The taj mahal is entirely clad in marble.
Composition of marble in taj mahal.
It is built of pure white marble and looks magnificent on a full moon night.
Taj mahal quartzite is a pristine countertop material that s able to fit into a wide variety of design style s due to its white base and brown veins.
The taj mahal is a perfect symmetrical planned building with an emphasis of bilateral symmetry along a central axis on which the main features are placed.
It would look stunning as a kitchen countertop or island top while giving off a luxurious beauty that we all seek in marble.
It also houses the tomb of shah jahan himself.
One day with my uncle i wished to see the building.
It was commissioned in 1632 by the mughal emperor shah jahan reigned from 1628 to 1658 to house the tomb of his favourite wife mumtaz mahal.
The complex houses the tombs of shah jahan and one of his wives known as mumtaz mahal.
Still it is one of the most beautiful buildings of the world.
In the art world the technical name of the artwork carried in the taj mahal is pietra dura.
The glistening effect created by the translucent marble is well described by kalim a mughal court poet who wrote that the taj resembles dawn s bright face.
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The marble inlay art of the taj mahal is a masterpiece and it will be an eye grabbing decorative element.
Marble is typically not foliated although there are exceptions.
Today its stunning architecture has made it one of the most iconic monuments in the world.
It looked grand and impressive.
The external decorations of the taj mahal are the perfect example for the beautiful mughal art.
The building material used is brick in lime mortar veneered with red sandstone and marble and inlay work of precious semi precious stones.
Crown of the palace taːdʒ ˈmɛːɦ ə l is an ivory white marble mausoleum on the southern bank of the river yamuna in the indian city of agra.
Taj mahal mausoleum complex in uttar pradesh in northern india built by the mughal emperor shah jahan in the 17th century.
Marble is a metamorphic rock composed of recrystallized carbonate minerals most commonly calcite or dolomite.