiny yellow crystal. Abernathyite is a “chemical cousin” to more common minerals like Autunite (calcium-based) and Metazeunerite (copper-based).

By studying how Abernathyite forms, geologists can understand how uranium and arsenic move through the earth’s crust. This is vital for environmental science, particularly in managing old mining sites and protecting groundwater from contamination.

Handling and Safety

If you are lucky enough to see a specimen in person, remember the three rules of radioactive minerals:

  1. Time: Limit the time you spend holding it.

  2. Distance: Keep it away from your living spaces.

  3. Shielding: Store it in a dedicated mineral case.

  4. Hygiene: Always wash your hands after handling any unsealed specimen.

Abernathyite is a perfect example of the hidden beauty found in the world of radioactive mineralogy—a mix of bright, neon colors and complex chemical history.