Marble is in the carbonate mineral group. Limestone and dolomite are also in the carbonate mineral group. Marble is formed from limestone.
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 Marble have calcite in them.
Slate and marble are examples of metamorphic rocks. They are formed when existing rocks undergo high temperatures and pressures, causing them to recrystallize into new forms with different characteristics.
Limestone and dolostone can metamorphose into marble.
Examples of non-foliated metamorphic rocks are quartzite and marble.
metamorphic rock.
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 Rocks range from 4 to 5 on the Mohs scale
Marble is a metamorphic rock.
Carbonate rocks.
marble
Limestone or dolostone.
New York
Neither. The terms intrusive and extrusive apply to igneous rocks; marble is metamorphic.