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Secret Of Marble Formation in Mother Earth
Marble is one of the greatest gifts of nature. Inimitably precious and irresistibly intriguing, marble is perceived as the most precious material that fascinates with its distinctive characteristics, colors, patterns, texture and finesse. The formation of marble involves a series of complex strides and processes. It begins at the deepest quarters and crust of our planet Earth and ends with the execution of remarkable interior designs and décor concepts. From extraction to installation, turning raw marble into a masterpiece requires rigorous contemplation.

Admired and revered for its brilliant aesthetics and supreme grandeur, the marble formation begins with the phenomena within the crust entailing the fusion of various elements, energies and forces.

To enlighten you about the complexities, intricacies and practices from creation to finalization of marble into a stunning masterpiece, we bring to you a short sequential guide illustrating the entire process.

How Marble is Formed?

The formation occurs due to a reaction when limestone is subjected to intensive heat and pressure. The composition of marble consists of various minerals such as clay minerals, quartz, pyrite, micas, iron oxides and graphite, etc. but primarily the calcite. The phenomena of metamorphism involves recrystallization of calcite in the limestone leading to formation of rock that is a result of collective amalgamation of calcite crystals.

Extraction of Marble

Extraction process of marble is executed at the quarries in the rocky mountains. To perform efficient sourcing and carriage operations, professionals with tremendous expertise and highly sophisticated equipment are deployed. The pre-extraction arrangements also includes preparation for safety and preservation.

Extraction of Marble

Extraction process of marble is executed at the quarries in the rocky mountains. To perform efficient sourcing and carriage operations, professionals with tremendous expertise and highly sophisticated equipment are deployed. The pre-extraction arrangements also includes preparation for safety and preservation.

Pre-dispatch Procedures




You’ve Got It, You Flaunt It!
For people who love the modern styles of interior decoration, the clean and crisp styles with no over dose of gilded golden glitter scattered around in distracting fashion, like the contemporary and minimalist, beige floorings are perfect too. Flaunt the beauty of your home, you don’t need a rug for covering up floors that sparkle with magnificence.

Interiors So Lit!
Beige coloured floorings look demure. They reflect the light that falls on their gleaming surface with soft scattering-like effect that makes it amazingly easy on the eyes and essentially visually appealing. The aesthetics are an important part of interiors. They make your soul sing with adoration when you gaze upon a beautifully decorated home.

But, Oh! The Contrast!
Imagine magenta against beige, or textures of mahogany… envision pink flowers and violet drapes… visualise velvet green upholstered ottoman in front of a rocking chair in your favourite reading nook…

The point behind this imaginative mental exercise is that beige provides the best contrast there is. The regal front that it fosters is just a natural property of beige. Your furniture look outstanding, decorative objects and showpieces attain the right amount focus, and soft lights create a peaceful overall ambience.

You’ve Got It, You Flaunt It!
For people who love the modern styles of interior decoration, the clean and crisp styles with no over dose of gilded golden glitter scattered around in distracting fashion, like the contemporary and minimalist, beige floorings are perfect too. Flaunt the beauty of your home, you don’t need a rug for covering up floors that sparkle with magnificence.

Granite stone is often used in buildings, bridges, paving, monuments, countertops, tile floors, stair treads and many other design elements.The word granite has been derived from the Latin word ‘granum’ meaning grain. Granite is an intrusive, igneous rock with a granular and phaneritic texture, occupying 70-80% of the Earth’s crust. It is plutonic in origin, implying that it was formed deep underground. This rock is primarily composed of interlocking crystals of alkali feldspar (65% by volume), quartz (20% by volume), mica, amphiboles and other minerals. Depending on the mineral composition, the colour of granite can be red, pink, grey or white with dark mineral grains visible to the unaided eye. Granite is a hard and tough rock with an average density between 2.65 and 2.75 g/cm.

Location

It is found in abundance in all continents as part of the continental crust. This rock is found either in small, stock like masses spread over an area less than 100 km2 or as batholiths which are part of orogenic mountain ranges. Granite usually forms the base underground rock with other continental and sedimentary rocks resting over it. Granite also occurs in lacoliths, dikes and sills. Other rock variations, similar in composition to granite, are alpites and pegmatites. Alpites with finer grain size than granite, occur at the margins of granitic intrusions. Pegmatites with coarser grains than granite often share locations with granite deposits.

Formation

There are several controversial theories regarding the origin of granite. The most widely propagated ones are the magmatic theory and the hypermetamorphic theory. According to the magmatic theory, plutonic rocks like granite, which are often found associated with mountain ranges, originated from magma. It is believed that during the formation of mountains, when one continental edge subdues another one below it, the pressure and frictional forces generated by this phenomenon is sufficient to melt the rocks underneath the subdued continental edge. This melted rock or magma seeps up in the form of large globules or plutons. It takes an extremely long time for the plutons to arrive at the surface of the earth and to be converted into a surface rock, the pluton must be eroded by the weathering forces acting on the ground. This could be one of the processes by which granite formation takes place. The hypermetamorphic theory, however, disregards the magmatic theory and instead propagates that granite is the result of melting and re-crystallization of sedimentary rock instead of magma. However, as of yet, the precise method of granite formation, is still under research till a conclusive proof of formation of this rock is attained.