Pure Cordillera
| Age: | 380 |
|---|---|
| Alignment: | Square |
| Butterfly: | No |
| Geometry: | Stained |
| Shade: | Black, Gray, White |
| Size category: | L |
| Topics: | Ice, Waters, Winter |
At the time of the formation of the natural stone of this STEINBILD a Variscan mountain building (collision of two continents) took place. This began the unfolding of the Rhenish slate mountains Harz and Eifel.
Mineralogy
At the end of the age üppige forests arose with the first ancestors of coniferous trees and the first seed plants. The primitive ferns (vascular plants) were already widely spread. They were able to develop and spread quickly, since there were no large herbivores at that time. At the same time the ammonites developed well.
380 million years
Age of rock
Marble
Type of stone
Magnesium, silicon, calcium, iron
Main component
At the time of the formation of the natural stone of this STEINBILD a Variscan mountain building (collision of two continents) took place. This began the unfolding of the Rhenish slate mountains Harz and Eifel.
Mineralogy
At the end of the age üppige forests arose with the first ancestors of coniferous trees and the first seed plants. The primitive ferns (vascular plants) were already widely spread. They were able to develop and spread quickly, since there were no large herbivores at that time. At the same time the ammonites developed well.
380 million years
Age of rock
Marble
Type of stone
Magnesium, silicon, calcium, iron
Main component