"Colligatio Vermilion Cliffs" is distinguished by the bright red coloration in the basic tone, which makes it even more unique combined with the fine, dark veining. The quartzite processed in the STEINBILD "Colligatio Vermilion Cliffs" was formed about 600 million years ago, when the supercontinent Rodinia newly formed into the supercontinent Pannotia.
 

History of origins

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

worldmap

The supercontinent Rodinia reformed again to form the last Neoproterozoic supercontinent Pannotia, also called Great Gondwana.

Mineralogy

Photosynthesis had almost completely stopped due to the ice age. Therefore, only microscopic plant life can be assumed at this time. In the fauna, the earliest known representative of the Bilateria (two-sided animals) appeared.

600 million years

Rock age

 

Quartzite

Type of rock

 

Quartz, admixtures of colouring ores

Main constituent

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