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Pietra serena quarried in the Firenzuola
area is formed by clastic sedimentary rocks called sandstone.
Sandstone is a compact stone, so it is coherent.
The mechanism for the formation of sandstone is the sedimentation
(cementing, consolidation) of incoherent materials (fragments,
granules, clasts) called sand.
Sand, such as all the clastic materials, both big (gravel)
and smaller (clay, mud and silt), is formed by rock particles
that have been broken off the main rock, usually on the
earth surface. These rocks can be magmatic, sedimentary
and metamorphic.
Quarrying started in 15th century, but only with the use
of modern instruments and methodologies, the pietra serena
started to be widely used and spread.
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