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Samarskite-(Y) from
Guadalupe deposit, Alamos area, Petaca Mining District, Rio Arriba County, New Mexico, USA


Locality type:Deposit
Classification
Species:Samarskite-(Y)
Formula:YFe3+Nb2O8
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Samarskite-(Y) data
Locality Data:Click here to view Guadalupe deposit, Alamos area, Petaca Mining District, Rio Arriba County, New Mexico, USA
Data Identifiers
Mindat Occurrence Record ID:794029
Long-form Identifier:1:3:794029:3
GUID (UUID V4):a9f51e71-82da-46e8-b0e5-47c11e054c32
Nearest other occurrences of Samarskite-(Y)
0.0km (0.0 miles) Carmelita deposit, Alamos area, Petaca Mining District, Rio Arriba County, New Mexico, USA
0.8km (0.5 miles) Globe pegmatite (Globe Mine), South Petaca, Petaca Mining District, Rio Arriba County, New Mexico, USA
1.1km (0.7 miles) Red claim (Peacock claim), Alamos area, Petaca Mining District, Rio Arriba County, New Mexico, USA
1.6km (1.0 miles) Alamos deposit (Parker deposit), Alamos area, Petaca Mining District, Rio Arriba County, New Mexico, USA
1.8km (1.1 miles) White Pegmatite (Lyons deposit), Alamos area, Petaca Mining District, Rio Arriba County, New Mexico, USA
2.0km (1.2 miles) El Floto deposit, La Madera-Paloma Canyon area, Petaca Mining District, Rio Arriba County, New Mexico, USA
2.1km (1.3 miles) Hillside deposit, Alamos area, Petaca Mining District, Rio Arriba County, New Mexico, USA
2.3km (1.4 miles) Ancen deposit (Ancon deposit), La Madera-Paloma Canyon area, Petaca Mining District, Rio Arriba County, New Mexico, USA
2.3km (1.4 miles) Alto deposit, Alamos area, Petaca Mining District, Rio Arriba County, New Mexico, USA
2.8km (1.7 miles) La Paloma deposit, La Madera-Paloma Canyon area, Petaca Mining District, Rio Arriba County, New Mexico, USA
References
Reference Search (possible matching items)
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{100},{111},{210} . . . n nz, n,, nt ®o> b0, co a,h Y Angstrom = 10~8 cm millimicron = 0.000001 mm crystallographic...which shows that it dates back to the beginnings of mining. By minerals we mean the constituents of rocks...placed by other minerals which are stable under the new conditions. Quite a few minerals, however, such as...accumulation in a par­ ticular locality, called a mineral deposit, is large enough. The percent­ age of the useful...useful component is high enough to make mining worth­ while. Some minerals contain important metals, such
 
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