| Locality type: | Quarry |
| Classification |
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| Species: | Gadolinite-(Y) |
| Formula: | Y2Fe2+Be2Si2O10 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Gadolinite-(Y) data |
| Locality Data: | Click here to view Graniczna quarry, Strzegom, Gmina Strzegom, Świdnica County, Lower Silesian Voivodeship, Poland |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 533581 |
| Long-form Identifier: | 1:3:533581:7 |
| GUID (UUID V4): | 4350bb47-3c55-47d9-a159-aa0b68aa49a8 |
| Nearest other occurrences of Gadolinite-(Y) |
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| 34.4km (21.3 miles) | ⓘKarpniki pegmatite, Karpniki, Gmina Mysłakowice, Karkonosze County, Lower Silesian Voivodeship, Poland |
| 37.4km (23.3 miles) | ⓘUnnamed quarry, Kowary, Karkonosze County, Lower Silesian Voivodeship, Poland |
| 38.7km (24.1 miles) | ⓘŁomnica pegmatites, Łomnica, Gmina Mysłakowice, Karkonosze County, Lower Silesian Voivodeship, Poland |
| 40.9km (25.4 miles) | ⓘJulianna pegmatite, DSS Piława Górna Quarry, Piława Górna, Dzierżoniów County, Lower Silesian Voivodeship, Poland |
| 49.6km (30.8 miles) | ⓘRudzianki pegmatite, Zachełmie, Gmina Podgórzyn, Karkonosze County, Lower Silesian Voivodeship, Poland |
| 54.3km (33.8 miles) | ⓘMichałowice granite quarry, Piechowice, Karkonosze County, Lower Silesian Voivodeship, Poland |
| 60.1km (37.3 miles) | ⓘSzklarska Poręba Huta granite quarry, Szklarska Poręba, Karkonosze County, Lower Silesian Voivodeship, Poland |
| 61.1km (38.0 miles) | ⓘSkalna Brama pegmatite, Szklarska Poręba, Karkonosze County, Lower Silesian Voivodeship, Poland |
| References |
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| Reference Search (possible matching items) |
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 | | Book | | term mineralurgia becomes more and more popular in Poland, Italy, Portugal, Spain, Slovakia, Hungry, Czech...processing grain 17 upper quark gluon molecule lower quark proton atom nucleus neutron electron Fig...example sulfides become sulfates, ions featuring lower degree of oxidation into highly oxidized ions. Oxidation...forming the minerals whose sum of molar volume is lower than the sum of molar volumes of original minerals...semi-products, intermediate products, concentrates of lower quality, and so on, are obtained. The analysis of |
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