| Locality type: | Road Cutting |
| Classification |
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| Species: | Microcline |
| Formula: | K(AlSi3O8) |
| Confirmation |
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| Validity: | Confirmed |
| Confirmation Methods: | Visually Identified |
| Data |
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| Mineral Data: | Click here to view Microcline data |
| Locality Data: | Click here to view Nalum, Brunlanes, Larvik, Vestfold, Norway |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1269555 |
| Long-form Identifier: | 1:3:1269555:5 |
| GUID (UUID V4): | 69659b14-3645-4f33-8b84-6af0863533c2 |
| Nearest other occurrences of Microcline |
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| 1.4km (0.9 miles) | ⓘJahrehagen cottage grounds, Jahren pegmatite, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 1.4km (0.9 miles) | ⓘJahren Feldspar Quarry (Jaren Feldspar Quarry), Jahren pegmatite, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 1.4km (0.9 miles) | ⓘRV 301 Helgeroaveien roadcut, Jahren pegmatite, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 2.0km (1.3 miles) | ⓘFuglevika Feldspar Prospect, Fuglevika, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 2.5km (1.5 miles) | ⓘNattmannsodden, Rakke, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 2.5km (1.5 miles) | ⓘPegmatite near Tangmathola, Rakke, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 2.5km (1.5 miles) | ⓘKuøya, Fuglevika, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 2.5km (1.6 miles) | ⓘPegmatite SW of Rakke Fort, Rakke, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 2.5km (1.6 miles) | ⓘPegmatite W of Rakke Fort, Rakke, Stavern (Fredriksvärn), Larvik, Vestfold, Norway |
| 3.1km (1.9 miles) | ⓘStavern (Fredriksvärn), Larvik, Vestfold, Norway |
| References |
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| Reference Search (possible matching items) |
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 | | Book | | professionally educated mineralogist. today call the Larvik plutonic complex have been described from the...system. Br0gger ( 1851- the various sites in the Larvik plutonic including involvement in the description...about 185minerals from these occurrences. in the Larvik plutonic complex, including since 1881,and became...and the publication of the elsewhere, and the Larvik pegmatites should be studied by modem methods...be fertile fields of investigation. part of the Larvik plutonic complex, The publication of this up-to-date |
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