Locality type: | Outcrop |
Classification |
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Species: | Fluorapatite |
Formula: | Ca5(PO4)3F |
Comments: | Reported as apatite by the authors prior to 2000. |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Fluorapatite data |
Locality Data: | Click here to view Camaldoli della Torre, Torre del Greco, Mount Vesuvius, Somma-Vesuvius Complex, Naples, Campania, Italy |
Data Identifiers |
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Mindat Occurrence Record ID: | 480144 |
Long-form Identifier: | 1:3:480144:3 |
GUID (UUID V4): | adcea45e-dc23-4fd9-9c64-d03e09c6cb96 |
Nearest other occurrences of Fluorapatite |
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3.2km (2.0 miles) | ⓘVilla Inglese quarries, Torre del Greco, Mount Vesuvius, Somma-Vesuvius Complex, Naples, Campania, Italy |
5.7km (3.5 miles) | ⓘSan Vito Quarry, San Vito, Ercolano, Mount Somma, Somma-Vesuvius Complex, Naples, Campania, Italy |
7.1km (4.4 miles) | ⓘCupa dell'Olivella, Sant'Anastasia, Mount Somma, Somma-Vesuvius Complex, Naples, Campania, Italy |
8.8km (5.5 miles) | ⓘLagno Macedonia, Somma Vesuviana, Mount Somma, Somma-Vesuvius Complex, Naples, Campania, Italy |
92.2km (57.3 miles) | ⓘPertosa-Auletta Cave, Pertosa, Salerno, Campania, Italy |
References |
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Reference Search (possible matching items) |
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| Macdonald, Ray, Bagiński, Bogusław, Rolandi, Giuseppe, De Vivo, Benedetto, Kopczyńska, Anna (2016) Petrology of parasitic and eccentric cones on the flanks and base of Somma-Vesuvius. Mineralogy and Petrology, 110 (1) 65-85 doi:10.1007/s00710-015-0410-6 | Journal (article/letter/editorial) | and eccentric cones on the flanks and base of Somma-Vesuvius Ray Macdonald 1,2 & Bogusław Bagiński 1 & Giuseppe...base of Somma-Vesuvius potentially provide information on the plumbing system of the complex. We present...Scienze della Terra, dell’Ambiente e delle Risorse, Università di Napoli Federico II, 80134 Naples, Italy...studied volcanic complex in the world, many aspects of the evolution of Somma-Vesuvius remain enigmatic...the flanks of the complex. The cones occur up to 10 km from the centre of the Somma caldera and thus are |
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