Abhurite

Last updated
Abhurite
Abhurite - Shipwreck Hydra, South coast of Norway.jpg
Brownish tabular crystals of abhurite from Shipwreck "Hydra", South coast of Norway
General
CategoryHalide mineral
Formula
(repeating unit)
Sn21O6(OH)14Cl16
IMA symbol Abh [1]
Strunz classification 3.DA.30
Crystal system Trigonal
Crystal class Trapezohedral (32)
H-M symbol: (32)
Space group R3 2
Unit cell a = 10.0175 Å, c = 44.014 Å; Z=3
Identification
ColorColorless/Pale yellow-greenish
Crystal habit Platy, thin crystals, cryptocrystalline crusts
Twinning On 0001
Cleavage None
Fracture Hackly
Tenacity Fragile
Mohs scale hardness2
Streak White
Diaphaneity Transparent
Specific gravity 4.42
Density 4.42 g/cm3 (Measured) 4.417 g/cm3 (Calculated)
Optical propertiesUniaxial (+)
Refractive index nω = 2.060 nε = 2.110
Birefringence δ = 0.050
Other characteristicsopalescent
References [2] [3] [4]

Abhurite is a mineral of tin, oxygen, hydrogen, and chlorine with the formula Sn21O6(OH)14Cl16 [4] [2] or Sn3O(OH)2Cl2. [5] It is named after its type locality, a shipwreck with tin ingots at Sharm Abhur, a cove near Jeddah in the Red Sea. Abhurite forms alongside other tin minerals like romarchite and cassiterite. [6] Abhurite can vary in color, from pale green/yellow to darker brown/green [7]

Contents

Locality and formation

Abhurite is attributed for forming on tin materials when in contact with sea water. The mineral was described in 1977 from a shipwreck near Hidra Island, Norway, where it occurred on pewter plates. However, that report was not recognized by the International Mineralogical Association. [2] Along with Sharm Abhur and the shipwreck near Hidra Island, abhurite was found on tin ingots in the Uluburun shipwreck. On the ingots, it was found with other tin minerals like cassiterite and romarchite, and calcium carbonate minerals like calcite and aragonite. [8]

See also

Related Research Articles

<span class="mw-page-title-main">Tourmaline</span> Cyclosilicate mineral group

Tourmaline is a crystalline silicate mineral group in which boron is compounded with elements such as aluminium, iron, magnesium, sodium, lithium, or potassium. This gemstone comes in a wide variety of colors.

<span class="mw-page-title-main">Cassiterite</span> Tin oxide mineral

Cassiterite is a tin oxide mineral, SnO2. It is generally opaque, but it is translucent in thin crystals. Its luster and multiple crystal faces produce a desirable gem. Cassiterite was the chief tin ore throughout ancient history and remains the most important source of tin today.

<span class="mw-page-title-main">Zinnwaldite</span>

Zinnwaldite, KLiFeAl(AlSi3)O10(OH,F)2, potassium lithium iron aluminium silicate hydroxide fluoride is a silicate mineral in the mica group. The IMA status is as a series between siderophyllite (KFe2Al(Al2Si2)O10(F,OH)2) and polylithionite (KLi2AlSi4O10(F,OH)2) and not considered a valid mineral species.

<span class="mw-page-title-main">Chlorite group</span> Type of mineral

The chlorites are the group of phyllosilicate minerals common in low-grade metamorphic rocks and in altered igneous rocks. Greenschist, formed by metamorphism of basalt or other low-silica volcanic rock, typically contains significant amounts of chlorite.

<span class="mw-page-title-main">Bismuthinite</span> Bismuth (III) sulfide mineral

Bismuthinite is a mineral consisting of bismuth sulfide (Bi2S3). It is an important ore for bismuth. The crystals are steel-grey to off-white with a metallic luster. It is soft enough to be scratched with a fingernail and rather dense.

<span class="mw-page-title-main">Stannite</span>

Stannite is a mineral, a sulfide of copper, iron, and tin, in the category of thiostannates.

<span class="mw-page-title-main">Elbaite</span> Cyclosilicate, mineral

Elbaite, a sodium, lithium, aluminium boro-silicate, with the chemical composition Na(Li1.5Al1.5)Al6Si6O18(BO3)3(OH)4, is a mineral species belonging to the six-member ring cyclosilicate tourmaline group.

<span class="mw-page-title-main">Sperrylite</span>

Sperrylite is a platinum arsenide mineral with the chemical formula PtAs2 and is an opaque metallic tin white mineral which crystallizes in the isometric system with the pyrite group structure. It forms cubic, octahedral or pyritohedral crystals in addition to massive and reniform habits. It has a Mohs hardness of 6–7 and a very high specific gravity of 10.6.

<span class="mw-page-title-main">Polycrase</span>

Polycrase or polycrase-(Y) is a black or brown metallic complex uranium yttrium oxide mineral with the chemical formula (Y,Ca,Ce,U,Th)(Ti,Nb,Ta)2O6. It is amorphous. It has a Mohs hardness of 5 to 6 and a specific gravity of 5. It is radioactive due to its uranium content. It occurs in granitic pegmatites.

