| Classification |
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| Species: | Quartz |
| Formula: | SiO2 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Quartz data |
| Locality Data: | Click here to view Klintberget, Hagfors, Värmland County, Sweden |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 733868 |
| Long-form Identifier: | 1:3:733868:7 |
| GUID (UUID V4): | d5c8e167-1bcc-4632-ac43-29ab6db2f00d |
| Nearest other occurrences of Quartz |
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| 20.5km (12.7 miles) | ⓘJakobsberg Mine, Jakobsberg ore field, Nordmark mining district, Filipstad, Värmland County, Sweden |
| 20.9km (13.0 miles) | ⓘLahäll Mines, Långban Ore District, Filipstad, Värmland County, Sweden |
| 23.7km (14.7 miles) | ⓘLångban Mine, Långban Ore District, Filipstad, Värmland County, Sweden |
| 24.9km (15.5 miles) | ⓘGåsborn, Filipstad, Värmland County, Sweden |
| 31.1km (19.3 miles) | ⓘHarstigen Mine, Pajsberg, Persberg ore district, Filipstad, Värmland County, Sweden |
| 32.2km (20.0 miles) | ⓘMörkhult Mine, Persberg, Filipstad, Värmland County, Sweden |
| 33.2km (20.6 miles) | ⓘGåsgruvan, Gåsgruvan ore field, Persberg ore district, Filipstad, Värmland County, Sweden |
| 33.2km (20.7 miles) | ⓘGåsgruvan Quarry, Persberg ore district, Filipstad, Värmland County, Sweden |
| 33.9km (21.1 miles) | ⓘHällefors silver mines, Hällefors, Örebro County, Sweden |
| 38.0km (23.6 miles) | ⓘRansätershöjden, Ransäter, Munkfors, Värmland County, Sweden |
| References |
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| Reference Search (possible matching items) |
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 | | Journal (volume) | | the industrial minerals K-feldspar, Nafeldspar, quartz and mica (e.g. Glover et al. 2012). For these reasons...pegmatite bodies, the occurrence of massive, monophase quartz cores in the centre of pegmatites and the extreme...Madagascar (Schaller 1916, Rickwood 1981). Massive quartz cores in pegmatites can reach dimensions of more...pegmatite-forming minerals, including feldspar, mica, and quartz, has potential for a chemical classification, even...(3) the common occurrence of massive, monophase quartz cores in the centre of pegmatites, and (4) the |
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