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Clinoferrosilite
A valid IMA mineral species - grandfathered
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About Clinoferrosilite
Formula:
Fe2+2Si2O6
Simplified: FeSiO3.
Colour:
Brown, colourless, green
Hardness:
5 - 6
Specific Gravity:
4.068 (Calculated)
Crystal System:
Monoclinic
Member of:
Name:
Named for being the monoclinic polymorph of ferrosilite.
Type Locality:
Polymorph of:
Isostructural with:
Pyroxene Group - Clinopyroxene Subgroup
Note: in some previous texts the name ferrosilite was used for what is now called clinoferrosilite, whereas the equivalent orthorhombic dimorph was called orthoferrosilite, so be careful when reading older texts.
Note: in some previous texts the name ferrosilite was used for what is now called clinoferrosilite, whereas the equivalent orthorhombic dimorph was called orthoferrosilite, so be careful when reading older texts.
Unique Identifiers
Mindat ID:
1073
Long-form identifier:
mindat:1:1:1073:9
Classification of Clinoferrosilite

Clinoferrosilite and its relation to other pyroxenes

Previous petrological nomenclature of clinopyroxenes from basaltic magmas, note described here as 'ferrosilite' (after Poldervaart & Hess, 1951)
IMA Classification of Clinoferrosilite
Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Fe2+SiO3
9.DA.10
9 : SILICATES (Germanates)
D : Inosilicates
A : Inosilicates with 2-periodic single chains, Si2O6; pyroxene family
9 : SILICATES (Germanates)
D : Inosilicates
A : Inosilicates with 2-periodic single chains, Si2O6; pyroxene family
65.1.1.2
65 : INOSILICATES Single-Width,Unbranched Chains,(W=1)
1 : Single-Width Unbranched Chains, W=1 with chains P=2
65 : INOSILICATES Single-Width,Unbranched Chains,(W=1)
1 : Single-Width Unbranched Chains, W=1 with chains P=2
14.21.4
14 : Silicates not Containing Aluminum
21 : Silicates of Fe and Mg
14 : Silicates not Containing Aluminum
21 : Silicates of Fe and Mg
Mineral Symbols
As of 2021 there are now IMAâCNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Please only use the official IMAâCNMNC symbol. Older variants are listed for historical use only.
Please only use the official IMAâCNMNC symbol. Older variants are listed for historical use only.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Cfs | IMAâCNMNC | Warr, L.N. (2021). IMAâCNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
| Cfs | Kretz (1983) | Kretz, R. (1983) Symbols of rock-forming minerals. American Mineralogist, 68, 277â279. |
| Cfs | Siivolam & Schmid (2007) | Siivolam, J. and Schmid, R. (2007) Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: List of mineral abbreviations. Web-version 01.02.07. IUGS Commission on the Systematics in Petrology. download |
| Cfs | Whitney & Evans (2010) | Whitney, D.L. and Evans, B.W. (2010) Abbreviations for names of rock-forming minerals. American Mineralogist, 95, 185â187 doi:10.2138/am.2010.3371 |
Pronunciation of Clinoferrosilite
Pronunciation:
| Play | Recorded by | Country |
|---|---|---|
| Jolyon Ralph | United Kingdom |
Physical Properties of Clinoferrosilite
Transparency:
Transparent, Translucent
Colour:
Brown, colourless, green
Streak:
White
Hardness:
5 - 6 on Mohs scale
Cleavage:
Distinct/Good
Density:
4.068 g/cm3 (Calculated)
Optical Data of Clinoferrosilite
Type:
Biaxial (+)
RI values:
nα = 1.764 nβ = 1.767 nγ = 1.792
2V:
Measured: 25° , Calculated: 40°
Max. Birefringence:
δ = 0.028
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 ”m 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 ”m 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:
Very 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:
very strong
Optical Extinction:
Z ⧠c = 31°.
Chemistry of Clinoferrosilite
Mindat Formula:
Fe2+2Si2O6
Simplified: FeSiO3.
Simplified: FeSiO3.
Element Weights:
Elements listed:
Crystallography of Clinoferrosilite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/c
Setting:
P21/c
Cell Parameters:
a = 9.7085 Å, b = 9.0872 Å, c = 5.2284 Å
β = 108.432°
β = 108.432°
Ratio:
a:b:c = 1.068 : 1 : 0.575
Unit Cell V:
437.60 Ă
Âł (Calculated from Unit Cell)
Z:
4
Comment:
Synthetic sample (pure Fe2Si2O6). Mg-bearing sample has 9.53, 9.21, 5.15 â«, 107.63°.