<span class="mw-page-title-main">Akaganeite</span> Iron(III) oxide-hydroxide mineral

Akaganeite, also written as the deprecated Akaganéite, is a chloride-containing iron(III) oxide-hydroxide mineral, formed by the weathering of pyrrhotite (Fe1−xS).

<span class="mw-page-title-main">Native metal</span> Form of metal

A native metal is any metal that is found pure in its metallic form in nature. Metals that can be found as native deposits singly or in alloys include antimony, arsenic, bismuth, cadmium, chromium, cobalt, indium, iron, manganese, molybdenum, nickel, niobium, rhenium, tantalum, tellurium, tin, titanium, tungsten, vanadium, and zinc, as well as the gold group and the platinum group. Among the alloys found in native state have been brass, bronze, pewter, German silver, osmiridium, electrum, white gold, silver-mercury amalgam, and gold-mercury amalgam.

<span class="mw-page-title-main">Aheylite</span>

Aheylite is a rare phosphate mineral with formula (Fe2+Zn)Al6[(OH)4|(PO4)2]2·4(H2O). It occurs as pale blue to pale green triclinic crystal masses. Aheylite was made the newest member of the turquoise group in 1984 by International Mineralogical Association Commission on New Minerals and Mineral Names.

<span class="mw-page-title-main">Augelite</span> Aluminium phosphate mineral

Augelite is an aluminium phosphate mineral with formula: Al2(PO4)(OH)3. The shade varies from colorless to white, yellow or rose. Its crystal system is monoclinic.

<span class="mw-page-title-main">Russellite (mineral)</span> Bismuth tungstate mineral

Russellite is a bismuth tungstate mineral with the chemical formula Bi2WO6. It crystallizes in the orthorhombic crystal system. Russellite is yellow or yellow-green in color, with a Mohs hardness of 3+12.

<span class="mw-page-title-main">Danalite</span> Iron beryllium silicate sulfide mineral

Danalite is an iron beryllium silicate sulfide mineral with formula: Fe2+4Be3(SiO4)3S.

<span class="mw-page-title-main">Plumbogummite</span> Alunite supergroup, phosphate mineral

Plumbogummite is a rare secondary lead phosphate mineral, belonging to the alunite supergroup of minerals, crandallite subgroup. Some other members of this subgroup are:

<span class="mw-page-title-main">Ixiolite</span>

Ixiolite is an accessory oxide mineral found in granitic pegmatites. It is an oxide with the general chemical formula (Ta,Nb,Sn,Mn,Fe)4O8 or (Ta,Mn,Nb)O2.

<span class="mw-page-title-main">Ferronigerite-2N1S</span>

Ferronigerite-2N1S is an iron, tin, alumino-hydroxide mineral that naturally occurs around sillimanite-quartz veins. Ferronigerite-2N1S belongs to the nigerite group, högbomite supergroup. The other constituents of the nigerite group are ferronigerite-6N6S, magnesionigerite-2N1S, magnesionigerite-6N6S, zinconigerite-2N1S and zinconigerite-6N6S. The 2N1S ending stands for the nolanite and spinel structural layers.

Chatkalite is a copper, iron, tin sulfide mineral with formula Cu6Fe2+Sn2S8. It crystallizes in the tetragonal crystal system and forms as rounded disseminations within tetrahedrite in quartz veins.

<span class="mw-page-title-main">Tacharanite</span> Calcium aluminium silicate hydrate mineral

Tacharanite is a calcium aluminium silicate hydrate (C-A-S-H) mineral of general chemical formula Ca12Al2Si18O33(OH)36 with some resemblance to the calcium silicate hydrate (C-S-H) mineral tobermorite. It is often found in mineral assemblage with zeolites and other hydrated calcium silicates.

References

  1. 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.
  2. 1 2 3 Mindat.org – Abhurite
  3. Webmineral.org – Abhurite
  4. 1 2 "Handbook of Mineralogy – Abhurite" (PDF). Archived from the original (PDF) on 2015-09-24. Retrieved 2013-01-26.
  5. Richard V. Gaines, H. Catherine W. Skinner, Eugene E. Foord, Brian Mason, and Abraham Rosenzweig: "Dana's new mineralogy", p. 401. John Wiley & Sons, 1997
  6. Memet, J. B. (2007). "The corrosion of metallic artefacts in seawater: descriptive analysis". In Dillmann, P.; Beranger, G.; Piccardo, P.; Matthiessen, H. (eds.). Corrosion of Metallic Heritage Artefacts: Investigation, Conservation and Prediction of Long Term Behaviour. Elsevier. pp. 152–169. doi:10.1533/9781845693015.152. ISBN   9781845693015.
  7. https://www.mindat.org/photoscroll.php?frm_id=pscroll&cform_is_valid=1&searchbox=Abhurite&submit_pscroll=Search
  8. Vandiver, Pamela B.; Goodway, Martha; Mass, Jennifer L. (2002-01-01). Materials Issues in Art and Archaeology VI: Symposium Held November 26–30, 2001, Boston, Massachusetts, U.S.A. Materials Research Society. ISBN   9781558996489.