The crust of our planet consists of the so-called platforms (relatively homogeneous, stable blocks) and folded zones, which differ from each other in age. If you look at the tectonic map of the world, you can see that the folding areas occupy no more than 20% of the Earth's surface. What is Hercynian folding? What is its time frame? And what mountain systems were formed in this era of tectogenesis? Our article will tell about it