| Locality type: | Mine |
| Classification |
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| Species: | Columbite-(Fe) |
| Formula: | Fe2+Nb2O6 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Columbite-(Fe) data |
| Locality Data: | Click here to view Palermo No. 2 Mine, Groton, Grafton County, New Hampshire, USA |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 325482 |
| Long-form Identifier: | 1:3:325482:0 |
| GUID (UUID V4): | 8c913069-ecbc-4ab9-88dc-ad0b11bdd507 |
| Nearest other occurrences of Columbite-(Fe) |
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| 0.3km (0.2 miles) | ⓘPalermo No. 1 Mine, Groton, Grafton County, New Hampshire, USA |
| 15.5km (9.6 miles) | ⓘPattuck Quarry, Alexandria, Grafton County, New Hampshire, USA |
| 15.6km (9.7 miles) | ⓘE.E. Smith Mine, Alexandria, Grafton County, New Hampshire, USA |
| 19.6km (12.2 miles) | ⓘRuggles Mine, Grafton, Grafton County, New Hampshire, USA |
| 58.5km (36.3 miles) | ⓘMoose pocket, Blue Mountain, Albany, Carroll County, New Hampshire, USA |
| 67.6km (42.0 miles) | ⓘAcworth, Sullivan County, New Hampshire, USA |
| 70.6km (43.8 miles) | ⓘRedstone "Red Granite" quarry, Redstone, Conway, Carroll County, New Hampshire, USA |
| 71.6km (44.5 miles) | ⓘHam and Weeks Mine, Wakefield, Carroll County, New Hampshire, USA |
| 74.3km (46.2 miles) | ⓘBlack Cap Mountain, North Conway, Conway, Carroll County, New Hampshire, USA |
| 89.5km (55.6 miles) | ⓘEstes Quarry, West Baldwin, Baldwin, Cumberland County, Maine, USA |
| References |
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| Reference Search (possible matching items) |
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 | | Journal (article/letter/editorial) | | bbirch@museum.vic.gov.au Abstract: Complex assemblages of Fe–Mn phosphate minerals occur in several granitic pegmatites...range of species, based on new nomenclature schemes for the three main groups of Fe–Mn phosphates present...Key-words: arrojadite; alluaudite; jahnsite–whiteite; Fe–Mn phosphates; granite pegmatite; Mount Wills; Victoria...https://pubs.geoscienceworld.org/eurjmin/). Specifically, Fe–Mn phosphate minerals have been collected from the...from the early mining operations (Fig. S1 and Fig. 2). However, the pegmatite dyke field extends for nearly |
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