| Locality type: | Mine |
| Classification |
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| Species: | 'Limonite' (not an IMA approved species) |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Limonite data |
| Locality Data: | Click here to view Banchet Mine, Névache, Briançon, Hautes-Alpes, Provence-Alpes-Côte d'Azur, France |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1489840 |
| Long-form Identifier: | 1:3:1489840:2 |
| GUID (UUID V4): | 9a1b182f-fcc3-4238-a990-187229ed15d0 |
| Nearest other occurrences of Limonite |
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| 4.4km (2.7 miles) | ⓘMont Thabor, Névache, Briançon, Hautes-Alpes, Provence-Alpes-Côte d'Azur, France |
| 10.3km (6.4 miles) | ⓘPlampinet, Névache, Briançon, Hautes-Alpes, Provence-Alpes-Côte d'Azur, France |
| 15.7km (9.7 miles) | ⓘLes Clochettes mine, Villar-d'Arêne, Briançon, Hautes-Alpes, Provence-Alpes-Côte d'Azur, France |
| 18.0km (11.2 miles) | ⓘ"Bardonecchia road" quartzite vein, Oulx, Metropolitan City of Turin, Piedmont, Italy |
| 18.5km (11.5 miles) | ⓘLa Beaume, Oulx, Metropolitan City of Turin, Piedmont, Italy |
| 22.3km (13.9 miles) | ⓘPunta Rascià, Cesana Torinese, Metropolitan City of Turin, Piedmont, Italy |
| 22.5km (14.0 miles) | ⓘMonte Cruzore (Monte Cruzeau), Cesana Torinese, Metropolitan City of Turin, Piedmont, Italy |
| 23.0km (14.3 miles) | ⓘRoccia Rossa, Cesana Torinese, Metropolitan City of Turin, Piedmont, Italy |
| 23.2km (14.4 miles) | ⓘMonte Gimont east slope (Grand Charvia east slope), Cesana Torinese, Metropolitan City of Turin, Piedmont, Italy |
| 25.6km (15.9 miles) | ⓘLago Nero spilite outcrop, Cesana Torinese, Metropolitan City of Turin, Piedmont, Italy |
| References |
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| Reference Search (possible matching items) |
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 | | Journal (article/letter/editorial) | | classic décollement of the Jura Mountains of eastern France (Bucher, 1933, p. 151; Rodgers, 1964). Rodgers...might also correspond to the Subalpine chains of France and to the Helvetic nappes as well as the Jura...and Drahovzal (1974) interpreted a thin zone of limonite mineralization along the contact as evidence of...two. However, no strata are missing. Zones of limonite are common in the coastal-plain strata — for example...stopped at the impermeable contact, and a hard limonite deposit may be built up. A similar situation exists |
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