Crystal Structure
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Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
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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) |
|---|---|---|---|---|---|---|---|
| 0001681 | Clinoferrosilite | Hugh-Jones D A, Woodland A B, Angel R J (1994) The structure of high-pressure C2/c ferrosilite and crystal chemistry of high-pressure C2/c pyroxenes American Mineralogist 79 1032-1041 | ![]() | 1994 | 0 | 293 | |
| 0001679 | Clinoferrosilite | Hugh-Jones D A, Woodland A B, Angel R J (1994) The structure of high-pressure C2/c ferrosilite and crystal chemistry of high-pressure C2/c pyroxenes American Mineralogist 79 1032-1041 | ![]() | 1994 | 0 | 293 | |
| 0000460 | Clinoferrosilite | Ohashi Y, Burnham C W, Finger L W (1975) The effect of Ca-Fe substitution on the clinopyroxene crystal structure Fs85Wo15 American Mineralogist 60 423-434 | ![]() | 1975 | 0 | 293 | |
| 0000459 | Clinoferrosilite | Ohashi Y, Burnham C W, Finger L W (1975) The effect of Ca-Fe substitution on the clinopyroxene crystal structure Fs80Wo20 American Mineralogist 60 423-434 | ![]() | 1975 | 0 | 293 | |
| 0000936 | Clinoferrosilite | Sueno S, Kimata M, Prewitt C T (1984) The crystal structure of high clinoferrosilicate American Mineralogist 69 264-269 | ![]() | 1984 | 0 | 1323 | |
| 0001680 | Clinoferrosilite | Hugh-Jones D A, Woodland A B, Angel R J (1994) The structure of high-pressure C2/c ferrosilite and crystal chemistry of high-pressure C2/c pyroxenes American Mineralogist 79 1032-1041 | ![]() | 1994 | 1.87 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 3.035 Ă | (100) |
| 2.603 Ă | (63) |
| 2.909 Ă | (55) |
| 2.408 Ă | (53) |
| 2.161 Ă | (51) |
| 4.605 Ă | (49) |
| 3.234 Ă | (40) |
Comments:
Synthetic.
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 4a: Earthâs earliest continental crust | >4.4-3.0 |
| 20 : Acidic volcanic rocks |
Type Occurrence of Clinoferrosilite
General Appearance of Type Material:
Needles about 0.05 x 0.005 mm in size.
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, number 102793.
Geological Setting of Type Material:
Lithophysae of obsidian.
Other Language Names for Clinoferrosilite
Dutch:Clinoferrosiliet
Japanese:ćæéçȘèŒçł
Russian:ĐĐ»ĐžĐœĐŸŃĐ”ŃŃĐŸŃОлОŃ
Simplified Chinese:æéèŸçł
Spanish:Clinoferrosilita
Relationship of Clinoferrosilite to other Species
Member of:
Other Members of Clinopyroxene Subgroup:
| Aegirine | NaFe3+Si2O6 | Mon. 2/m : B2/b |
| Aegirine-augite | (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6 | Mon. 2/m : B2/b |
| Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 | Mon. 2/m : B2/b |
| Burnettite | CaVAlSiO6 | Mon. 2/m : B2/b |
| Clinoenstatite | MgSiO3 | Mon. 2/m : P21/c |
| Colomeraite | NaTi3+Si2O6 | Mon. 2/m : B2/b |
| Davisite | CaScAlSiO6 | Mon. 2/m : B2/b |
| Diopside | CaMgSi2O6 | Mon. 2/m : B2/b |
| Esseneite | CaFe3+[AlSiO6] | Mon. 2/m : B2/b |
| Grossmanite | CaTi3+ AlSiO6 | Mon. 2/m : B2/b |
| Hedenbergite | CaFe2+Si2O6 | Mon. 2/m : B2/b |
| Jadeite | Na(Al,Fe3+)Si2O6 | Mon. 2/m : B2/b |
| Jervisite | NaSc3+Si2O6 | Mon. 2/m : B2/b |
| Johannsenite | CaMn2+Si2O6 | Mon. 2/m : B2/b |
| Kanoite | Mn2+MgSi2O6 | Mon. 2/m : P21/c |
| Kosmochlor | NaCrSi2O6 | Mon. 2/m : B2/b |
| Kushiroite | CaAlAlSiO6 | Mon. 2/m : B2/b |
| Namansilite | NaMn3+Si2O6 | Mon. 2/m : B2/b |
| Natalyite | NaV3+Si2O6 | Mon. 2/m : B2/b |
| Omphacite | (NaaCabFe2+cMgd)(AleFe3+fFe2+gMgh)Si2O6 | Mon. 2/m |
| Petedunnite | CaZnSi2O6 | Mon. 2/m : B2/b |
| Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 | Mon. 2/m : P21/c |
| Ryabchikovite | CuMgSi2O6 | Mon. 2/m : P21/c |
| Spodumene | LiAlSi2O6 | Mon. 2/m : B2/b |
| Tissintite | (Ca,â»)AlSi2O6 | Mon. 2/m : B2/b |
| 'UM2003-36-SiO:CaNa' | NaCrSi2O6 - CaMgSi2O6 | Mon. 2/m : B2/b |
