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Alleghany Mining District (Forest Mining District), Sierra County, California, USAi
Regional Level Types
Alleghany Mining District (Forest Mining District)Mining District
Sierra CountyCounty
CaliforniaState
USACountry

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Mindat Locality ID:
24049
Long-form identifier:
mindat:1:2:24049:8
GUID (UUID V4):
3d7b570c-c3ad-45fe-bfa6-b08ceac419ff


NOTE: There is no file in the USGS MRDS database for this district. The USGS MRDS database gives priority to the name of Forest District while Clark (1970a) gives priority to the name of Alleghany District. Since Clark is the authority on California gold mining districts, Mindat gives deference to that reference.

Location: Alleghany is in southwestern Sierra County. This district is in a belt of gold mineralization that extends from Goodyear's Bar, S and SE through Forest, Alleghany, Chip's Flat, and Minnesota. This gold-bearing belt continues south to the Washington district in Nevada County. This district continues S across the Middle Yuba River, taking in a slice of land along the S side of the river. The Downieville and American Hill districts are to the east, and the Pike district is to the west.

History: The streams in the area were placer-mined soon after the beginning of the gold rush, and the Forest diggings were discovered in the summer of 1852 by some sailors. Some of these sailors were "Kanakas" or Hawaiians who also had deserted their ships in San Francisco. Forest, first known as Brownsville and then Elizaville, got its present name in 1853. The Bald Mountain and other drift mines were highly productive from then until around 1885. Hydraulic mining was done at Minnesota and Chip's Flat during these years. The town of Alleghany was named for Alleghany, Pennsylvania. Quartz mining was reported to have begun in the district in 1853 at the German Bar and Irelan mines. Although the quartz mines were moderately productive until the 1870's, drift mining was the principal source of gold then. The rediscovery of the Tightner vein in 1904 by H. F. Johnson (erroneously given as 1907 in many reports) led to the revival of lode mining, which continued until 1965.

Alleghany was the only town in California after World War II where gold mining was the principal segment of the economy. After 1960, production from the district, which had been averaging more than 1,500,000 (period values) per year, decreased greatly as more and more mining operations were curtailed. By 1963, the output was less than 1,100,000 (period values) per year. The Sixteen-to-One mine, the largest gold source in the district, curtailed normal operations late in 1962, and the Brush Creek mine, the second largest operation, was shut down in 1964. At the end of 1965 the Sixteen-to-One Mine was completely shut down, ending an operation that had lasted more than 60 years. Intermittent operations have continued at several mines, such as the Kate Hardy, Oriental, El Dorado-Plumbago, and Mugwump mines. Several of the mines received Federal exploration loans. Skin divers are active in the streams of the area.

Alleghany was the most famous high-grade gold mining district in California. The value of the total output is unknown, estimated at $50 million (period values). Much of this production was from small but spectacularly rich ore bodies.

Geology: The district is underlain by N and NW-trending beds of metamorphic rocks of the Calaveras Formation (Carboniferous to Permian), serpentine and greenstone. In the vicinity of Alleghany and Forest this formation has been divided into six units: Blue Canyon Slate, Tightner Formation (chiefly amphibolite and chlorite schist), Kanka Formation (conglomerate, chert, and slate), Relief Quartzite, Cape Horn Slate, and the Delhi Formation (phyllite and slate). These rocks have been invaded by many basic and ultra-basic intrusions; the ultra-basic rocks have been largely serpentinized. Mariposite-bearing rock, locally known as "bluejay," is commonly adjacent to the serpentine. Also present are fine to medium-grained dioritic dikes. The higher ridges are capped by andesite and basalt, which in places overlies auriferous Tertiary channel gravels.

Ore deposits: The gold-quartz veins strike in a northerly direction, dip either E or W, and usually range from two to five feet in thickness. They occupy minor reverse faults, and occur in all of the rocks of the Calaveras Formation, and in the greenstone. The largest number of mines are in amphibolites of the Tightner Formation. The most characteristic features of the ore deposits are the extreme richness, erratic distribution and small size of the ore shoots. They range from small masses of gold and quartz yielding a few hundred dollars to ore bodies that have yielded hundreds of thousands of dollars. One ore body at the Sixteen-to-One mine, which had a pitch length of 40 feet, contained nearly $1 million (period values), while another at the Oriental mine about 14 feet long yielded $1,734,000 (period values).

