Limestone was probably metamorphed into marble.
Marble is a metamorphic rock so it was formed by heat and pressure. :)
No. Marble is metamorphosed limestone, recrystallized from heat, pressure, or both.
Marble is a metamorphic rock because it is formed from limestone that has been squeezed under pressure.
Some examples are probably slate, marble, quartzite.
Igneous rock is classified as extrusive or intrusive.
The original rock that was changed into marble by the addition of heat and pressure is likely limestone. Marble is a metamorphic rock that forms from the recrystallization of limestone under high heat and pressure conditions.
Schist and marble would be common examples.
Yes, marble can be changed by pressure and heat through a process called metamorphism. When subjected to high temperatures and pressures, the calcite or dolomite in marble can recrystallize, resulting in a denser and more durable rock. This process can also lead to the formation of new minerals and changes in texture. However, under typical conditions, marble is relatively stable and does not easily transform without significant geological forces.
This process is called metamorphism and it creates metamorphic rocks, such as marble.
Heat and pressure turn limestone into marble through the process of metamorphism, where the mineral composition and texture of the rock are changed. This transformation occurs as a result of high temperature and pressure altering the original calcium carbonate minerals of limestone into the interlocking crystals that characterize marble.
When limestone goes through heat and pressure, it becomes the metamorphic rock marble.
Marble is a metamorphic rock type form. Marble is used as a building material and as sculpture material also.
Marble is a metamorphic rock so it was formed by heat and pressure. :)
It is possible if the marble contains platy minerals like mica.
When rocks are changed by heat, pressure, or steam, they can undergo metamorphism. This process can produce new minerals, change the texture of the rock, and create foliation or banding. The end result can be metamorphic rocks such as marble, slate, or schist.
Heat and Pressure.
Marble was originally limestone, a sedimentary rock formed from the compression of shells, coral, and other calcium-rich materials. Through heat and pressure within the Earth's crust, the limestone was recrystallized into marble, a metamorphic rock with a distinctive crystalline structure and unique color variations.