Common Associates
Associations Based on Photo Data:
| 8 photos of Clinoferrosilite associated with 'Amethyst' | SiO2 |
| 5 photos of Clinoferrosilite associated with Sanidine | K(AlSi3O8) |
| 2 photos of Clinoferrosilite associated with Quartz | SiO2 |
| 1 photo of Clinoferrosilite associated with Diopside | CaMgSi2O6 |
| 1 photo of Clinoferrosilite associated with Hemleyite | Fe2+SiO3 |
| 1 photo of Clinoferrosilite associated with Clinoenstatite | MgSiO3 |
| 1 photo of Clinoferrosilite associated with 'Fayalite-Forsterite Series' | |
| 1 photo of Clinoferrosilite associated with 'Maskelynite' | |
| 1 photo of Clinoferrosilite associated with Taenite | (Ni,Fe) |
Related Minerals - Strunz-mindat Grouping
| 9.DA. | Colomeraite | NaTi3+Si2O6 |
| 9.DA. | Protoenstatite | Mg2Si2O6 |
| 9.DA. | Ryabchikovite | CuMgSi2O6 |
| 9.DA.05 | Donpeacorite | Mn2+MgSi2O6 |
| 9.DA.05 | Enstatite | Mg2Si2O6 |
| 9.DA.05 | Ferrosilite | Fe2+2Si2O6 |
| 9.DA.10 | Clinoenstatite | MgSiO3 |
| 9.DA.10 | Kanoite | Mn2+MgSi2O6 |
| 9.DA.10 | Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| 9.DA.15 | Grossmanite | CaTi3+ AlSiO6 |
| 9.DA.15 | Diopside | CaMgSi2O6 |
| 9.DA.15 va | 'Jeffersonite' | Ca(Mn,Zn,Fe)Si2O6 |
| 9.DA.15 | Hedenbergite | CaFe2+Si2O6 |
| 9.DA.15 | Johannsenite | CaMn2+Si2O6 |
| 9.DA.15 | Petedunnite | CaZnSi2O6 |
| 9.DA.15 | Esseneite | CaFe3+[AlSiO6] |
| 9.DA.15 | Kushiroite | CaAlAlSiO6 |
| 9.DA.15 | Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| 9.DA.15 | Davisite | CaScAlSiO6 |
| 9.DA.20 | Aegirine-augite | (NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6 |
| 9.DA.20 | Omphacite | (NaaCabFe2+cMgd)(AleFe3+fFe2+gMgh)Si2O6 |
| 9.DA.25 | Jadeite | Na(Al,Fe3+)Si2O6 |
| 9.DA.25 | Namansilite | NaMn3+Si2O6 |
| 9.DA.25 | Natalyite | NaV3+Si2O6 |
| 9.DA.25 | Aegirine | NaFe3+Si2O6 |
| 9.DA.25 | Jervisite | NaSc3+Si2O6 |
| 9.DA.25 | Tissintite | (Ca,â»)AlSi2O6 |
| 9.DA.25 | Kosmochlor | NaCrSi2O6 |
| 9.DA.30 | Spodumene | LiAlSi2O6 |
| 9.DA.35 | Hiroseite | FeSiO3 |
Other Information
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 Clinoferrosilite
mindat.org URL:
https://www.mindat.org/min-1073.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Clinoferrosilite
Reference List:
Poldervaart, A., Hess, H. H. (1951) Pyroxenes in the Crystallization of Basaltic Magma. The Journal of Geology, 59 (5) 472-489 doi:10.1086/625891
Sueno, Shigeho, Kimata, Mitsuyoshi, Prewitt, Charles T. (1984) The crystal structure of high clinoferrosilite. American Mineralogist, 69 (3-4) 264-269
Localities for Clinoferrosilite
Showing 29 localities.
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
â - 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.
Australia | |
| Birch (1999) |
Brazil | |
| Jour. of South American Earth Sci. ... |
China | |
| Dongyang Zhang et al. (2010) |
Eurasian Plate | |
| Lu et al. (2026) |
Finland | |
| Kallio et al. (2021) +1 other reference |
Germany | |
| BlaĂ et al. (1995) |
| BlaĂ et al. (2003) |
| BlaĂ et al. (2009) |
India | |
| Bhattacharjee et al. (2012) |
Italy | |
| Marzio Mamberti find & collection |
Japan | |
| Matsueda (1980) |
Kenya | |
| Rocky Mountain (53rd) |
| Bowen N L (1935) |
Mongolia | |
| Savina et al. (2020) |
| Peretyazhko et al. (2018) |
| Peretyazhko et al. (2017) | |
Russia | |
| Safina et al. (2015) |
| Sharygin et al. (2010) |
| |
| [World of Stones 12:49] | |
South Africa | |
| Cairncross et al. (1995) |
| Excalibur Minerals photo ID 140072 |
| Fosso-Kankeu et al. (2015, November) |
Tajikistan | |
| Sharygin et al. (2009) |
USA | |
| ... |
| Bowen (1935) +2 other references |
| Bowen (1935) +2 other references | |
| Gunnar FĂ€rber - Mineralienliste 3-2017. |
| Amer.J.Sci. (1935) |
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Sant'Antioco, South Sardinia Province, Sardinia, Italy