The gold occurs in the native state commonly with arsenopyrite but only small amounts of other sulfides. In a few places pyrite is abundant. The numerous serpentine bodies and associated mariposite rock are structurally important in the localization of the ore bodies. The quartz veins tend to fray or bend near serpentine, and it is in these frayed or bend portions of the veins that the high-grade ore bodies are often found. High-grade ore also is found in vein junctions or in sheared portions of the veins.

Channel gravels: A major tributary of the Tertiary
Yuba River extended S from Rock Creek through Forest and Alleghany and then SE through Chip's Flat and Minnesota to Moore's Flat in Nevada County. This is commonly known as the "Great Blue Lead" or Forest channel. It was uniformly rich except where cut by later channels. The largest gold producers were the Ruby, Live Yankee, and Bald Mountain drift mines, where many coarse nuggets were recovered. During the late 1930's a number of fist-sized gold nuggets were recovered from the Ruby mine. These were displayed for many years in the Sierra County exhibit at the California State Fair in Sacramento.

Mines: Lode: Brush Creek ($4 million+), Dreadnaught ($50,000 to $100,000), Docile ($100,000 to $200,000), Eclipse ($20,000 to $50,000), El Dorado ($325,000), German Bar ($200,000), Gold Canyon ($750,000 to $1 million), Gold Crown, Golden King ($250,000), Irelan ($350,000 to $500,000), Kate Hardy ($700,000), Kenton ($1 million to $1.25 million), Mariposa ($50,000), Morning Glory ($80,000 to $100,000), Mugwump [both lode and placer] ($50,000), North Fork [both lode and placer] ($125,000), Oriflamme, Ophir *, Oriental *($2.85 million), Osceola *, Plumbago ($3.5 million), Rainbow * ($2.5 million), Rainbow Extension*, Red Ledge, Red Star-Osceola* ($200,000), Rising Sun ($58,000), Shannon, Sixteen-to-One ($25 million+), South Fork [both lode and placer], Spoohn, Tightner *, Twenty One*, Wyoming, Yellowjacket.

Drift: Bald Mountain ($3.1 million), Bald Mountain Extension ($500,000 to $1 million), Gold Star ($250,000+), Highland & Masonic ($300,000+), Live Yankee ($750,000 to $1 million), Ruby ($1 million+).

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded from this region.


Mineral List

Mineral list contains entries from the region specified including sub-localities

36 valid minerals.

Detailed Mineral List:

