The product of the old limestone springs is seen in relatively large areas. In most cases, the layers are located in the reserves of this rock or with a gentle slope that is subjected to the surface morphology. So that in some cases, huge deposits are deposited in vast areas. Like the huge mines of Azar Shahr and neighborhoods, white travertine is of a higher quality if its color is uniformly white and colored and ductile. The sale of this stone from the mines of the neighborhoods, which are of great quality, are unsurpassed. Of course, the presence of colored veins caused by the contamination of iron oxides in white travertine may give a special stone.
The stone has a porous texture and a variety of stripes of different colors, due to the difference in the composition that occurs during the sedimentation of the stone elements and shows itself in various veins. It should be noted that because these veins have a different chemical composition than the rocky field, they have less firmness in the rock formed and constitute the sensitive point of a rock that exhibits the least resistance against impact or pressure, and the stone has streaks And fewer impurities, it has a higher strength.
These rocks are based on the type of incisional and non-wavy slabs based on their shape and their minerals and their characteristics in different types such as:
Travertine Abbas Abad, Maku, Mahabad, Dasheir, Isfahan, Yazd Abyaneh, Abarkuh, Travertine Eghlid and …
These rocks can be used even in very cold and rainy areas on the facade of the building without worrying about rolling the stone.
In the interior view, you can also:
- Wall bracket, rock mass and …