A banded, compact variety of limestone called yellow travertine is frequently formed along rivers, near waterfalls, and in the vicinity of hot and cold springs in Iran. Carbon dioxide bubbles trapped during the stone's formation caused the holes in this travertine. It has an unfilled or naturally occurring open texture as a result. The majority of its colors are cream and tan, and it has a lineal (vein cut) or concentric (crosscut) appearance. Moreover, we now offer a line with darker veins. You
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