β“˜ Albite
Formula: Na(AlSi3O8)
Localities:
Description: Occurs at a composition of about An10 in vein material & in wall rock of gold mines in the district.
β“˜ 'Amphibole Asbestos'
β“˜ 'Amphibole Supergroup'
Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Description: Occurs in amphibolite schist.
β“˜ Ankerite
Formula: Ca(Fe2+,Mg)(CO3)2
Description: Occurs as crystals on the faces of Quartz crystals.
β“˜ Arsenopyrite
Formula: FeAsS
Localities: Reported from at least 17 localities in this region.
β“˜ 'Asbestos'
β“˜ Beidellite
Formula: (Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 · nH2O
Colour: Gray
Description: Occurs as microscopically crystalline masses in cavities in veins of the district.
β“˜ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
β“˜ Calcite
Formula: CaCO3
β“˜ Chalcocite
Formula: Cu2S
Description: Occurs in very minor amounts.
β“˜ Chalcopyrite
Formula: CuFeS2
β“˜ 'Chlorite Group'
β“˜ Chromite
Formula: Fe2+Cr3+2O4
Localities: Reported from at least 8 localities in this region.
β“˜ Chrysotile
Formula: Mg3(Si2O5)(OH)4
β“˜ Dawsonite
Formula: NaAlCO3(OH)2
Habit: Fibrous
Colour: Pale green or tan tint
Description: Occurs as clusters of minute fibers as daughter products in fluid inclusions of gold-quartz veins. Individual crystals 5-20 microns long and 1 to 3 microns thick, although some as large as 200 x 5 microns noted.
β“˜ Dolomite
Formula: CaMg(CO3)2
β“˜ Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
β“˜ Galena
Formula: PbS
Localities: Reported from at least 8 localities in this region.
β“˜ Gold
Formula: Au
Localities: Reported from at least 111 localities in this region.
Description: Placer material. Apparently somewhat argentiferous.
β“˜ Graphite
Formula: C
β“˜ 'Hornblende'
Habit: "Needle" crystals.
Description: Occurs in a amphibolite schist.
β“˜ Jamesonite
Formula: Pb4FeSb6S14
Habit: Acicular
Description: Occurs as small needles and clusters in vugs in quartz gangue.
β“˜ 'Limonite'
β“˜ Magnesiochromite
Formula: MgCr2O4
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
Habit: Perfect octahedral
β“˜ Marcasite
Formula: FeS2
β“˜ 'Mica Group'
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Localities: Reported from at least 12 localities in this region.
β“˜ Muscovite var. Mariposite
Formula: K(Al,Cr)2(Al,Si)4O10(OH)2
Localities: Reported from at least 10 localities in this region.
β“˜ Muscovite var. Phengite
Formula: KAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
Localities: Reported from at least 10 localities in this region.
β“˜ Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Opal
Formula: SiO2 · nH2O
β“˜ Orthoclase
Formula: K(AlSi3O8)
β“˜ Palygorskite
Formula: (Mg,Al)2Si4O10(OH) · 4H2O
Description: Occurs as tough, felt-like sheets filling small veins.
β“˜ Paragonite
Formula: NaAl2(AlSi3O10)(OH)2
β“˜ Pentlandite
Formula: (NixFey)Ξ£9S8
β“˜ Pyrite
Formula: FeS2
Localities: Reported from at least 24 localities in this region.
β“˜ Quartz
Formula: SiO2
Localities: Reported from at least 90 localities in this region.
β“˜ Quartz var. Chalcedony
Formula: SiO2
β“˜ Rutile
Formula: TiO2
Habit: Acicular
Description: Occurs as small needles.
β“˜ Scorodite
Formula: Fe3+AsO4 · 2H2O
β“˜ 'Serpentine Subgroup'
Formula: D3[Si2O5](OH)4
Localities: Reported from at least 17 localities in this region.
β“˜ Siderite
Formula: FeCO3
β“˜ Silver
Formula: Ag
β“˜ Sphalerite
Formula: ZnS
β“˜ Stromeyerite
Formula: AgCuS
β“˜ Talc
Formula: Mg3Si4O10(OH)2
Localities: Reported from at least 8 localities in this region.
β“˜ 'Tetrahedrite Subgroup'
Formula: Cu6(Cu4C2+2)Sb4S12S
β“˜ Tremolite
Formula: ◻Ca2Mg5(Si8O22)(OH)2
β“˜ Uvarovite
Formula: Ca3Cr2(SiO4)3
Description: Occurs as minute crystals in veinlets of serpentine in gold mines of the district.
β“˜ 'Wad'

