Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Chlorite Group from
Águila area (Fé mine), Saelices el Chico, Salamanca, Castile and Leon, Spain


Locality type:Mine
Classification
Species:'Chlorite Group' (not an IMA approved species)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Chlorite Group data
Locality Data:Click here to view Águila area (Fé mine), Saelices el Chico, Salamanca, Castile and Leon, Spain
Data Identifiers
Mindat Occurrence Record ID:598956
Long-form Identifier:1:3:598956:0
GUID (UUID V4):0
Nearest other occurrences of Chlorite Group
26.9km (16.7 miles) ⓘPortugal 1 & 2 quarries, Malpartida, Malpartida e Vale de Coelha, Almeida, Guarda, Portugal
65.3km (40.6 miles) ⓘNumão prospect, Numão, Vila Nova de Foz Côa, Guarda, Portugal
66.7km (41.5 miles) ⓘFonte Santa Mine, Lagoaça e Fornos, Freixo de Espada à Cinta, Bragança, Portugal
67.8km (42.1 miles) ⓘCabeço da Mua Mine, Felgar e Souto da Velha, Torre de Moncorvo, Bragança, Portugal
71.6km (44.5 miles) ⓘLos Santos W deposit, Los Santos, Salamanca, Castile and Leon, Spain
83.5km (51.9 miles) ⓘBom Sucesso No. 4 quarry, Tavares (Chãs; Várzea e Travanca), Mangualde, Viseu, Portugal
84.3km (52.4 miles) ⓘVigia Mine, U.F. Aguiar da Beira e Coruche, Aguiar da Beira, Guarda, Portugal
86.6km (53.8 miles) ⓘVárzea de Trevões Mine, U.F S.J.da Pesqueira e Várzea de Trevões, São João da Pesqueira, Viseu, Portugal
87.5km (54.4 miles) ⓘVenturinha, Sezures, Penalva do Castelo, Viseu, Portugal
90.1km (56.0 miles) ⓘSão Pedro das Águias Mine, U.F Távora e Pereiro, Tabuaço, Viseu, Portugal
References
Both, R. A., Arribas, A., de Saint-Andre, B. (1994) The origin of breccia-hosted uranium deposits in carbonaceous metasediments of the Iberian Peninsula; U-Pb geochronology and stable isotope studies of the Fe Deposit, Salamanca Province, Spain. Economic Geology, 89 (3) 584-601 doi:10.2113/gsecongeo.89.3.584
 
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