Marble is in the carbonate mineral group. Limestone and dolomite are also in the carbonate mineral group. Marble is formed from limestone.
Limestone and marble belong to the carbonate mineral group. Limestone is primarily composed of calcite (calcium carbonate), while marble is a metamorphic rock that forms from the recrystallization of limestone under heat and pressure, also primarily consisting of calcite. Both are important sedimentary and metamorphic rocks used in construction and sculpture.
The group of rocks formed under high temperature and high pressure is called metamorphic rocks. These rocks are created when existing rocks, either igneous, sedimentary, or other metamorphic rocks, undergo metamorphism, resulting in changes to their mineral composition and texture. Common examples of metamorphic rocks include schist, gneiss, and marble.
Neither. The terms intrusive and extrusive apply to igneous rocks; marble is metamorphic.
Marble and quartzite are examples of massive metamorphic rocks that lack banding. Marble is formed from the metamorphism of limestone, while quartzite is formed from the metamorphism of sandstone. Both rocks typically have a uniform composition and lack the distinct layering or banding that is characteristic of other metamorphic rocks.
Marble is a metamorphic rock that typically does not have clearly defined layers like sedimentary rocks. However, some marbles may exhibit faint banding or veining due to variations in mineral composition or deformation during the rock's formation.
Limestone and dolostone can metamorphose into marble.
Examples of non-foliated metamorphic rocks are quartzite and marble.
These minerals belong to the carbonate mineral group. They are primarily composed of calcium carbonate (CaCO3) and form through the accumulation and compaction of organic remains in aquatic environments.
marble
metamorphic rock.
Marble Rocks range from 4 to 5 on the Mohs scale
Marble is a metamorphic rock.
The group of rocks formed under high temperature and high pressure is called metamorphic rocks. These rocks are created when existing rocks, either igneous, sedimentary, or other metamorphic rocks, undergo metamorphism, resulting in changes to their mineral composition and texture. Common examples of metamorphic rocks include schist, gneiss, and marble.
Carbonate rocks.
marble
Limestone or dolostone.
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