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Gold1.AA.05Au
β“˜Graphite1.CB.05aC
β“˜Silver1.AA.05Ag
Group 2 - Sulphides and Sulfosalts
β“˜Arsenopyrite2.EB.20FeAsS
β“˜Chalcocite2.BA.05Cu2S
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Jamesonite2.HB.15Pb4FeSb6S14
β“˜Marcasite2.EB.10aFeS2
β“˜Pentlandite2.BB.15(NixFey)Ξ£9S8
β“˜Pyrite2.EB.05aFeS2
β“˜Sphalerite2.CB.05aZnS
β“˜Stromeyerite2.BA.40AgCuS
β“˜'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
β“˜Chromite4.BB.05Fe2+Cr3+2O4
β“˜Magnesiochromite4.BB.05MgCr2O4
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜Opal4.DA.10SiO2 Β· nH2O
β“˜Quartz4.DA.05SiO2
β“˜var. Chalcedony4.DA.05SiO2
β“˜Rutile4.DB.05TiO2
Group 5 - Nitrates and Carbonates
β“˜Ankerite5.AB.10Ca(Fe2+,Mg)(CO3)2
β“˜Calcite5.AB.05CaCO3
β“˜Dawsonite5.BB.10NaAlCO3(OH)2
β“˜Dolomite5.AB.10CaMg(CO3)2
β“˜Siderite5.AB.05FeCO3
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Scorodite8.CD.10Fe3+AsO4 Β· 2H2O
Group 9 - Silicates
β“˜Albite9.FA.35Na(AlSi3O8)
β“˜Beidellite9.EC.40(Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 Β· nH2O
β“˜Chrysotile9..Mg3(Si2O5)(OH)4
β“˜Epidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜var. Mariposite9.EC.15K(Al,Cr)2(Al,Si)4O10(OH)2
β“˜var. Phengite9.EC.15KAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
β“˜var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Orthoclase9.FA.30K(AlSi3O8)
β“˜Palygorskite9.EE.20(Mg,Al)2Si4O10(OH) Β· 4H2O
β“˜Paragonite9.EC.15NaAl2(AlSi3O10)(OH)2
β“˜Talc9.EC.05Mg3Si4O10(OH)2
β“˜Tremolite9.DE.10β—»Ca2Mg5(Si8O22)(OH)2
β“˜Uvarovite9.AD.25Ca3Cr2(SiO4)3
Unclassified Minerals, Rocks, etc.
β“˜'Amphibole Asbestos'-
β“˜'Amphibole Supergroup'-AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
β“˜'Asbestos'-
β“˜'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
β“˜'Chlorite Group'-
β“˜'Hornblende'-
β“˜'Limonite'-
β“˜'Mica Group'-
β“˜'Serpentine Subgroup'-D3[Si2O5](OH)4
β“˜'Wad'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
Hβ“˜ TalcMg3Si4O10(OH)2
Hβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Hβ“˜ ChrysotileMg3(Si2O5)(OH)4
Hβ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Hβ“˜ DawsoniteNaAlCO3(OH)2
Hβ“˜ Palygorskite(Mg,Al)2Si4O10(OH) · 4H2O
Hβ“˜ Muscovite var. MaripositeK(Al,Cr)2(Al,Si)4O10(OH)2
Hβ“˜ Beidellite(Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 · nH2O
Hβ“˜ ScoroditeFe3+AsO4 · 2H2O
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Hβ“˜ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Hβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Hβ“˜ OpalSiO2 · nH2O
Hβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Hβ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
CCarbon
Cβ“˜ CalciteCaCO3
Cβ“˜ SideriteFeCO3
Cβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Cβ“˜ DawsoniteNaAlCO3(OH)2
Cβ“˜ DolomiteCaMg(CO3)2
Cβ“˜ GraphiteC
OOxygen
Oβ“˜ RutileTiO2
Oβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
Oβ“˜ QuartzSiO2
Oβ“˜ TalcMg3Si4O10(OH)2
Oβ“˜ ChromiteFe2+Cr23+O4
Oβ“˜ CalciteCaCO3
Oβ“˜ SideriteFeCO3
Oβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Oβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Oβ“˜ ChrysotileMg3(Si2O5)(OH)4
Oβ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Oβ“˜ MagnesiochromiteMgCr2O4
Oβ“˜ DawsoniteNaAlCO3(OH)2
Oβ“˜ Palygorskite(Mg,Al)2Si4O10(OH) · 4H2O
Oβ“˜ Muscovite var. MaripositeK(Al,Cr)2(Al,Si)4O10(OH)2
Oβ“˜ AlbiteNa(AlSi3O8)
Oβ“˜ Beidellite(Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 · nH2O
Oβ“˜ UvaroviteCa3Cr2(SiO4)3
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ ScoroditeFe3+AsO4 · 2H2O
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Oβ“˜ DolomiteCaMg(CO3)2
Oβ“˜ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Oβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Oβ“˜ OpalSiO2 · nH2O
Oβ“˜ Quartz var. ChalcedonySiO2
Oβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Oβ“˜ OrthoclaseK(AlSi3O8)
Oβ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
FFluorine
Fβ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Fβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
NaSodium
Naβ“˜ DawsoniteNaAlCO3(OH)2
Naβ“˜ AlbiteNa(AlSi3O8)
Naβ“˜ Beidellite(Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 · nH2O
Naβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
MgMagnesium
