what is yellow travertine ?

what is yellow travertine ?

Yellow travertine :

Travertine is a type of porous limestone that is considered a sedimentary and decorative stone.
These stones are left from the sediments of hot springs.
The cavities in these stones are a sediment source due to the space occupied by gases in hot water.
The fewer water-soluble elements in these sources, the lighter the color of the rock.
The amount of heat and height of the area also affects the quality of travertine.
Travertine has a porous texture and various colors and stripes, the color variation of which is due to differences in the compounds present at the time of deposition in the rock elements and manifest themselves in the form of different veins.

Golden Yellow travertine

travertine

top stones for flooring 

 

More about yellow travertine

The consumer should note that because these veins have a different chemical composition from the stone background, they have less strength in the rock and form the critical point of a rock that shows the least resistance to impact or pressure, and whatever stone has veins; the lower the impurities, the higher the strength.
Travertines are suitable for interior and exterior facades of buildings due to their very high porosity.
Travertines can be used in the building’s facade, even in icy and rainy areas, without worrying about dropping stones.

The interior view can also be referred to as:

Wall cornice
Stone next to the stairs
And…
Used depending on taste.

This stone is available in the form of cups, slabs, and tiles.
Yellow travertine is one of the most beautiful travertine stones.
This natural stone has irregular waves on its surface with brown and white streaks.
Yellow travertine mines are located in Azarshahr city of East Azerbaijan province, Mako city, Kashan city in Isfahan province.
Yellow travertine is a good choice for flooring in residential and office projects and is also used in building facades and wall coverings.
This stone is available in the form of cups, slabs, and tiles.

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