"Glacier Moss" inspires with its wild mix of beige and green parts, which are characterized by dark veins. The quartzite processed in the STEINBILD "Glacier Moss" was formed about 350 million years ago, when due to the collision of two continents the Variscan mountain building took place.
 

History of origins

Each STEINBILD tells the probably oldest story in the world - our earth history

worldmap

At the time of the formation of the natural stone of this STEINBILD, a Variscan mountain building (collision of two continents) took place. This started the unfolding of the Rhenish slate mountains Harz and Eifel.

Mineralogy

At the end of the age, lush forests emerged with the first ancestors of conifers and the first seed plants. The primitive ferns (vascular plants) had already spread over a wide area. These were able to develop and spread quickly because there were no large herbivores at the time. At the same time, the ammonites were developing well.

350 million years

Rock age

 

Quartzite

Type of rock

 

Quartz, admixtures of colouring ores

Main constituent

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Developed and completed in Germany

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