Ba(UO2)2(AsO4)2·8H2O
a vivid green warmth that feeds the heart with life, worked at a distance
The name carries two layers of meaning. The prefix meta- comes from the Greek for "after" or "beyond" and in mineralogy denotes a dehydrated form of a hydrated mineral — metaheinrichite is precisely that: a lower-hydrate phase that forms when the parent mineral heinrichite loses some of its water. The second element, heinrichite, honours Eberhardt William Heinrich (1918–1991), an American mineralogist and professor at the University of Michigan who first characterised and described the mineral in 1958 from specimens found in Oregon. The naming thus records both the structural transformation the crystal undergoes and the person who brought it to scientific attention.
Metaheinrichite is a hydrated barium uranyl arsenate built on the layered sheet architecture common to the autunite group. Flat uranyl arsenate sheets — UO₂²⁺ units linked by arsenate tetrahedra — are interleaved with barium ions and structural water molecules in a monoclinic (sphenoidal, space group P 2₁) framework. The mineral carries eight water molecules per formula unit. This is a reduced water content compared to its parent species, heinrichite, which holds ten to twelve water molecules. The transformation is straightforward: as heinrichite loses water — whether through gentle warming, dry-air storage, or simply the passage of time — it converts to metaheinrichite. This dehydration relationship places metaheinrichite firmly as an alteration product of heinrichite, and the same process can, in reverse humid conditions, partially re-hydrate the structure. The barium, uranium, and arsenic chemistry gives the mineral its vivid yellowish-green colour, its very low hardness of 2.5 on the Mohs scale, and its dual hazard of radioactivity and toxicity.
Metaheinrichite was first described in 1958 by E. W. Heinrich from specimens collected at the White King mine, located approximately 22 kilometres northwest of Lakeview in Lake County, Oregon, USA. The White King mine was a uranium-mining operation active during the mid-twentieth century and became the type locality for several rare uranium minerals. As a secondary mineral, metaheinrichite forms in the oxidised zones of uranium deposits where barium-bearing groundwaters interact with primary uranium ores and arsenate-rich fluids. Its occurrence is rare and typically localised to such chemically complex uranium ore bodies. Beyond Oregon, the mineral has been documented in a small number of uranium-mining districts elsewhere in the United States and Europe, always as a minor secondary phase among assemblages of related uranyl phosphate and arsenate minerals.
This crystal contains naturally radioactive elements and emits low-level radiation. Owning radioactive minerals may be restricted where you live — some countries regulate them strictly, with legal limits as low as 1 becquerel per gram. Check your local law before acquiring or shipping one.
All radiation safety comes down to three words: time, distance, and shielding. Handle a specimen only briefly, keep it at arm's length, and store it behind glass or lead. Enjoy it visually, or for energy work at a distance — never worn as jewellery, slept beside, or held in prolonged contact.
The chief practical risk is not the dose from the shelf but radon — a heavy radioactive gas that sinks and pools in low, unventilated spaces. Keep specimens well-ventilated, or sealed in a gas-tight container; with radon's 3.8-day half-life it never builds without limit and clears within weeks. Stored sensibly, the real dose is tiny — far below what people willingly absorb at a radon spa.
How dangerous are radioactive crystals really? Usually far less than people fear — and the science of low-dose radiation is genuinely surprising. Our full guide covers safe handling and storage, how to read a dose, the truth about radon, and the radioactive beaches and century-old healing spas where people seek radiation out on purpose.
Read the full guide →Metaheinrichite contains two toxic elements: barium, a heavy metal that is harmful if ingested or inhaled as dust, and arsenic, a highly toxic metalloid that poses serious health risks through ingestion, inhalation of fine particles, or prolonged skin contact.
Do not handle with bare hands for extended periods. Never crush, grind, or abrade specimens. Do not ingest or allow near food and drink. Keep away from children and animals. Wash hands thoroughly after any contact. Store in a sealed, labelled container. No water elixirs or gem essences should ever be prepared from this mineral.
The colour of metaheinrichite — a saturated yellowish green — is produced entirely by the uranyl ion (UO₂²⁺). The uranium-oxygen bond absorbs specific wavelengths and re-radiates visible light in the yellow-green range, giving the mineral an almost luminous appearance even in ordinary light. This coloration is a hallmark of uranyl minerals and links metaheinrichite visually to the broader family of vivid green uranium-bearing phases, including autunite and torbernite.
Under both shortwave and longwave ultraviolet illumination, metaheinrichite glows with a bright green to greenish-yellow fluorescence. The uranyl chromophore is among the most efficient UV-to-visible emitters in the mineral world, and the layered autunite-group crystal structure amplifies this response. In UV displays, specimens appear to radiate from within — a property that has made uranium minerals among the most visually arresting subjects in mineralogical photography.
Unusually, metaheinrichite concentrates three elements of independent concern — uranium (radioactive), barium (toxic heavy metal), and arsenic (highly toxic metalloid) — within a single monoclinic crystal. This combination is extremely rare in nature and makes the mineral a geochemical curiosity: each element contributes a distinct hazard profile, and their co-occurrence in a layered sheet structure is a consequence of the specific oxidation chemistry of uranium ore deposits where barium-rich and arsenic-rich fluids meet.
"There is one thing that destroys anyone's ability to advance spiritually: the inability to control the mind and emotions."— Swami Rudrananda
There is something very quiet about working with this stone. You do not hold it. You do not place it on the body. You set it across the room, perhaps on a shelf, and you simply sit — and something in the chest begins to settle, the way a pool settles after a stone has been dropped in it. The mind is still chattering, but somewhere beneath the chatter there is a warmth, steady and unhurried, that seems to have always been there.
That warmth is the quality this stone carries most naturally: a slow vitality, feeding into the heart centre the way a river feeds a lake — not dramatically, but continuously, without effort on your part. The heart is the meeting place of everything, the point where the inner life touches the outer world without the mind's filter between them. Metaheinrichite works precisely there, at that junction, softening what has grown tight, restoring a sense of aliveness to the emotional centre that stress and the passage of time can quietly drain away.
"The heart is the hub of all sacred places. Go there and roam."— Bhagawan Nityananda
And so you go there. Not by doing anything, but by allowing the stone's presence — at its safe distance, never touched — to act as a gentle reminder. The heart is not broken. It is simply waiting to be noticed again. The energy radiating outward from this mineral expands that noticing, making it a little wider, a little more willing to include what was previously kept outside. This is what expansion means at the level of the heart: not a dramatic opening, but a gradual willingness to receive more of what is already here.
Working at a DistanceBecause metaheinrichite is both radioactive and toxic, all engagement with it takes place at a distance — through sight, through the photograph on this page, or through quiet energetic attunement across a room. This is not a limitation; it is simply the nature of the stone's relationship to the body. Many people find that distance work with this mineral is entirely sufficient, since the medium-depth duration of its action means it can continue quietly working for hours, settling into the chest layer by layer, without any direct physical proximity. There is something almost freeing in this: you do not have to manage the stone, hold it correctly, or prepare a space. You acknowledge it, and it does what it does.
Life-Force and the RareRarity itself carries an energetic signature. To be drawn to a stone that few people have ever held, that formed under very specific conditions in a single Oregon mine, is to have already demonstrated something — a persistence, a willingness to seek out what is genuinely uncommon rather than settle for what is simply available. This quality of havingness loops back into the energetic body and feeds the life-force dimension of the stone's action. The chest opens not only to warmth but to a quiet recognition that the unusual is possible, that what is rare can be found, and that life has more to offer than habit has taught us to expect.