Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Cryobostryxite

A valid IMA mineral species
This page is currently not sponsored. Click here to sponsor this page.
Hide all sections | Show all sections

About CryobostryxiteHide

Formula:
KZnCl3 · 2H2O
Colour:
Colorless
Lustre:
Vitreous
Hardness:
2
Specific Gravity:
2.30
Crystal System:
Monoclinic
Name:
The mineral name is based on two Greek words, κρύος, cold or ice, and βóστρυξ, curl, reflecting the typical appearance: visually, anthodites of the mineral are very similar to ice curls.
Chemically related to flinteite and mellizinkalite (both anhydrous).

In the structure there are isolated Zn-centered ZnCl3(H2O) tetrahedra connected with KCl7(H2O) polyhedra to constitute a framework. Water in the above polyhedra contains O(1) atoms only. H2O(2) molecules reside within holes of the above pseudo-framework.


Unique IdentifiersHide

Mindat ID:
46440
Long-form identifier:
mindat:1:1:46440:8
GUID
(UUID V4):
17e0b95f-7d19-415e-bc5b-9bd13a93452d

Classification of CryobostryxiteHide

Approved
Approval year:
2014
First published:
2015
3.BA.20

3 : HALIDES
B : Simple halides, with H2O
A : M:X = 1:1 and 2:3

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference
CbxIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of CryobostryxiteHide

Vitreous
Transparency:
Transparent
Colour:
Colorless
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
None Observed
Parting:
None obeserved.
Fracture:
Irregular/Uneven
Density:
2.30(2) g/cm3 (Measured)    2.300 g/cm3 (Calculated)

Optical Data of CryobostryxiteHide

Type:
Biaxial (+)
RI values:
nα = 1.522(2) nβ = 1.530(2) nγ = 1.576(3)
2V:
Measured: 30° (15), Calculated: 46°
Max Birefringence:
δ = 0.054
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Surface Relief:
Low
Dispersion:
None.
Optical Extinction:
Plane of optical axes is (010); Z ∧ c = 26°.
Pleochroism:
Non-pleochroic

Chemical Properties of CryobostryxiteHide

Formula:
KZnCl3 · 2H2O
Common Impurities:
Tl

Crystallography of CryobostryxiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Setting:
P21/c
Cell Parameters:
a = 6.2795(3) Å, b = 10.1397(3) Å, c = 12.0829(7) Å
β = 107.732(5)°, γ = 107.732(5)°
Ratio:
a:b:c = 0.619 : 1 : 1.192
Unit Cell V:
732.79 ų
Z:
4

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
7.62 Å(30)
5.986 Å(43)
5.766 Å(35)
3.907 Å(33)
3.466 Å(20)
3.062 Å(100)
2.996 Å(24)
2.853 Å(27)
Comments:
Northern fumarole field, First scoria cone, Tolbachik Volcanic field, Russia. Data from the type description.

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45b : [Other oxidized fumarolic minerals]

Type Occurrence of CryobostryxiteHide

General Appearance of Type Material:
Anthodites (up to 0.5 × 2 mm), their aggregates (up to 4 × 5 mm), granular crusts (up to 2 × 2 mm) and, rarely, coarse prismatic to acicular crystals (up to 0.2 × 1 mm).
Place of Conservation of Type Material:
Type material is deposited in the collections of the Fersman Mineralogical Museum of the Russian Academy of Sciences, Moscow, Russia, registration number 4576/1.
Geological Setting of Type Material:
Secondary mineral formed in the upper, moderately hot (30–80 °C) zone of active fumaroles, probably as a product of the interactions between high-temperature volcanic sublimates and meteoric water. Formed on the surface of basalt scoria.
Associated Minerals at Type Locality:

Synonyms of CryobostryxiteHide

Common AssociatesHide

Associated Minerals Based on Photo Data:
1 photo of Cryobostryxite associated with HaliteNaCl

Related Minerals - Strunz-mindat GroupingHide

3.BA.05HydrohaliteNaCl · 2H2OMon. 2/m : P21/b
3.BA.10CarnalliteKMgCl3 · 6H2OOrth. mmm (2/m 2/m 2/m) : Pnna
3.BA.15Novograblenovite(NH4)MgCl3 · 6H2OMon. 2/m : B2/b

Other InformationHide

IR Spectrum:
O–H stretching (3200–3600 cm-1) and H–O–H bending (1607 cm-1), vibrations of H2O molecules as a whole (508 cm-1). A band at 3590 cm-1 and a doublet 3533 + 3520 cm-1 conform with weak hydrogen bonds formed by the atoms H3 and H4. Bands at 3372 and 3210 cm-1 conform with strong hydrogen bonds formed by the atoms H1 and H2. Weak bands in the range 600–1200 cm-1 correspond to overtones and combination modes. Absorptions corresponding to B–O, C–O, N–O and N–H bonds are absent.
Notes:
Readily dissolves in H2O at room temperature.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

References for CryobostryxiteHide

Reference List:
Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
Süsse, P., Brehler, B. (1964). Die Kristallstruktur des KZnCl3·2H2O. Beiträge zur Mineralogie und Petrographie, 10, 132–140. (synthetic)
Pekov, I.V., Zubkova, N.V., Britvin, S.N., Yapaskurt, V.O., Chukanov, N.V., Lykova, I.S., Sidorov, E.G. and Pushcharovsky, D.Y. (2014) Cryobostryxite, IMA 2014-058. CNMNC Newsletter No. 22, October 2014, page 1247. Mineralogical Magazine, 78, 1241-1248.
Pekov, I.V., Zubkova, N.V., Britvin, S.N., Yapaskurt, V.O., Chukanov, N.V., Lykova, I.S., Sidorov, E.G., Pushcharovsky, D.Y. (2015): New zinc and potassium chlorides from fumaroles of the Tolbachik volcano, Kamchatka, Russia: mineral data and crystal chemistry. III. Cryobostryxite, KZnCl3·2H2O. European Journal of Mineralogy: 27(6): 805-812.

Internet Links for CryobostryxiteHide

Localities for CryobostryxiteHide

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.

Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Russia (TL)
 
  • Kamchatka Krai
    • Milkovsky District
      • Tolbachik Volcanic field
        • Great Fissure eruption (Main Fracture)
          • Northern Breakthrough (North Breach)
            • First scoria cone
Pekov, I.V., Zubkova, N.V., Britvin, S.N., Yapaskurt, V.O., Chukanov, N.V., Lykova, I.S., Sidorov, E.G. and Pushcharovsky, D.Y. (2014) Cryobostryxite, IMA 2014-058. CNMNC Newsletter No. 22, October 2014, page 1247; Mineralogical Magazine, 78, 1241-1248.
 
Mineral and/or Locality  
Mindat Discussions Facebook Logo Instagram Logo Discord Logo
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 26, 2024 22:04:07 Page updated: June 25, 2023 11:37:33
Go to top of page