Clays would become shale, then metamorphose into slate with heat and pressure.
If limestone undergoes contact metamorphism, it will typically turn into marble. Marble forms from the recrystallization of limestone under high temperature and pressure conditions.
Clay can turn into limestone through a process called diagenesis, where the clay particles are subjected to compaction and cementation, forming a new rock material. Over time, the minerals in the clay are altered and precipitate out to form calcium carbonate, which is the primary mineral in limestone.
Marble can turn back into limestone through a process called metamorphism. When subjected to high pressure and temperature underground over long periods of time, the minerals in marble can recrystallize and rearrange to form limestone. This transformation occurs in the Earth's crust, where the conditions favor the alteration of marble back into limestone.
Limestone typically turns into marble when subjected to heat and pressure. Marble is a metamorphic rock with a finer texture and often exhibits a wider range of colors than limestone.
Limestone is the parent rock of marble. The word marble can be used to refer to both metamorphosed and unmetamorphosed limestone.
No. Limestone turns into marble, not sandstone.
If limestone undergoes contact metamorphism, it will typically turn into marble. Marble forms from the recrystallization of limestone under high temperature and pressure conditions.
Clay can turn into limestone through a process called diagenesis, where the clay particles are subjected to compaction and cementation, forming a new rock material. Over time, the minerals in the clay are altered and precipitate out to form calcium carbonate, which is the primary mineral in limestone.
Marble can turn back into limestone through a process called metamorphism. When subjected to high pressure and temperature underground over long periods of time, the minerals in marble can recrystallize and rearrange to form limestone. This transformation occurs in the Earth's crust, where the conditions favor the alteration of marble back into limestone.
Limestone can turn into the metamorphic rock called marble through a process of metamorphism involving high pressure and high temperature.
Limestone typically turns into marble when subjected to heat and pressure. Marble is a metamorphic rock with a finer texture and often exhibits a wider range of colors than limestone.
Marble is metamorphosed limestone.
Marble is made from limestone.
Marble is not made from igneous rock. Marble is a metamorphic rock made from either limestone or dolormite. Its texture is non-foliated. Non-foliated metamorphic rocks are those which either receive equal pressure from all sides as they form, or they are those which were formed from minerals that did not have any distinct patterns of growth. Pure marble is white. The swirling and splotches of color in marble come from substances such as clay, sand, and silt in the limestone. So as the limestone is changing into marble, the clay, sand, silt and other elements in the limestone become swirls or splotches of color.
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.
Marble is metamorphosed limestone or dolostone.
Pure marble is the result of metamorphism of a very pure limestone or dolomite. Colored marble varieties are usually due to various mineral impurities such as clay, silt, sand, iron oxides, or chert which were originally grains or layers in the limestone.