northern bohemia panska skala basalt organ

navigate by keyword : rock wall terrain northern bohemia pansk basalt organ panska skala connected collision continental lithospheric european mesozoic tertiary periods reactivation volcanism landscape magma surface million composition forced area spilled chalky bedrock lava began cool slowly zlom africk

Northern Bohemia, Panska skala, basalt organ Royalty Free Stock Photo
Northern Bohemia, Panska skala, basalt organ Royalty Free Stock Photo
Northern Bohemia, Panska skala, basalt organ Royalty Free Stock Photo
Northern Bohemia, Panska skala, basalt organ Royalty Free Stock Photo
Unique basalt organ pipes of Panska skala near Kamenicky Senov in Northern Bohemia, Czech Republic Royalty Free Stock Photo
Basalt rock Panska Skala, Czech republic Royalty Free Stock Photo
Basalt rock Panska Skala, Czech republic Royalty Free Stock Photo
Northern Bohemia, Panska skala, basalt organ
Unique basalt organ pipes of Panska skala near Kamenicky Senov in Northern Bohemia, Czech Republic Royalty Free Stock Photo
Unique basalt organ pipes of Panska skala near Kamenicky Senov in Northern Bohemia, Czech Republic Royalty Free Stock Photo
Rock formation natural monument Basalt organ. Polygonal structures of basalt columnar separation in Panska skala near Kamenicky Royalty Free Stock Photo
Rock formation natural monument Basalt organ. Polygonal structures of basalt columnar separation in Panska skala near Kamenicky Royalty Free Stock Photo
Rock formation natural monument Basalt organ. Polygonal structures of basalt columnar separation in Panska skala near Kamenicky Royalty Free Stock Photo
Rock formation natural monument Basalt organ. Polygonal structures of basalt columnar separation in Panska skala near Kamenicky Royalty Free Stock Photo
Rock formation natural monument Basalt organ. Polygonal structures of basalt columnar separation in Panska skala near Kamenicky Royalty Free Stock Photo
The formation of Panska skala is connected with the collision of the continental African lithospheric plate with the European one, which led in the Mesozoic and Tertiary periods to Alpine folding and the reactivation of volcanism in this landscape due to the formation of new fractures in the crust. Through these fractures, magma could flow again to the surface. Around 30 million years ago, magma of a basalt composition was forced upwards in the area of Panská skály, which spilled over the chalky bedrock as a lava flow. The lava flow began to cool slowly, which began to form the typical cleavage that can be observed today.


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