Locality type: | Quarry |
Classification |
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Species: | 'Scapolite' (not an IMA approved species) |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Scapolite data |
Locality Data: | Click here to view Neumühle quarry, Loistal, Schiltern, Langenlois, Krems-Land District, Lower Austria, Austria |
Data Identifiers |
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Mindat Occurrence Record ID: | 884358 |
Long-form Identifier: | 1:3:884358:6 |
GUID (UUID V4): | fe0e0376-fa5e-42c3-ab30-44dc3260822c |
Nearest other occurrences of Scapolite |
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7.0km (4.3 miles) | ⓘAltenhof, Stiefern, Schönberg am Kamp, Krems-Land District, Lower Austria, Austria |
16.7km (10.4 miles) | ⓘMalaschofsky Quarry, Lichtenau im Waldviertel, Krems-Land District, Lower Austria, Austria |
18.3km (11.4 miles) | ⓘScapolite occurrence, Tiefenbach, Krumau am Kamp, Krems-Land District, Lower Austria, Austria |
20.6km (12.8 miles) | ⓘWietzen, Lichtenau im Waldviertel, Krems-Land District, Lower Austria, Austria |
21.5km (13.3 miles) | ⓘMarble quarries (incl. Renz Quarry; Bundesheer Quarry), Winkl, Röhrenbach, Horn District, Lower Austria, Austria |
22.2km (13.8 miles) | ⓘRadlbachtal (Radlgraben; Huthof), Spitz, Krems-Land District, Lower Austria, Austria |
22.9km (14.2 miles) | ⓘRitzlinggraben, Laaben, Spitz, Krems-Land District, Lower Austria, Austria |
23.3km (14.5 miles) | ⓘSteiner quarry, Spitz, Krems-Land District, Lower Austria, Austria |
24.2km (15.0 miles) | ⓘSchwallenbach, Spitz, Krems-Land District, Lower Austria, Austria |
25.6km (15.9 miles) | ⓘMarble quarry, Atzelsdorf, Brunn an der Wild, Horn District, Lower Austria, Austria |
References |
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Reference Search (possible matching items) |
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| | Journal (article/letter/editorial) | eruption (bombs in agglomerate), normal flow of lava on land, viscous flow and fracturing of stiff lava, lava...spheroidal and ellipsoidal structure in the mining district of Saint Andreasberg, in the Harz Mountains. The...more chloritic in others, and at one place (near Neumühle) large spheroids are embedded in a light gray...rock being considered the equivalent of “only the lower layers of the volcanic caldron,” the upper portions...IS ---- O R IG IN O F P IL L O W LAVAS ably of Lower Arenig age. A close jointed dark gray chert occurs |
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