MINERALS
Miscellaneous
- Family: None
- Region: None
- Mined At: Unspecified
- Raw Mineral: Yes
- Generic: No
Notes
(Richard Willis)
The crystallized aggregates of atomic elements, morphologically distinguishable by 32 possible geometrical shapes (symmetry elements and their combinations) which in turn can be grouped into six crystal systems according to the complexity of their symmetries: isometric, hexagonal, tetragonal, orthorhombic, monoclinic, and triclinic. The aggregates (elements combined forming a given mineral) are determined by chemical bonding, which can occur electrostatically, electron-sharing, metallicazation, or residuali
zation. Bonding effects hardness, density, solubility, melting point, tenacity, specific gravity, magnetism, structural properties, colors, etc. Subsequently, minerals can be classified into 11 groups according to chemical and physical properties: native elements, sulfides, sulfosalts, oxides and hydroxides, halides, carbonates, nitrates, borates, sulfates, phosphates, and silicates. see individual listings for further details
major native elements
metals: gold group (gold Au, silver Ag, copper Cu); platinum group (platinum Pt); iron group [(iron Fe),, (kamacite: Fe, Ni), (taenite: Fe, Ni)]
semimetals: arsenic group (arsenic As), bismuth Bi
nonmetals: sulfur S, diamond C, graphite C
Major types, with examples, used in studio ceramics:
oxides
X2O and XO types
cupric Cu2O
zincite (Zn, Mn)O
X2O3 type
corundum Al2O3
hematite group
hematite Fe203
ilmenite FeTiO3
XO2 type
rutile group
rutile TiO2
pyrolusite MnO2
cassiterite SnO2
XY2O4 type
spinel group
gahnite MgAI204
hydroxides
X(OH) type
brucite Mg(OH)2
manganite MnO(OH)
wavellite Al3(PO4)2(OH,F)3, 5H2O
carbonates
calcite group (hexagonal)
calcite CaC03
magnesite MgCO3
sidenite FeCO3
phodochrosite MnCo3
smithsonite ZnC03
monoclinic carbonates w/(OH)
malachite Cu2CO3(0H)7
azurite Cu3(CO3)2(OH)2
aragonite group
(orthorhombic)
aragonite CaCO3
witherite BaCO3
strontianite SrC0
cerussite PbCO3
dolomite group (hexagonal)
dolomite CaMg(CO3)2
ankerite CaFe(CO3)2
phosphates
apatite group
apatite Ca5(PO4)3(F,Cl,OH)
pyromorphite Pb5(PO4)3Cl
ambligonite (Li,Na)AlPO4(F,OH)
turquoise CuAl6(PO4)4(OH)8,4H2O
autunite Ca(UO2)2(PO4)2,10-12H2O
sulfides, sulfarsenides, sulfosalts, and sulfates
sulfides and sulfarsenides
chalcocite Cu2S
bornite Cu2FeS4
galena PbS
sphalerite ZnS
chalcopyrite CuFeS2
pyrrhotite Fe1-xS (x= 0-0.2)
pentlandite (Fe, Ni)9S8
covellite CuS
cinnabar HgS
realgar AsS
orpiment As2S3
stibnite Sb2S3
pyrite FeS
marcasite FeS2
molybdenite MoS
arsenopyrite FeAsS
.sulfosalts
pyrargynite Ag3SbS3
proustite Ag3AsS3
tetrahedrite (Cu, Fe)12Sb4S13
tennantite (Cu, Fe)12As4S13
enargite Cu3AsS4
bournonite PbCuSbS3
sulfates
barite group
barite BaSO4
celesite SrSO4
anglesite PbSO4
anhydrite CaSO4
gypsum CaSO4, 2H2O
halides
halite NaCl
sylvite KCl
chlorargyrite AgCl
fluorite CaF
nitrates
Seven known naturally occurring nitrates with the form XNO3, two of which are nitratite (NaNO3) and nitre (KNO3)
borates
groups: BO3, B2O5, B3O6,B2O4, [B4O5(OH)4]2
silicates
neosilicates: olivine group, garnet group, zircon group, alumina group, topaz, and staurolite
sorosilicates: epidote group, and vesurvianite group
Cyclo[ring]silicates of the forms Si3O9, Si4O12, and Si6O18 benitoite, axinite, beryl, tourmaline, etc.
