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from the Upper Silurian age
It rarely occurs in crystal form but is often found in botryoidal or fibrous formations
which over the course of millions of years becomes solid while retaining the semitransparent yellowish hue of tree sap
red and many other colors corresponding to their physical makeup and conditions when the mineral was formed
A widespread and industrially important mineral
Petrified Coral Malachite from the Upper Silurian age
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