"Mountain Spring" captivates with its strong wave-like structures in subtle shades of blue, which came about due to the subduction of the Pacific plates at that time. The quartzite processed in the STEINBILD "Mountain Spring" was formed about 150 million years ago during the Pangaea era.

History of origins

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

worldmap

At the time when the natural stone of this STEINBILD was formed, mountain building took place around the Pacific Ocean. Subduction of the Pacific plates started the unfolding of the Andes. Regression in Central Europe due to the recession of the sea. Pangaea finally broke apart.

Mineralogy

The first flowering plants emerged and the high rainfall ensured expansion of the plant world. This created dense, lush tropical forests with more flowering plants. Due to the strong reef formation, hexacorals, mussels, crinoids and echinoderms appeared. In addition, the Archaeopteryx (prehistoric bird) is well developed with feathers and skeleton during this time.

150 million years

Rock age

 

Quartzite

Type of rock

 

Quartz, admixtures of colouring ores.

Main constituent

Made in Germany

Developed and completed in Germany

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30 days return policy

Free return if the STEINBILD does not convince you

Assembly service

Have your unique STONE IMAGE professionally mounted