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Panská skála, Kamenický Šenov, Česká Lípa District, Liberec Region, Czech Republici
Regional Level Types
Panská skálaQuarry
Kamenický ŠenovMunicipality
Česká Lípa DistrictDistrict
Liberec RegionRegion
Czech RepublicCountry

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Latitude & Longitude (WGS84):
50° 46' 10'' North , 14° 29' 5'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Kamenický Šenov3,982 (2018)0.9km
Okrouhlá495 (2018)3.0km
Nový Oldřichov660 (2018)3.0km
Polevsko343 (2018)3.9km
Volfartice599 (2018)4.9km
Mindat Locality ID:
254292
Long-form identifier:
mindat:1:2:254292:1
GUID (UUID V4):
0
Name(s) in local language(s):
, Kamenický Šenov-Panská skála


Old basalt quarry.

The formation of Panská skála is connected with the impact of the continental African lithospheric plate into the European one, which led to alpine folds in the Mesozoic and Tertiary and reactivation of volcanism in this landscape due to the formation of new faults in the crust. Through these fractures, magma could flow to the surface again. In the area of ​​Panská skála, magma of basalt composition was pushed up about 30 million years ago, but it remained in a flue or supply channel and never reached the surface. The trapped magma began to cool very slowly, creating a typical detachment that can be observed today. In geomorphological division, the rock is part of the subunit of the Verneřický středohoří and the Benešovské středohoří district.

NOTE:
Remember to check Google Maps for additional, awesome pictures of this formation!

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Standard Detailed Gallery Strunz Chemical Elements

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List of minerals arranged by Strunz 10th Edition classification

Unclassified
ⓘ'Fayalite-Forsterite Series'-

Other Databases

Wikipedia:https://cs.wikipedia.org/wiki/Pansk%C3%A1_sk%C3%A1la
Wikidata ID:Q1426184

Other Regions, Features and Areas containing this locality

Czech Republic
Eurasian PlateTectonic Plate
EuropeContinent

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