Erdite (original) (raw)

A valid IMA mineral species

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About ErditeHide

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Crystal System:

Monoclinic

Name:

Named by G.K. Czamanske, B.F. Leonard, J.R. Clark in 1980 in honor of Richard Clarkson "Dick" Erd (29 February 1924, Lexington, Kentucky, USA - 20 May 2008, Springdale, Arkansas, USA), mineralogist with the US Geological Survey. He had previously synthesized the substance in 1956.

This page provides mineralogical data about Erdite.

Unique IdentifiersHide

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Long-form identifier:

mindat:1:1:1394:5

1ca24dc2-0ec0-4812-8eb8-4069a6b066f1

IMA Classification of ErditeHide

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Classification of ErditeHide

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2.FD.20

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
F : Sulfides of arsenic, alkalies; sulfides with halide, oxide, hydroxide, H2O
D : With O, OH, H2O

2.14.5.1

2 : SULFIDES
14 : Hydroxysulfides and Hydrated Sulfides

3.0.1

3 : Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1)
0 : Sulphides etc. of the alkalis

Mineral SymbolsHide

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

Symbol Source Reference
Erd IMA–CNMNC Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Pronunciation of ErditeHide

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Pronunciation:

Play Recorded by Country
Sorry, your browser doesn't support HTML5 audio. Jolyon Ralph United Kingdom

Physical Properties of ErditeHide

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Comment:

Tarnishes quickly

Hardness:

VHN15=22 - 67 kg/mm2 - Vickers

Cleavage:

Distinct/Good
{110} Good

Density:

2.30 g/cm3 (Measured) 2.216 g/cm3 (Calculated)

Comment:

Measured contaminated with magnetite

Optical Data of ErditeHide

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Reflectivity:

Wavelength R1 R2
400nm 10.2% 23.8%
420nm 9.8% 28.8%
440nm 10.1% 27.3%
460nm 10.9% 20.8%
480nm 11.3% 15.6%
500nm 11.3% 16.6%
520nm 11.0% 23.3%
540nm 10.6% 25.7%
560nm 10.3% 25.7%
580nm 10.0% 31.6%
600nm 9.8% 36.6%
620nm 9.7% 43.1%
640nm 9.8% 46.9%
660nm 10.0% 44.3%
680nm 10.6% 39.3%
700nm 11.0% 35.3%

Reflectance graph
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 46.9%.
R1 shown in black, R2 shown in red

Comments:

Extreme. Brilliant reddish-orange through greenish grays and pinkish grays to dark gray with barely perceptible bluish or greenish tint.

Chemistry of ErditeHide

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Mindat Formula:

NaFeS2 · 2H2O

Crystallography of ErditeHide

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Crystal System:

Monoclinic

Class (H-M):

2/m - Prismatic

Cell Parameters:

a = 10.693 Å, b = 9.115 Å, c = 5.507 Å
β = 92.17°

Ratio:

a:b:c = 1.173 : 1 : 0.604

Unit Cell V:

536.36 ų (Calculated from Unit Cell)

Morphology:

Minute fibers, fine bladed crystals to 1 mm long.

Crystal StructureHide

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ID Species Reference Link Year Locality Pressure (GPa) Temp (K)
0000785 Erdite Konnert J A, Evans H T (1980) The crystal structure of erdite, NaFeS2*2H2O American Mineralogist 65 516-521 1980 Coyote Peak, Humboldt County, California, USA 0 293

CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

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Powder Diffraction Data:

d-spacing Intensity
6.935 Å (100)
5.342 Å (71)
4.556 Å (41)
3.467 Å (28)
2.310 Å (23)
2.902 Å (15)
3.317 Å (12)

Comments:

Coyote Peak, California, USA.

Geological EnvironmentHide

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Geological Setting:

Pegmatites in nepheline syenite

Type Occurrence of ErditeHide

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General Appearance of Type Material:

Copper-red granular masses of impure erdite reach dimensions of several millimeters. The largest clean single crystals measure 0.5 x 1 mm.

Place of Conservation of Type Material:

National Museum of Natural History, Washington, D.C., USA.

Geological Setting of Type Material:

In mafic, alkalic diatreme. Very young rock (29 m.y.)

Associated Minerals at Type Locality:

Synonyms of ErditeHide

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Other Language Names for ErditeHide

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Common AssociatesHide

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Associated Minerals Based on Photo Data:

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2.FD. Ferrovalleriite 2(Fe,Cu)S · 1.5Fe(OH)2 Trig.
2.FD.05 Kermesite Sb2S2O Tric. 1 : _P_1
2.FD.10 Viaeneite (Fe,Pb)4S8O Mon.
2.FD.25 Coyoteite NaFe3S5 · 2H2O Tric.
2.FD.30 Haapalaite (Fe2+,Ni)2(Mg,Fe2+)1.61S2(OH)3.22 Hex.
2.FD.30 Valleriite (Fe2+,Cu)4(Mg,Al)3S4(OH,O)6 Trig.
2.FD.30 Yushkinite (Mg,Al)V4+S2(OH)2 Trig. 3_m_ _(_32/m ) : _P_3_m_1
2.FD.30 Ekplexite (Nb,Mo,W)S2 · (Mg1-xAlx)(OH)2+x Trig.
2.FD.35 Tochilinite Fe2+5-6(Mg,Fe2+)5S6(OH)10 Mon.
2.FD.35 Ferrotochilinite Fe2+6(Fe2+,Mg)5S6(OH)10 Mon.
2.FD.35 Kaskasite (Mo,Nb)S2 · (Mg1-xAlx)(OH)2+x Trig.
2.FD.35 Manganokaskasite (Mo,Nb)S2 · (Mn1-xAlx)(OH)2+x Trig.
2.FD.40 Wilhelmramsayite Cu3FeS3 · 2H2O Orth. m m m _(_2/_m_2/_m_2/m ) : P m m m
2.FD.45 Vyalsovite FeCaAlS(OH)5 Orth.
2.FD.50 Bazhenovite Ca8S2(S3)(S2O3)(OH)12 · 20H2O Mon. 2/m : _P_21/b
2.FD.55 UM2004-56-OS:BiCuPb PbCu4Bi4S2(O,OH,H2O)16 (?) Tet.

Other InformationHide

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Thermal Behaviour:

When heated in a closed tube, it gives off water, sulfur and eventually turns black and strongly magnetic.

Notes:

Easily soluble in cold dilute acids with effervescence of H2S.

Health Risks:

No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

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References for ErditeHide

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Localities for ErditeHide

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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

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- 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.

Canada
Québec Montérégie La Vallée-du-Richelieu RCM Mont Saint-Hilaire Poudrette quarry (De-Mix quarry; Demix quarry; Uni-Mix quarry; Carrière Mont Saint-Hilaire; MSH) Horváth et al. (1990) +1 other reference
Lajemmerais RCM Varennes & St-Amable Saint-Amable sill Horváth et al. (1998)
Demix-Varennes quarry Horváth et al. (1998)
Poland
Silesian Voivodeship Wodzisław County Radlin Marcel mine heap ? Cu +2 other references
Russia
Murmansk Oblast Lovozersky District Alluaiv Mountain [World of Stones 95:5-6
USA (TL)
California Humboldt County Coastal Range Coyote Peak (TL) Van Nostrand Reinholt Press: 67 +4 other references