Inosilicates: pyroxenes and amphiboles
phyllosilicates: serpentine group, clay minerals group, talc, mica group, chlorite group
tectosilicates: SiO2 group, feldspar group, feldspathoid group, f zeolite group
Authors
- Richard Willis (Owner)
XML
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<material name="MINERALS" descrip="" generic="0" rawmineral="1" searchkey="" loi="0.00">
<notes>
<note>The crystallized aggregates of atomic elements, morphologically distinguishable by 32 possible geometrical shapes (symmetry elements and their combinations) which in turn can be grouped into six crystal systems according to the complexity of their symmetries: isometric, hexagonal, tetragonal, orthorhombic, monoclinic, and triclinic. The aggregates (elements combined forming a given mineral) are determined by chemical bonding, which can occur electrostatically, electron-sharing, metallicazation, or residuali
zation. Bonding effects hardness, density, solubility, melting point, tenacity, specific gravity, magnetism, structural properties, colors, etc. Subsequently, minerals can be classified into 11 groups according to chemical and physical properties: native elements, sulfides, sulfosalts, oxides and hydroxides, halides, carbonates, nitrates, borates, sulfates, phosphates, and silicates. <FONT SIZE=2>see individual listings for further details</FONT><BR>
<B>major native elements<BR>
<I>metals</I></B>: gold group (gold Au, silver Ag, copper Cu); platinum group (platinum Pt); iron group [(iron Fe),, (kamacite: Fe, Ni), (taenite: Fe, Ni)]<BR>
<B><I>semimetals</I>: </B>arsenic group (arsenic As), bismuth Bi<B><I><BR>
nonmetals</I>: </B>sulfur S, diamond C, graphite C<BR>
Major types, with examples, used in studio ceramics:<BR>
<B>oxides</B><BR>
<B>X<FONT SIZE=2><SUB>2</SUB></FONT>O </B>and<B> XO </B>types<B><BR>
</B>cupric Cu<FONT SIZE=2><SUB>2</SUB></FONT>O<B><BR>
</B>zincite (Zn, Mn)O<BR>
<B>X<FONT SIZE=2><SUB>2</SUB></FONT>O<FONT SIZE=2><SUB>3</SUB></FONT></B><FONT SIZE=2></FONT> type<BR>
corundum Al<FONT SIZE=2><SUB>2</SUB></FONT>O<FONT SIZE=2><SUB>3</SUB></FONT><BR>
<B><I>hematite group<BR>
</I></B>hematite Fe<FONT SIZE=2><SUB>2</SUB></FONT>0<FONT SIZE=2><SUB>3</SUB></FONT><BR>
ilmenite FeTiO<FONT SIZE=2><SUB>3</SUB></FONT><B><BR>
XO<FONT SIZE=2><SUB>2</SUB></FONT></B><FONT SIZE=2></FONT> type<BR>
<B><I>rutile group</I><BR>
</B>rutile TiO<FONT SIZE=2><SUB>2</SUB></FONT><B><BR>
</B>pyrolusite MnO<FONT SIZE=2><SUB>2</SUB></FONT><B><BR>
</B>cassiterite SnO<FONT SIZE=2><SUB>2</SUB></FONT><B><BR>
XY<FONT SIZE=2><SUB>2</SUB></FONT>O<FONT SIZE=2><SUB>4</SUB></FONT></B><FONT SIZE=2></FONT> type<BR>
<B><I>spinel group<BR>
</I></B>gahnite MgAI<FONT SIZE=2><SUB>2</SUB></FONT>0<FONT SIZE=2><SUB>4</SUB></FONT><B><BR>
hydroxides<BR>
X(OH)</B> type<BR>
brucite Mg(OH)<FONT SIZE=2><SUB>2</SUB></FONT><B><BR>
