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Downeyite

A valid IMA mineral species
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About DowneyiteHide

Formula:
SeO2
Colour:
Colourless (red - included selenium, yellow - included sulfur)
Lustre:
Adamantine
Specific Gravity:
4.146 (Calculated)
Crystal System:
Tetragonal
Name:
For Wayne F. Downey, Jr. (Harrisburg, Pennsylvania, USA), who discovered the mineral. He was a high school student at the time and devised a way to collect the extremely hygroscopic mineral.
Naturally occuring selenium(IV) oxide, extremely hygroscopic.


Unique IdentifiersHide

Mindat ID:
1315
Long-form identifier:
mindat:1:1:1315:0

IMA Classification of DowneyiteHide

Classification of DowneyiteHide

4.DE.05

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
D : Metal: Oxygen = 1:2 and similar
E : With medium-sized cations; with various polyhedra
4.4.3.1

4 : SIMPLE OXIDES
4 : AX2
7.17.1

7 : Oxides and Hydroxides
17 : Oxides of Se and Te

Mineral SymbolsHide

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

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

Physical Properties of DowneyiteHide

Adamantine
Transparency:
Transparent
Colour:
Colourless (red - included selenium, yellow - included sulfur)
Streak:
White
Density:
4.146 g/cm3 (Calculated)

Optical Data of DowneyiteHide

Type:
Uniaxial (+)
Optical Extinction:
Parallel
Comments:
Indices of refraction are > 1.80

Chemistry of DowneyiteHide

Mindat Formula:
SeO2
Element Weights:
Element% weight
Se71.162 %
O28.839 %

Calculated from ideal end-member formula.

Crystallography of DowneyiteHide

Crystal System:
Tetragonal
Class (H-M):
4/mmm (4/m 2/m 2/m) - Ditetragonal Dipyramidal
Space Group:
P42/mbc
Setting:
P42/mbc
Cell Parameters:
a = 8.36 Å, c = 5.06 Å
Ratio:
a:c = 1 : 0.605
Unit Cell V:
353.64 ų (Calculated from Unit Cell)
Z:
8
Morphology:
Acicular crystals to 2 cm.
Twinning:
Contact twinning

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0011027DowneyiteStahl K, Legros J P, Galy J (1992) The crystal structure of SeO2 at 139 and 286 K Zeitschrift fur Kristallographie 202 99-1071992synthetic0139
0011028DowneyiteStahl K, Legros J P, Galy J (1992) The crystal structure of SeO2 at 139 and 286 K Zeitschrift fur Kristallographie 202 99-1071992synthetic0286
0017909DowneyiteMcCullough J (1937) The Crystal Structure of Selenium Dioxide _cod_database_code 1010994 Journal of the American Chemical Society 59 789-79419370293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.008 Å(100)
3.742 Å(60)
4.180 Å(55)
3.227 Å(55)
2.531 Å(25)
1.933 Å(18)
1.883 Å(14)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45a : [Sulfates, arsenates, selenates, antimonates]
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
50 : Coal and/or oil shale minerals<0.36
Stage 10b: Anthropogenic minerals<10 Ka
54 : Coal and other mine fire minerals (see also #51 and #56)
Geological Setting:
Burning coal banks.

Type Occurrence of DowneyiteHide

General Appearance of Type Material:
Acicular to prismatic crystals
Place of Conservation of Type Material:
National Museum of Natural History (Smithsonian), Washington, D.C, USA
Geological Setting of Type Material:
Burning anthracite culm banks
Associated Minerals at Type Locality:

Synonyms of DowneyiteHide

Other Language Names for DowneyiteHide

Dutch:Downeyiet
German:Downeyit
Spanish:Downeyita

Related Minerals - Strunz-mindat GroupingHide

4.DE.ColchesteriteBi3+2Mo6+2O9Mon. 2/m
4.DE.PertolditeGeO2Trig. 3 2
4.DE.ZiroiteZrO2Tet. 4/mmm (4/m 2/m 2/m) : P42/nmc
4.DE.10Koragoite(Mn2+,Fe3+)3(Nb,Ta,Ti)2(Nb,Mn)2(W,Ta)2O20Mon. 2 : P21
4.DE.15RusselliteBi2WO6Orth. mm2 : Pca21
4.DE.15KoechliniteBi2MoO6Orth. mm2 : Pna21
4.DE.15TungstibiteSb3+2WO6Orth. 2 2 2
4.DE.20TelluriteTeO2Orth. mmm (2/m 2/m 2/m) : Pbca
4.DE.25ParatelluriteTeO2Tet. 4 2 2
4.DE.30BismutotantaliteBiTaO4Orth.
4.DE.30StibiotantaliteSb(Ta,Nb)O4Orth. mm2
4.DE.30CervantiteSb3+Sb5+O4Orth. mm2
4.DE.30BismutocolumbiteBi(Nb,Ta)O4Orth. mmm (2/m 2/m 2/m)
4.DE.30StibiocolumbiteSb(Nb,Ta)O4Orth. mm2
4.DE.30ClinocervantiteSb3+Sb5+O4Mon. 2/m : B2/b
4.DE.35BaddeleyiteZrO2Mon. 2/m : P21/b
4.DE.40BillwiseiteSb3+5Nb3WO18Mon. 2/m : B2/m
4.DE.45KyawthuiteBi3+Sb5+O4Mon. 2/m

Fluorescence of DowneyiteHide

Other InformationHide

Notes:
Extremely hygroscopic. In air will deliquesce in a few minutes and be absorbed into substrate or evaporate leaving colorless film. Readily soluble in cold H2O, mineral acids, and acetone.
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 DowneyiteHide

References for DowneyiteHide

Localities for DowneyiteHide

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.
Italy
 
  • Campania
    • Metropolitan City of Naples
Russo et al. (2004)
USA
 
  • Pennsylvania
    • Northumberland County
Lapham et al. (1980)
    • Schuylkill County
Finkelman et al. (1977)
 
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