A sourced material profile

Charoite: purple ornamental rock and the structure within a mineral

Charoite is a mineral found within mixed ornamental rock. Dated accounts, studies of its structure and tests on specific samples keep its purple story precise.

Independent educational writing. Sources were reviewed for this edition; the notes below distinguish documented evidence from interpretation.

79CharoiteCharoite: purple ornamental rock and the structure within a mineralCharoite is a mineral species within mixed ornamental rock; dated descriptions, structural studies and measured sample scopes keep the purple story precise.

This educational reading uses dated examples. Mineral properties, mixed rocks and tested research samples each have their own scope. It does not authenticate a supplied object, an untreated state, origin, value or therapeutic benefit.

Mohs hardness
Not determined
Cleavage
Good in three directions

A mineral name inside an ornamental material

The revised Handbook describes charoite as fibrous or massive and deep lilac to violet. It is a mineral with a complex silicate composition that contains calcium and alkalis. This names the mineral. It does not fully describe every purple object sold under that name. Ask whether a polished piece is labelled for one mineral within it or for the whole material. Describe its visible pattern separately from any mineral analysis. You can enjoy a complex surface without assuming that every vein or coloured area has been tested. Even a beautiful name needs a clear account of what the piece is.

Evidence: Charoite — Handbook of Mineralogy

The rock has room for other minerals

Dutrow and Henry’s 2015 conference abstract distinguishes the mineral charoite from the rock charoitite. They describe folded charoite fibres in mats that contain or enclose other minerals. These include feldspar, aegirine, tinaksite and quartz. Some rock they studied contains up to 90% charoite. The other minerals are not, just because they are there, flaws or signs of an imitation. A result for one mineral does not give the composition of a whole carving. Nor is that upper percentage a standard purity grade for ornaments. A useful description names the charoite-bearing rock and states which minerals were identified. If there is only a trade label, leave the full list open. Do not name coloured patches by eye.

Evidence: Charoite, charoitites and associated minerals: the products of intense metasomatic activity

Read the contact, not only the map point

The Handbook records metasomatised syenite–limestone contacts in Russia’s Murun massif. It links the name to the Chara River. The 2015 abstract describes metasomatism caused by fluids linked to igneous activity. This account concerns rock and fluid interactions in a stated setting. It tells us more than a country name, but does not prove the origin of a supplied cabochon. A modern label needs a collecting and trading record to link that object to an occurrence. A scientific name tells us how the mineral is classed. The river link does not prove a first human encounter or a discovery legend. No current extraction rights, operating mine or unbroken collecting chain is claimed here.

Evidence: Charoite, charoitites and associated minerals: the products of intense metasomatic activity, Charoite — Handbook of Mineralogy

1978 is a publication date to preserve

Sofia’s National Museum of Natural History lists the original 1978 description by Rogova, Rogov, Drits and Kuznetsova. It appeared in volume 107, pages 94–100, of the Soviet mineralogical society journal. The translated title introduces a new mineral and jewellery stone. The museum bibliography was readable, but the linked Russian original was not accessible in this review. We can describe that publication without claiming to have examined its detailed wording. Do not replace this gap with a tale of a traveller finding the first purple rock. A species description, an earlier collecting event and first human use are separate claims. The dated list of sources marks when science recognised the mineral. It does not supply an invented witness or journey.

Evidence: Publication 0275: Rogova, Rogov, Drits and Kuznetsova (1978)

Seeing further than the polished surface

Rozhdestvenskaya and colleagues’ February 2010 article abstract reports how charoite’s structure was solved. The work used electron diffraction, imaging and spectroscopy. It describes several silicate-chain arrangements, with ions and water molecules in channels. Cambridge’s July 2018 online date is later than the original journal issue. A structural drawing shows the inside of a studied crystal. It is not an enlarged view of the swirls on an ornamental rock. Check the scale and method before linking those images. The publisher abstract supports this outline; the full article was not examined here. Keeping both dates avoids mistaking a hosting update for a new discovery. Research into the structure continued after naming. What science knew did not arrive complete in one moment.

Evidence: The structure of charoite solved by conventional and automated electron diffraction

A spectrum belongs to a recorded acquisition

Raman Open Database entry 1000064 names charoite and links the 2010 structure paper. Its measurement fields give a 780 nm excitation wavelength, 4 cm−1 resolution, an unoriented measurement and a 1 μm spot. These details describe how an instrument was used. They do not make the database card an analysis of an owned object. No spectral file was independently interpreted for this profile. No peak-matching shortcut is offered. When reading a gem report, ask what was sampled and how it was measured. You can describe how a whole polished rock looks. An instrument tests a smaller question under stated conditions. Keep both scopes clear, rather than using a spectrum as decoration.

Evidence: Raman Open Database: information card 1000064

Purple appearance and a qualified explanation

A 2017 IUCrJ study of denisovite compares it with charoite and discusses colours caused by impurities in charoite. The authors distinguish the two structures despite their similarities. Dutrow and Henry suggest that manganese in their charoite samples is probably responsible for the purple colour. Keep the word “Probably”: it marks an interpretation. These statements concern particular tests and comparisons. They do not promise the same cause of colour in every mixed rock used for ornaments. A violet area and a contrasting inclusion may need separate descriptions. Ask which mineral was analysed and which proposed cause the report supports. Similarity between minerals is a research question. It does not permit their names to be exchanged on a label.