</B>manganite MnO(OH)<BR>
wavellite Al<FONT SIZE=2><SUB>3</SUB></FONT>(PO<FONT SIZE=2><SUB>4</SUB></FONT>)<FONT SIZE=2><SUB>2</SUB></FONT>(OH,F)<FONT SIZE=2><SUB>3</SUB></FONT>, 5H<FONT SIZE=2><SUB>2</SUB></FONT>O<BR>
<B>carbonates<BR>
<I>calcite group (hexagonal)</I><BR>
</B>calcite CaC0<FONT SIZE=2><SUB>3</SUB></FONT><B><BR>
</B>magnesite MgCO<FONT SIZE=2><SUB>3</SUB></FONT><B><BR>
</B>sidenite FeCO<FONT SIZE=2><SUB>3</SUB></FONT><B><BR>
</B>phodochrosite MnCo<FONT SIZE=2><SUB>3</SUB></FONT><B><BR>
</B>smithsonite ZnC0<FONT SIZE=2><SUB>3</SUB></FONT><B><BR>
<I>monoclinic carbonates w/(OH)</I><BR>
</B>malachite Cu<FONT SIZE=2><SUB>2</SUB></FONT>CO<FONT SIZE=2><SUB>3</SUB></FONT>(0H)<FONT SIZE=2><SUB>7</SUB></FONT><B><BR>
</B>azurite Cu<FONT SIZE=2><SUB>3</SUB></FONT>(CO<FONT SIZE=2><SUB>3</SUB></FONT>)<FONT SIZE=2><SUB>2</SUB></FONT>(OH)<FONT SIZE=2><SUB>2</SUB></FONT><B><BR>
<I>aragonite group</I><BR>
<I>(orthorhombic)<BR>
</I></B>aragonite CaCO<FONT SIZE=2><SUB>3</SUB></FONT><B><I><BR>
</I></B>witherite BaCO<FONT SIZE=2><SUB>3</SUB></FONT><B><I><BR>
</I></B>strontianite SrC0<B><BR>
</B>cerussite PbCO<FONT SIZE=2><SUB>3<BR>
</SUB></FONT><B><I>dolomite group (hexagonal)</I></B><FONT SIZE=2><SUB><BR>
</SUB></FONT>dolomite CaMg(CO<FONT SIZE=2><SUB>3</SUB></FONT>)<FONT SIZE=2><SUB>2<BR>
</SUB></FONT>ankerite CaFe(CO<FONT SIZE=2><SUB>3</SUB></FONT>)<FONT SIZE=2><SUB>2<BR>
</SUB></FONT><B>phosphates<BR>
</B>apatite group<BR>
apatite Ca<FONT SIZE=2><SUB>5</SUB></FONT>(PO<FONT SIZE=2><SUB>4</SUB></FONT>)<FONT SIZE=2><SUB>3</SUB></FONT>(F,Cl,OH)<BR>
pyromorphite Pb<FONT SIZE=2><SUB>5</SUB></FONT>(PO<FONT SIZE=2><SUB>4</SUB></FONT>)<FONT SIZE=2><SUB>3</SUB></FONT>Cl<BR>
ambligonite (Li,Na)AlPO<FONT SIZE=2><SUB>4</SUB></FONT>(F,OH)<BR>
turquoise CuAl<FONT SIZE=2><SUB>6</SUB></FONT>(PO<FONT SIZE=2><SUB>4</SUB></FONT>)<FONT SIZE=2><SUB>4</SUB></FONT>(OH)<FONT SIZE=2><SUB>8</SUB></FONT>,4H<FONT SIZE=2><SUB>2</SUB></FONT>O<BR>
autunite Ca(UO<FONT SIZE=2><SUB>2</SUB></FONT>)<FONT SIZE=2><SUB>2</SUB></FONT>(PO<FONT SIZE=2><SUB>4</SUB></FONT>)<FONT SIZE=2><SUB>2</SUB></FONT>,10-12H<FONT SIZE=2><SUB>2</SUB></FONT>O<B><BR>
sulfides, sulfarsenides, sulfosalts</B>, <B>and sulfates</B><BR>
<B><I>sulfides and sulfarsenides</I></B><BR>
chalcocite Cu<FONT SIZE=2><SUB>2</SUB></FONT>S<BR>
bornite Cu<FONT SIZE=2><SUB>2</SUB></FONT>FeS<FONT SIZE=2><SUB>4</SUB></FONT><BR>
galena PbS<SUP><BR>
</SUP>sphalerite ZnS<BR>
chalcopyrite CuFeS<FONT SIZE=2><SUB>2</SUB></FONT><BR>
pyrrhotite Fe<FONT SIZE=2><SUB>1</SUB></FONT><SUB>-x</SUB>S (x= 0-0.2)<BR>
pentlandite (Fe, Ni)<FONT SIZE=2><SUB>9</SUB></FONT>S<FONT SIZE=2><SUB>8</SUB></FONT><BR>
covellite CuS<BR>
cinnabar HgS<BR>
realgar AsS<BR>
orpiment As<FONT SIZE=2><SUB>2</SUB></FONT>S<FONT SIZE=2><SUB>3</SUB></FONT><SUB><BR>
