|Latitude & Longitude (WGS84):||49° 28' 47'' North , 16° 14' 31'' East|
|Latitude & Longitude (decimal):||49.47996,16.24205|
|Other regions containing this locality:||Moravia (Mähren; Maehren), Czech Republic|
|Köppen climate type:||Cfb : Temperate oceanic climate|
|Name(s) in local language(s):||Kraj Vysočina|
The Rožná pegmatite is a classic locality studied from 18th century. It is located in Strážek Moldanubicum, along contact with the Svratka Unit, and it is hosted in migmatized biotite gneisses. The pegmatite dike is about 1 km long and 35 m wide. It was opened on the Hradisko hill, on the Borovina hill and in locality Rožná-north.
Lepidolite subtype pegmatite.
Mineral ListMineral list contains entries from the region specified including sub-localities
44 valid minerals. 1 (TL) - type locality of valid minerals. 1 erroneous literature entry.
Rock Types Recorded
Rock list contains entries from the region specified including sub-localities
Select Rock List TypeAlphabetical List Tree Diagram
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
541 - 1000 Ma
|Neoproterozoic crystalline metamorphic rocks|
Age: Neoproterozoic (541 - 1000 Ma)
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. 
541 - 4000 Ma
Age: Precambrian (541 - 4000 Ma)
Description: high grade 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.