Evidence: Charoite, charoitites and associated minerals: the products of intense metasomatic activity, The structure of denisovite — comparative charoite discussion

One selected crystal, two measurements

Lacalamita’s 2018 study tested one light-violet crystal chosen from Murun material. It used micro-infrared spectroscopy and electron-probe analysis. Spectra before and after four hours at 100°C showed no significant change in the relevant water/OH absorption. The author interpreted differences in water bands using the charoite-90 structure model. The choice of sample matters as much as the instruments. The result concerns that crystal and those tests. It is not an operating temperature for jewellery. It does not show that a whole carving has the same structure. Even when a test finds no change, its scope still has limits. Read what was sought, what was measured and which comparison supported the interpretation before calling a result universal.

Evidence: Micro-FTIR and EPMA Characterisation of Charoite from Murun Massif (Russia)

A changed colour may accompany a changed phase

Ionov and colleagues’ 2024 institutional abstract describes controlled tests at high temperatures. Charoite changed towards wollastonite-related phases. Floating-zone melting produced pseudowollastonite and changed lilac to rose pink. The look can thus change while the substance itself changes too. This was an experimental transformation, not a routine jewellery treatment or the growth of new charoite crystals. The linked full text was unavailable. Further conditions and interpretations are not supplied here. The reviewed sources did not document a supply of laboratory-grown ornamental charoite. That is a research gap, not proof that synthesis is impossible. A seller’s origin or treatment claim still needs evidence and a precise material name.

Evidence: Experimental studies of charoite mineral transformations under thermal treatment

Leave an undetermined number undetermined

The 2020 revised Handbook marks Mohs hardness as not determined. It records good cleavage in three directions. This profile does not fill the gap with a range from an unverified commercial table. A missing value with a clear source is more useful than a number added merely to complete a card. For care, keep the material description, treatment record and condition of the whole object. Ask an appropriate professional before cleaning or repair. Do not copy a laboratory heating experiment or try a household test. The reviewed evidence gives no general permission for steam, ultrasonic, chemical or heat cleaning.

Evidence: Charoite — Handbook of Mineralogy

Reading exercise: move between three scales

The linked sources cover rock composition, crystal structure and measurement conditions. Choose the rock abstract, structure abstract and Raman information card. Make three headings: whole rock, studied crystal and recorded measurement. Under each, note what the source describes, the supporting method or record, and one unanswered question. Write a short caption for an imagined original diagram linking the headings. Use arrows labelled “contains” or “measured from” only where the record supports them. A decorative swirl is not an atomic channel. This original exercise helps you read about a whole rock and the much smaller parts within it. It needs no specimen, magnification, heating, grinding or interpretation of spectra.

Evidence: Charoite, charoitites and associated minerals: the products of intense metasomatic activity, Raman Open Database: information card 1000064, The structure of charoite solved by conventional and automated electron diffraction

Sources & reading

  1. Micro-FTIR and EPMA Characterisation of Charoite from Murun Massif (Russia)Maria Lacalamita; Journal of Spectroscopy · 2026-10-05

    Single selected crystal; heating result not a jewel-cleaning protocol.

  2. Charoite, charoitites and associated minerals: the products of intense metasomatic activityDutrow and Henry; Geological Society of America · 2026-10-05

    Conference summary; proposed colour mechanism remains qualified.

  3. Charoite — Handbook of MineralogyMineralogical Society of America · 2026-10-05

    Revised entry; Mohs hardness not determined; optical numerical table unused.

  4. The structure of denisovite — comparative charoite discussionRozhdestvenskaya et al.; IUCrJ · 2026-10-05

    Denisovite main study; only explicit charoite comparisons used.

  5. Publication 0275: Rogova, Rogov, Drits and Kuznetsova (1978)National Museum of Natural History, Sofia · 2026-10-05

    Evidence of published description, not first human encounter.

  6. Raman Open Database: information card 1000064Raman Open Database / original data authors · 2026-10-05

    No spectrum file independently analysed; card not a specimen authentication.

  7. The structure of charoite solved by conventional and automated electron diffractionRozhdestvenskaya et al.; Mineralogical Magazine · 2026-10-05

    2010 issue distinct from 2018 online hosting date; structural claims abstract-scoped.

  8. Experimental studies of charoite mineral transformations under thermal treatmentIonov et al.; HSE University / Physics and Chemistry of Minerals · 2026-10-05

    Controlled high-temperature experiment; neither commercial treatment prevalence nor synthetic charoite demonstrated.

Editorial method, responsibility and corrections

Purple fibrous swirling rock texture with dark inclusions and pale yellow areas
Close view of charoitite, identified by photographer James St. John as a charoite-dominated rock from Siberia. Purple fibrous swirls occur alongside other components; this is not a claim of a pure single-mineral specimen. James St. John · CC BY 2.0 · Photo record. Flickr-published non-square large JPEG derivative; no project crop, recolouring, retouching, reencoding or enlargement.
Responsive WebP copy · full frame retained

Responsive display copies: proportionally downsampled and encoded as WebP by Goutte de Rosée; full frame retained, with no crop, retouching, recolouring or enlargement. Display orientation follows the original EXIF; any colour profile and attribution metadata are retained. The original-file description above remains applicable to the preserved original.

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