Admontite
A valid IMA mineral species
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About Admontite
Formula:
MgB6O10 · 7H2O
Colour:
Colourless
Lustre:
Vitreous
Hardness:
2 - 3
Specific Gravity:
1.82
Crystal System:
Monoclinic
Name:
Named after its discovery locality, at Schildmauer near Admont, Austria.
This page provides mineralogical data about Admontite.
Unique Identifiers
Mindat ID:
27
Long-form identifier:
mindat:1:1:27:3
IMA Classification of Admontite
Approved
IMA Formula:
MgB6O10·7H2O
Approval year:
1978
First published:
1979
Classification of Admontite
6.FA.15
6 : BORATES
F : Hexaborates
A : Neso-hexaborates
6 : BORATES
F : Hexaborates
A : Neso-hexaborates
26.6.3.1
26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
6 : Hexaborates
26 : HYDRATED BORATES CONTAINING HYDROXYL OR HALOGEN
6 : Hexaborates
9.2.13
9 : Borates
2 : Borates of Be and Mg
9 : Borates
2 : Borates of Be and Mg
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Amt | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Admontite
Vitreous
Transparency:
Transparent, Translucent
Colour:
Colourless
Streak:
White
Hardness:
2 - 3 on Mohs scale
Cleavage:
None Observed
Fracture:
Conchoidal
Density:
1.82 g/cm3 (Measured) 1.831 g/cm3 (Calculated)
Optical Data of Admontite
Type:
Biaxial (-)
RI values:
nα = 1.442 nβ = 1.500 nγ = 1.504
Max. Birefringence:
δ = 0.062
Based on recorded range of RI values above.
Based on recorded range of RI values above.
Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Surface Relief:
Moderate (negative)
Relative to Canada balsam mounting medium (n ≈ 1.537).
Relative to Canada balsam mounting medium (n ≈ 1.537).
This shows the grain boundary and Becke line effect under plane-polarised
light, based on the contrast between this mineral's average refractive
index and the mounting medium. It does not take into account mineral
colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure
- the conoscopic view for a grain cut perpendicular to the acute bisectrix, using
this mineral's 2V. The two small white dots mark the melatopes - the points
where the two optic axes emerge - and are shown only when they fall within the
field of view. The coloured bands are isochromatics, and the dark bands are
isogyres.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
No measured or calculated 2V is on file for this mineral, so the value used here (29°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
No measured or calculated 2V is on file for this mineral, so the value used here (29°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Dispersion:
not observed
Chemistry of Admontite
Mindat Formula:
MgB6O10 · 7H2O
Element Weights:
Elements listed:
Crystallography of Admontite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/c
Setting:
P21/c
Cell Parameters:
a = 12.68(2) Å, b = 10.07(2) Å, c = 11.32(2) Å
β = 109.68(10)°
β = 109.68(10)°
Ratio:
a:b:c = 1.259 : 1 : 1.124
Unit Cell V:
1,360.99 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Crystals are poorly developed or corroded, to about 1 mm, elongated along [001], flattened parallel to {100}.
Crystal Structure
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Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
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Labels
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0012333 | Admontite | dal Negro A, Ungaretti L, Basso R (1976) The crystal structure of synthetic hydrated borates: (II) MgO*3B2O3*7H2O Crystal Structure Communications 5 433-436 | 1976 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 7.60 Å | (10vb) |
| 12.08 Å | (9) |
| 2.68 Å | (9) |
| 3.93 Å | (8) |
| 5.29 Å | (7) |
| 3.09 Å | (6) |
| 5.72 Å | (4) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Near-surface Processes | |
| 25 : Evaporites (prebiotic) |
Type Occurrence of Admontite
General Appearance of Type Material:
poorly developed or corroded crystals to ca. 1 mm; [001] elongation, {100} flattening
Place of Conservation of Type Material:
n.d.
Geological Setting of Type Material:
In a gypsum deposit.
Associated Minerals at Type Locality:
Synonyms of Admontite
Other Language Names for Admontite
Related Minerals - Strunz-mindat Grouping
| 6.FA.05 | Aksaite | Mg[B6O7(OH)6] · 2H2O |
| 6.FA.10 | Mcallisterite | Mg2[B6O7(OH)6]2 · 9H2O |
| 6.FA.20 | Rivadavite | Na6Mg[B6O7(OH)6]4 · 10H2O |
| 6.FA.25 | Teruggite | Ca4Mg[AsO4]2[B6O7(OH)6]2 · 12H2O |
Other Information
Notes:
Slowly decomposed in H2O.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for Admontite
mindat.org URL:
https://www.mindat.org/min-27.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Admontite
Reference List:
Localities for Admontite
Showing 1 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
Austria (TL) | |
| Walenta (1979) +2 other references |
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symbol to view information about a locality.
The
Schildmauer quarry, Kematen, Admont, Liezen District, Styria, Austria