</SUB>stibnite Sb<FONT SIZE=2><SUB>2</SUB></FONT>S<FONT SIZE=2><SUB>3</SUB></FONT><BR>
pyrite FeS<BR>
marcasite FeS<FONT SIZE=2><SUB>2</SUB></FONT><BR>
molybdenite MoS<BR>
arsenopyrite FeAsS<BR>
.<B><I>sulfosalts</I></B><BR>
pyrargynite Ag<FONT SIZE=2><SUB>3</SUB></FONT>SbS<FONT SIZE=2><SUB>3</SUB></FONT><BR>
proustite Ag<FONT SIZE=2><SUB>3</SUB></FONT>AsS<FONT SIZE=2><SUB>3</SUB></FONT><BR>
tetrahedrite (Cu, Fe)<FONT SIZE=2><SUB>12</SUB></FONT>Sb<FONT SIZE=2><SUB>4</SUB></FONT>S<FONT SIZE=2><SUB>13</SUB></FONT><BR>
tennantite (Cu, Fe)<FONT SIZE=2><SUB>12</SUB></FONT>As<FONT SIZE=2><SUB>4</SUB></FONT>S<FONT SIZE=2><SUB>13</SUB></FONT><BR>
enargite Cu<FONT SIZE=2><SUB>3</SUB></FONT>AsS<FONT SIZE=2><SUB>4</SUB></FONT><BR>
bournonite PbCuSbS<FONT SIZE=2><SUB>3</SUB></FONT><BR>
<B><I>sulfates</I></B><BR>
<B><I>barite group</I></B><BR>
barite BaSO<FONT SIZE=2><SUB>4</SUB></FONT><BR>
celesite SrSO<FONT SIZE=2><SUB>4</SUB></FONT><BR>
anglesite PbSO<FONT SIZE=2><SUB>4</SUB></FONT><BR>
anhydrite CaSO<FONT SIZE=2><SUB>4</SUB></FONT><BR>
gypsum CaSO<FONT SIZE=2><SUB>4</SUB></FONT>, 2H<FONT SIZE=2><SUB>2</SUB></FONT>O<BR>
<B>halides<BR>
</B>halite NaCl<B><BR>
</B>sylvite KCl<B><BR>
</B>chlorargyrite AgCl<B><BR>
</B>fluorite CaF<B><BR>
nitrates<BR>
</B>Seven known naturally occurring nitrates with the form XNO<FONT SIZE=2><SUB>3</SUB></FONT>, two of which are<B> </B>nitratite (NaNO<FONT SIZE=2><SUB>3</SUB></FONT>) and nitre (KNO<FONT SIZE=2><SUB>3</SUB></FONT>)<BR>
<B>borates</B><BR>
groups: BO<FONT SIZE=2><SUB>3</SUB></FONT>, B<FONT SIZE=2><SUB>2</SUB></FONT>O<FONT SIZE=2><SUB>5</SUB></FONT>, B<FONT SIZE=2><SUB>3</SUB></FONT>O<FONT SIZE=2><SUB>6</SUB></FONT>,B<FONT SIZE=2><SUB>2</SUB></FONT>O<FONT SIZE=2><SUB>4</SUB></FONT>, [B<FONT SIZE=2><SUB>4</SUB></FONT>O<FONT SIZE=2><SUB>5</SUB></FONT>(OH)<FONT SIZE=2><SUB>4</SUB></FONT>]<FONT SIZE=2><SUP>2</SUP></FONT><SUP><BR>
</SUP><B>silicates</B><BR>
<B><I>neosilicates</I></B>: olivine group, garnet group, zircon group, alumina group, topaz, and staurolite<BR>
<B><I>sorosilicates</I></B>: epidote group, and vesurvianite group<BR>
<B><I>Cyclo[</I></B>&#147;<B><I>ring</I></B>&#148;<B><I>]silicates</I></B> of the forms Si<FONT SIZE=2><SUB>3</SUB></FONT>O<FONT SIZE=2><SUB>9</SUB></FONT>, Si<FONT SIZE=2><SUB>4</SUB></FONT>O<FONT SIZE=2><SUB>12</SUB></FONT>, and Si<FONT SIZE=2><SUB>6</SUB></FONT>O<FONT SIZE=2><SUB>18</SUB></FONT><SUB> </SUB>benitoite, axinite, beryl, tourmaline, etc.<BR>
<B><I>Inosilicates</I></B>: pyroxenes and amphiboles<BR>
<B><I>phyllosilicates</I></B>: serpentine group, clay minerals group, talc, mica group, chlorite group<BR>
<B><I>tectosilicates</I></B>: SiO<FONT SIZE=2><SUB>2</SUB></FONT> group, feldspar group, feldspathoid group, f zeolite group<BR>
</note>
</notes>
</material>
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