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Chalcedony from
Lower serpentinite quarry, Zwettler Leiten, Felling, Gföhl, Krems-Land District, Lower Austria, Austria


Locality type:Quarry
Classification
Species:Quartz var: Chalcedony
Formula:SiO2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Chalcedony data
Locality Data:Click here to view Lower serpentinite quarry, Zwettler Leiten, Felling, Gföhl, Krems-Land District, Lower Austria, Austria
Data Identifiers
Mindat Occurrence Record ID:1442920
Long-form Identifier:1:3:1442920:2
GUID (UUID V4):75087e88-c5b4-4eca-ae15-5323089178db
Nearest other occurrences of Chalcedony
0.8km (0.5 miles) Latzenhof, Felling, Gföhl, Krems-Land District, Lower Austria, Austria
2.9km (1.8 miles) Karaufeld, Felling, Gföhl, Krems-Land District, Lower Austria, Austria
3.6km (2.2 miles) Malaschofsky Quarry, Lichtenau im Waldviertel, Krems-Land District, Lower Austria, Austria
4.4km (2.7 miles) Klein-Heinrichschlag, Albrechtsberg an der Großen Krems, Krems-Land District, Lower Austria, Austria
11.5km (7.2 miles) Graphite quarry, Amstall, Mühldorf, Krems-Land District, Lower Austria, Austria
17.4km (10.8 miles) Quartz occurrence, Nonnersdorf, Maria Laach am Jauerling, Krems-Land District, Lower Austria, Austria
17.5km (10.9 miles) Nonnersdorf, Maria Laach am Jauerling, Krems-Land District, Lower Austria, Austria
18.6km (11.5 miles) Dürnitzbügel (Dürnitzbiegl; Dürnitzbühel), Schiltern, Langenlois, Krems-Land District, Lower Austria, Austria
20.9km (13.0 miles) Hohenwarthberg quarry, Schönbühel-Aggsbach, Melk District, Lower Austria, Austria
23.4km (14.5 miles) Winzing, Obritzberg-Rust, Sankt Pölten-Land District, Lower Austria, Austria
References
Reference Search (possible matching items)
Report (volume)
2 5 6 7 7 8 13 ........ ...... ....... 15 Serpentinite _____________________________ .. _ ..-- -. ...calculated for two alternative models of a magnetic serpentinite dike ________________________ 3-7. Maps showing:...another that is similar but structurally lower. Serpentinite, in tabular masses and in lenses, occurs...along high-angle faults. The most extensive serpentinite body follows a northwesttrending fault along...National Forest headquarters in Willows and at District Ranger Stations in Upper Lake and Stonyford. Well-maintained
 
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