Hannebachite
A valid IMA mineral species
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About Hannebachite
Formula:
CaSO3 · H2O
Colour:
Colourless, white
Lustre:
Vitreous
Hardness:
3½
Specific Gravity:
2.52
Crystal System:
Orthorhombic
Name:
Named for the type locality.
This page provides mineralogical data about Hannebachite.
Unique Identifiers
Mindat ID:
1997
Long-form identifier:
mindat:1:1:1997:8
IMA Classification of Hannebachite
Classification of Hannebachite
4.JE.10
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
E : Sulfites
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
E : Sulfites
Dana 7th ed.:
34.2.4.1
34.2.5.1
34 : SELENITES, TELLURITES AND SULFITES
2 : A(XO3)·xH2O
34 : SELENITES, TELLURITES AND SULFITES
2 : A(XO3)·xH2O
27.1.1
27 : Sulphites, Chromates, Molybdates and Tungstates
1 : Sulphites
27 : Sulphites, Chromates, Molybdates and Tungstates
1 : Sulphites
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 |
|---|---|---|
| Hbc | 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 Hannebachite
Vitreous
Transparency:
Transparent
Colour:
Colourless, white
Streak:
White
Hardness:
3½ on Mohs scale
Cleavage:
Perfect
{110}
{110}
Density:
2.52 g/cm3 (Measured) 2.54 g/cm3 (Calculated)
Optical Data of Hannebachite
Type:
Biaxial (+)
RI values:
nα = 1.596 nβ = 1.6 nγ = 1.634
2V:
Measured: 38° , Calculated: 40°
Max. Birefringence:
δ = 0.038
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:
High (positive)
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.
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.
Dispersion:
r < v weak
Optical Extinction:
Parallel. X = a; Y = c; Z = b.
Chemistry of Hannebachite
Mindat Formula:
CaSO3 · H2O
Element Weights:
Elements listed:
Crystallography of Hannebachite
Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 6.473(5) Å, b = 9.782(9) Å, c = 10.646(9) Å
Ratio:
a:b:c = 0.662 : 1 : 1.088
Unit Cell V:
674.09 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Crystals elongate [010], flattened on {001} and modified by {l01} and {021}.
Comment:
Non-standard space-group setting Pbna.
Crystal Structure
Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Show
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Display Options
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
View
CIF File Best | x | y | z | a | b | c
CIF File Best | x | y | z | a | b | c
Rotation
Stop | Start
Stop | Start
Labels
Console Off | On | Grey | Yellow
Console Off | On | Grey | Yellow
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) |
|---|---|---|---|---|---|---|---|
| 0015778 | Hannebachite | Schropfer L (1973) Strukturelle untersuchungen an CaSO3*1/2H2O Zeitschrift fur Anorganische und Allgemeine Chemie 401 1-14 | 1973 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 5.54 Å | (40) |
| 3.79 Å | (80) |
| 3.15 Å | (100) |
| 2.617 Å | (90) |
| 1.950 Å | (40) |
| 1.843 Å | (50) |
| 1.671 Å | (40) |
Comments:
Hannebacher Ley, Germany. The data are from the type description.
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 45a : [Sulfates, arsenates, selenates, antimonates] | |
| Stage 10b: Anthropogenic minerals | <10 Ka |
| 56 : Slag and smelter minerals (see also #51 and #55) |
Type Occurrence of Hannebachite
General Appearance of Type Material:
Crystals up to q mm long, elongate on [010] and flattened {001}.
Place of Conservation of Type Material:
Naturhistorisches Museum Mainz, Mainz, Germany, numbers M1990/3093 (holotype/cotype).
Geological Setting of Type Material:
In cavities in melilite-nepheline-leucite lava at a Quarternary volcano. Thought to be a primary mineral.
Associated Minerals at Type Locality:
Synonyms of Hannebachite
Other Language Names for Hannebachite
Common Associates
Associations Based on Photo Data:
| 4 photos of Hannebachite associated with Native Sulphur | S8 |
| 3 photos of Hannebachite associated with Phillipsite-K | K6(Si10Al6)O32 · 12H2O |
| 2 photos of Hannebachite associated with Dolomite | CaMg(CO3)2 |
| 2 photos of Hannebachite associated with Metacinnabar | HgS |
| 1 photo of Hannebachite associated with Gypsum | CaSO4 · 2H2O |
| 1 photo of Hannebachite associated with Phillipsite Subgroup | (Ca0.5,K,Na,Ba0.5)4-7[Al4-7Si12-9O32] . 12H2O |
Related Minerals - Strunz-mindat Grouping
| 4.JE.X | Albertiniite | Fe2+(SO3) · 3H2O |
| 4.JE. | Mikenewite | Mn2+(S4+O3) · 3H2O |
| 4.JE. | Vanpeltite | (Mo2O5)(S4+O3) · 4H2O |
| 4.JE.05 | Fleisstalite | FeSO3 · 3H2O |
| 4.JE.05 | Gravegliaite | Mn2+SO3 · 3H2O |
| 4.JE.15 | Orschallite | Ca3(SO3)2(SO4) · 12H2O |
| 4.JE.20 | Scotlandite | PbSO3 |
| 4.JE.25 | Kollerite | (NH4)2Fe3+(SO3)2(OH) · H2O |
Other Information
IR Spectrum:
IR absorption bands at 980, 940, and 650 cm-1 that are characteristic for SO3.
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 Hannebachite
mindat.org URL:
https://www.mindat.org/min-1997.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Hannebachite
Localities for Hannebachite
Showing 14 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 | |
| Program and Abstracts Volume +2 other references |
| Postl et al. (2005) +1 other reference |
Canada | |
| Greengrass et al. (1999) |
France | |
| Ł. Kruszewski EPMA/PXRD/Rietveld data +1 other reference |
Germany | |
| Weiß (1990) |
| Blaß et al. (1995) |
| Hentschel et al. (1985) |
| Hentschel (1987) +1 other reference |
| Hentschel (1993) |
| Witzke et al. (1998) |
Hungary | |
| collector: Gábor Koller |
Poland | |
| Lukasz Kruszewski 2005: Minerals arising in cause of underground fires of "Skalny" coal mine dump in Laziska (unpublished) |
Russia | |
| Ershov et al. (1987) +1 other reference |
Spain | |
| Sainz de Baranda Graf et al. (2024) |
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The
Hannebacher Ley, Hannebach, Spessart, Brohltal, Ahrweiler, Rhineland-Palatinate, Germany