| Locality type: | Quarry |
| Classification |
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| Species: | Natrojarosite |
| Formula: | NaFe3(SO4)2(OH)6 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Natrojarosite data |
| Locality Data: | Click here to view Trandorf, Mühldorf, Krems-Land District, Lower Austria, Austria |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 268571 |
| Long-form Identifier: | 1:3:268571:7 |
| GUID (UUID V4): | 5973914c-f0eb-4ae9-95db-7d4f634a6b47 |
| Nearest other occurrences of Natrojarosite |
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| 0.7km (0.5 miles) | ⓘRoad cut, Amstall, Mühldorf, Krems-Land District, Lower Austria, Austria |
| 1.0km (0.6 miles) | ⓘWeinberg Middle, Amstall, Mühldorf, Krems-Land District, Lower Austria, Austria |
| 1.5km (0.9 miles) | ⓘGraphite quarry, Amstall, Mühldorf, Krems-Land District, Lower Austria, Austria |
| 2.4km (1.5 miles) | ⓘGraphite mine, Elsenreith, Kottes-Purk, Zwettl District, Lower Austria, Austria |
| 7.5km (4.7 miles) | ⓘArzberg (Atzberg; Michaeler Berg), Spitz, Krems-Land District, Lower Austria, Austria |
| 18.1km (11.2 miles) | ⓘGraphite deposit, Hengstberg, Hafnerbach, Sankt Pölten-Land District, Lower Austria, Austria |
| 39.6km (24.6 miles) | ⓘMarble quarry, Atzelsdorf, Brunn an der Wild, Horn District, Lower Austria, Austria |
| 54.3km (33.7 miles) | ⓘGraphite quarry, Wollmersdorf (Zettlitz-Wollmersdorf), Drosendorf-Zissersdorf, Horn District, Lower Austria, Austria |
| 92.5km (57.5 miles) | ⓘHaringgraben gypsum mine, Oberort (Tragöß-Oberort), Tragöß-Sankt Katharein, Bruck-Mürzzuschlag District, Styria, Austria |
| 98.3km (61.1 miles) | ⓘUnnamed mine, Teschengraben, Krieglach, Bruck-Mürzzuschlag District, Styria, Austria |
| References |
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| Reference Search (possible matching items) |
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 | | Journal (article/letter/editorial) | | alunite-group minerals as well as the mineral natrojarosite were discovered within the metamorphic quartz...l'alunite (ces min~raux 6rant dissous) et de la natrojarosite, inclus dans la matrice quartzitique m6tamorphique;...schists occur near the base of the belt within the "Lower Sediments" which comprise also shales, banded iron...have taken place during the deposition of the "Lower Sediments" because of the frequent occurrence of...the quartz fabric, that were identified as natrojarosite, NaFe~+[SO4]~(OH)6. If this correlation can |  | | Journal (article/letter/editorial) | | within a distinct range of H2SO4-concentrations, the lower limit being independent of the temperature and of...natroalunite, the upper limit lies at somewhat lower concentrations (~0,2). If the concentration of H2SO...gel-like products, at concentrations below the lower limit, the starting material remains unchanged....starting material, jarosite is generally formed at lower temperatures, at higher temperatures alunite is...temperatures higher acid concentrations yield jarosite and lower concentrations alunite. In the temperature range |  | | Book | | index are distinctive. Garnet and spine! have n1uch lower indices of refraction and are usually highly colored...uneven color, usually purple. Cryolite has even lower index of refraction (n :::::: l.338) and shows weak...Cassiterite and baddeleyite (ZrO 2 ) have much lower birefringence. Anatase and hen1atite are optically...and untwinned, and apatite has lower indices of refraction and lower birefringence. DISTINGUlSHING FEATURES...O 3 in partial solid solution above 1050"C. At lower temperatures, exsolut ion occurs, a nd ilmenite |
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