| Tetradymite | |
|---|---|
 Tetradymite - British Columbia, Canada | |
| General | |
| Category | Sulfide mineral |
| Formula (repeating unit) | Bi2Te2S |
| IMA symbol | Ttd[1] |
| Strunz classification | 2.DC.05c |
| Dana classification | 02.11.07.01 |
| Crystal system | Trigonal |
| Crystal class | Hexagonal scalenohedral (3m) H-M symbol: (3 2/m) |
| Space group | R3m |
| Identification | |
| Color | Steel-gray with dull to iridescent tarnish; white in polished section |
| Crystal habit | Pyramidal prisms, commonly granular, massive to foliated, also bladed |
| Twinning | Twin planes {0118} and {0115} |
| Cleavage | Perfect on {0001} |
| Fracture | Uneven |
| Tenacity | Laminae flexible, slightly sectile. |
| Mohs scale hardness | 1.5 – 2 |
| Luster | Metallic, splendent on fresh surfaces, dull if tarnished |
| Streak | Steel-gray |
| Diaphaneity | Opaque |
| Specific gravity | 7.2 – 7.9 |
| References | [2][3][4][5] |
Tetradymite is a mineral consisting of bismuth, tellurium and sulfide, Bi2Te2S, also known as telluric bismuth. If sulfur is absent the mineral is tellurobismuthite and the formula is then Bi2Te3. Traces of selenium are usually present.[6]
Crystals are rhombohedral, but are rarely distinctly developed; they are twinned together in groups of four; hence the name of the mineral, from the Greek for fourfold. There is a perfect cleavage parallel to the basal plane and the mineral usually occurs in foliated masses of irregular outline. The color is steel-gray, and the luster metallic and brilliant. The mineral is very soft (H = 1.5 – 2) and marks paper. The specific gravity is 7.2 to 7.9.[6]
The type locality is Zupkov (Zsubko; Schubkau), Stredoslovenský Kraj, Slovak Republic where it was reported in 1831.[5] It was first found, in 1815, at Telemark in Norway.[6] It often occurs in high temperature hydrothermal quartz veins associated with native gold and in contact metamorphic deposits.[3]
References
[edit]- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ Mineralienatlas
- ^ a b http://rruff.geo.arizona.edu/doclib/hom/tetradymite.pdf Handbook of Mineralogy
- ^ http://webmineral.com/data/Tetradymite.shtml Webmineral data
- ^ a b http://www.mindat.org/min-3921.html Mindat.org
- ^ a b c Spencer 1911.
Attribution:
External links
[edit]This article incorporates text from a publication now in the public domain: Spencer, Leonard James (1911). "Tetradymite". In Chisholm, Hugh (ed.). Encyclopædia Britannica. Vol. 26 (11th ed.). Cambridge University Press. p. 670.
| Authority control databases: National |
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Well, that’s interesting to know that Psilotum nudum are known as whisk ferns. Psilotum nudum is the commoner species of the two. While the P. flaccidum is a rare species and is found in the tropical islands. Both the species are usually epiphytic in habit and grow upon tree ferns. These species may also be terrestrial and grow in humus or in the crevices of the rocks.
View the detailed Guide of Psilotum nudum: Detailed Study Of Psilotum Nudum (Whisk Fern), Classification, Anatomy, Reproduction