|Latitude & Longitude (WGS84):||48° 13' 6'' North , 15° 1' 28'' East|
|Latitude & Longitude (decimal):||48.21861,15.02472|
|Köppen climate type:||Cfb : Temperate oceanic climate|
|Name(s) in local language(s):||Steinbruch "In der Gleisen" (Yspertal; Ispertal; Unterfell), St. Oswald, Waldviertel, Niederösterreich, Österreich|
Abandoned quarry (quarries in fact) in pyrope-serpentinite.
Suggested as a minable occurrence of vermiculite (which occurs as lenticular bodies within the serpentinite).
Located east of Nöchling (but within the St. Oswald community), near the confluence of the rivers Große Ysper and Kleine Ysper.
17 valid minerals. 1 (TL) - type locality of valid minerals.
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
252.17 - 358.9 Ma
|Paleozoic intrusive rocks|
Age: Paleozoic (252.17 - 358.9 Ma)
Lithology: Intrusive igneous rocks
Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. 
|Silurian - Neoproterozoic|
419.2 - 1000 Ma
|Bohemian Massif (Böhmische Masse)|
Description: undifferentiated metamorphic
Reference: Asch, K. The 1:5M International Geological Map of Europe and Adjacent Areas: Development and Implementation of a GIS-enabled Concept. Geologisches Jahrbuch, SA 3.