Mgβ“˜ TalcMg3Si4O10(OH)2
Mgβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Mgβ“˜ ChrysotileMg3(Si2O5)(OH)4
Mgβ“˜ MagnesiochromiteMgCr2O4
Mgβ“˜ Palygorskite(Mg,Al)2Si4O10(OH) · 4H2O
Mgβ“˜ DolomiteCaMg(CO3)2
Mgβ“˜ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Mgβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Mgβ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
AlAluminium
Alβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Alβ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Alβ“˜ DawsoniteNaAlCO3(OH)2
Alβ“˜ Palygorskite(Mg,Al)2Si4O10(OH) · 4H2O
Alβ“˜ Muscovite var. MaripositeK(Al,Cr)2(Al,Si)4O10(OH)2
Alβ“˜ AlbiteNa(AlSi3O8)
Alβ“˜ Beidellite(Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 · nH2O
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Alβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Alβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Alβ“˜ OrthoclaseK(AlSi3O8)
Alβ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
SiSilicon
Siβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
Siβ“˜ QuartzSiO2
Siβ“˜ TalcMg3Si4O10(OH)2
Siβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Siβ“˜ ChrysotileMg3(Si2O5)(OH)4
Siβ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Siβ“˜ Palygorskite(Mg,Al)2Si4O10(OH) · 4H2O
Siβ“˜ Muscovite var. MaripositeK(Al,Cr)2(Al,Si)4O10(OH)2
Siβ“˜ AlbiteNa(AlSi3O8)
Siβ“˜ Beidellite(Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 · nH2O
Siβ“˜ UvaroviteCa3Cr2(SiO4)3
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Siβ“˜ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Siβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Siβ“˜ OpalSiO2 · nH2O
Siβ“˜ Quartz var. ChalcedonySiO2
Siβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Siβ“˜ OrthoclaseK(AlSi3O8)
Siβ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
SSulfur
Sβ“˜ ArsenopyriteFeAsS
Sβ“˜ PyriteFeS2
Sβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
Sβ“˜ GalenaPbS
Sβ“˜ SphaleriteZnS
Sβ“˜ MarcasiteFeS2
Sβ“˜ JamesonitePb4FeSb6S14
Sβ“˜ ChalcociteCu2S
Sβ“˜ StromeyeriteAgCuS
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ Pentlandite(NixFey)Ξ£9S8
ClChlorine
Clβ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
KPotassium
Kβ“˜ Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
Kβ“˜ Muscovite var. MaripositeK(Al,Cr)2(Al,Si)4O10(OH)2
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Kβ“˜ OrthoclaseK(AlSi3O8)
Kβ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
CaCalcium
Caβ“˜ CalciteCaCO3
Caβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Caβ“˜ Beidellite(Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 · nH2O
Caβ“˜ UvaroviteCa3Cr2(SiO4)3
Caβ“˜ DolomiteCaMg(CO3)2
Caβ“˜ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Caβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
TiTitanium
Tiβ“˜ RutileTiO2
Tiβ“˜ Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Tiβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
CrChromium
Crβ“˜ ChromiteFe2+Cr23+O4
Crβ“˜ MagnesiochromiteMgCr2O4
Crβ“˜ Muscovite var. MaripositeK(Al,Cr)2(Al,Si)4O10(OH)2
Crβ“˜ UvaroviteCa3Cr2(SiO4)3
FeIron
Feβ“˜ ArsenopyriteFeAsS
Feβ“˜ PyriteFeS2
Feβ“˜ ChromiteFe2+Cr23+O4
Feβ“˜ SideriteFeCO3
Feβ“˜ AnkeriteCa(Fe2+,Mg)(CO3)2
Feβ“˜ MarcasiteFeS2
Feβ“˜ JamesonitePb4FeSb6S14
Feβ“˜ MagnetiteFe2+Fe23+O4
Feβ“˜ ScoroditeFe3+AsO4 · 2H2O
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Feβ“˜ Pentlandite(NixFey)Ξ£9S8
Feβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2
Feβ“˜ Muscovite var. PhengiteKAl1.5(Mg,Fe)0.5(Al0.5Si3.5O10)(OH)2
NiNickel
Niβ“˜ Pentlandite(NixFey)Ξ£9S8
CuCopper
Cuβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
Cuβ“˜ ChalcociteCu2S
Cuβ“˜ StromeyeriteAgCuS
Cuβ“˜ ChalcopyriteCuFeS2
ZnZinc
Znβ“˜ SphaleriteZnS
AsArsenic
Asβ“˜ ArsenopyriteFeAsS
Asβ“˜ ScoroditeFe3+AsO4 · 2H2O
AgSilver
Agβ“˜ SilverAg
Agβ“˜ StromeyeriteAgCuS
SbAntimony
Sbβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
Sbβ“˜ JamesonitePb4FeSb6S14
AuGold
Auβ“˜ GoldAu
PbLead
Pbβ“˜ GalenaPbS
Pbβ“˜ JamesonitePb4FeSb6S14

Fossils

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Localities in this Region

Other Regions, Features and Areas that Intersect


This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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