Marble has a crystalline texture of visible interlocked calcite or dolomite mineral 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.
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.
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.
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.
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.
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.
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.
it has a very tight crystalline structure and small but definite porosity
Because Glass doesn't have a crystal structure.
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.
I think to structure, hardness and color.
It is made of white marble and many gems are put in it
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.
Marble does not have a lustre because it is not a mineral
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.
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.
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.