Locality type: | Gorge |
Classification |
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Species: | 'Apatite' (not an IMA approved species) |
Formula: | Ca5(PO4)3(Cl/F/OH) |
Comments: | In rocks of the Werfen Formation. |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Apatite data |
Locality Data: | Click here to view Bletterbach Gorge, Radein (Redagno), Aldein (Aldino), Ăberetsch-Unterland (Oltradige-Bassa Atesina), South Tyrol, Trentino-Alto Adige (Trentino-South Tyrol), Italy |
Data Identifiers |
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Mindat Occurrence Record ID: | 1426523 |
Long-form Identifier: | 1:3:1426523:3 |
GUID (UUID V4): | 8fd0fcab-2f5c-431e-852f-a5f0dea7988c |
Nearest other occurrences of Apatite |
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15.6km (9.7 miles) | âCanzoccoli Quarry, Predazzo, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
16.9km (10.5 miles) | âBedovina mine, Predazzo, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
18.1km (11.3 miles) | âMonte MulĂ t (Monte Mulazzo; Monte Mulatto), Predazzo, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
19.7km (12.2 miles) | âCosta di Viezzena (Porta di Viezzena), Moena, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
22.1km (13.7 miles) | âPizmeda (Piz Meda), Moena, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
25.5km (15.8 miles) | âToal del Malinverno, San Giovanni di Fassa, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
26.1km (16.2 miles) | âCima D'Asta-Campo Regana, Castello Tesino, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
26.7km (16.6 miles) | âSelle Lake area, Pozza di Fassa, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
31.2km (19.4 miles) | âErla Mine, "Le Trote" ("La Trota"), Baselga di PinĂš, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
32.8km (20.4 miles) | âViarago Mine, Pergine Valsugana, Trento Province (Trentino), Trentino-Alto Adige (Trentino-South Tyrol), Italy |
References |
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Reference Search (possible matching items) |
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| | Book | between Vienna and Graz in Austria and Genova in Italy. They resulted from the collision of the African...into the Helvetic, Penninic, Austro-Alpine and South-Alpine domains. The basic idea in planning the book...Bernina Massif (Grisons, Switzerland; Valtellina, Italy). . . . . . . . . . . . . . . . . . . . . . . ....M. THONI Austro-Alpine Basement Complex to the South of the Tauern Window. . . . . . .. 495 B. SCHULZ...Metamorphic Histories in the Orobic Southern Alps, Italy ............................................... | | | Book | Spain Dock House, The Waterfront, Cape Town 8001, South Africa http ://www. Cambridge. org © Cambridge University...West Tethys provinces 29 Iran Afghanistan South Tibet South China Correlation of Himalayan and Salt Range...References 7 Permo-Triassic boundary relations in South China Permo-Triassic boundary on the Indian peninsula...Rajmahal, Malda-Galsi, Purnea, and Birbhum basins South Rewa basins Mahanadi and SE Son Valley basins Kamptee-Wardha...Transcaucasia North Caucasus Pamirs Mangyshlak peninsula South Primorye Physical and chemical characteristics of | | | Report (issue) | 1. Sedimentary basinsâItalyâDolomite AlpsâCongresses. 2. Rocks, CarbonateâItalyâDolomite AlpsâCongress...AlpsâCongress. 3. Sedimentary structuresâItalyâDolomite AlpsâMathematical modelsâCongresses. 4. Sequence stratigraphyâCongresses... StratigraphicâMesozoicâCongresses. 6. GeologyâItalyâDolomite AlpsâCongresses. I. Boer, Poppe Lubberts...platform: the Rosengarten, Middle Triassic, Dolomites, Italy Axel Emmerich, Robert Tscherny, Thilo BechstĂ€dt...Predicting discharge and sediment ïŹux of the Po River, Italy since the Last Glacial Maximum 171 Albert J. Kettner | | | Book (volume) | sediments from continental sources lying to the south, east and north. The southern and eastern sources...Devonian clastic sediments in a vast foreland basin south and southwest of the future Sverdrup Basin (Fig...clastics derived from the rising Brooks Ranges to the south, while. the northern clastic source was being rifted...accumulated within two depositional areas (Fig. 5): 1) a south-sloping stable platform (called here the Northern...southern Brooks Range to the south; and (2) an equally wide trough to the south (called here the Northern |
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