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Marble has a crystalline texture of visible interlocked calcite or dolomite mineral grains.

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What does marble have instead of grains?

Marble does not have grains like other rock types. Instead, marble has a crystalline structure that forms as a result of the metamorphism of limestone. This structure gives marble its characteristic veining and smooth texture.


What is the structure of marble?

Marble is a metamorphic rock primarily composed of recrystallized calcite or dolomite minerals. It typically has interlocking, coarse-grained crystals that give it a distinctive veined appearance. This structure allows marble to be polished to a high luster, making it a popular choice for decorative purposes.


What is the grain shape of marble?

The grain shape of marble is typically interlocking. This means that the individual mineral grains in the marble are tightly interwoven or interlocked with each other, forming a solid and dense structure.


A metamorphic rock made from limestone?

Marble is a metamorphic rock formed from limestone that has undergone intense heat and pressure deep within the Earth's crust. The process of metamorphism recrystallizes the original minerals in limestone to create the distinct crystalline structure and smooth texture of marble. Marble is valued for its beauty and is commonly used in architecture and sculpture.


What element is the metallic component of the mineral marble?

The metallic component of marble is primarily calcium, which is present as the mineral calcite. This gives marble its characteristic white color and distinctive crystal structure. Other elements present in marble include magnesium, iron, and trace amounts of other elements.

Related Questions

What does marble have instead of grains?

Marble does not have grains like other rock types. Instead, marble has a crystalline structure that forms as a result of the metamorphism of limestone. This structure gives marble its characteristic veining and smooth texture.


Is corrosion of marble is a chemical or physical change?

Corrosion of marble is a chemical change. It occurs when the minerals in the marble undergo a chemical reaction with substances like acids or salts, leading to the deterioration of the marble's structure.


What is the crystal system of marble?

it has a very tight crystalline structure and small but definite porosity


Why is marble not considered a mineral?

Because Glass doesn't have a crystal structure.


What is the structure of marble?

Marble is a metamorphic rock primarily composed of recrystallized calcite or dolomite minerals. It typically has interlocking, coarse-grained crystals that give it a distinctive veined appearance. This structure allows marble to be polished to a high luster, making it a popular choice for decorative purposes.


What is the most distinctive physical property for marble?

I think to structure, hardness and color.


What is the structure of the The Taj Mahal?

It is made of white marble and many gems are put in it


What is the grain shape of marble?

The grain shape of marble is typically interlocking. This means that the individual mineral grains in the marble are tightly interwoven or interlocked with each other, forming a solid and dense structure.


What is the lustre of marble?

Marble does not have a lustre because it is not a mineral


What does marble metemorphosize from?

Limestone/chalk. Limestone has been subjected to heat and/or pressure, it metamorposes into marble. Both limestone and marble are calcium carbonate (CaCO3). Its just that the internal physical structure of limestone is altered.


Why marble is not a mineral?

Marble is in fact a type of metamorphic rock. Rocks are aggregate of one or many different kinds of minerals with no definite chemical composition and a specific crystalline structure that all minerals have, so marble is not a mineral.


What temperature does marble form?

Marble forms from limestone, which undergoes metamorphism at temperatures between 400-800 degrees Celsius and pressures of 1500-5000 bars. This process results in the recrystallization of the parent rock into marble, with a distinctive crystalline structure.