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== Limestone, dolomite and marble are carbonate rocks.

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What is the metamorphosed form of dolomite?

The metamorphosed form of dolomite is called marble. Dolomite is a sedimentary rock primarily composed of the mineral dolomite, while marble is a metamorphic rock that forms from the recrystallization of limestone or dolomite under high heat and pressure.


How did marbles start?

Marble is a metamorphic rock. It is a metamorphism of limestone or dolostone and contains calcite and dolomite.


What is limestone to marble?

calcite and dolomite.


What was formed?

The protolith of marble was limestone or dolomite.


What was formed from?

The protolith of marble was limestone or dolomite.


What mineral forms stalactites and stalagmites?

A metamorphic form of limestone is marble.


What group of rocks is marble in?

Marble is in the carbonate mineral group. Limestone and dolomite are also in the carbonate mineral group. Marble is formed from limestone.


Which two rocks are primarily composed of a mineral that bubbles with acid?

The two rocks that are primarily composed of a mineral that bubbles with acid are limestone and marble.


What is marble composed of?

Marble is primarily composed of calcium carbonate, which is derived from the metamorphism of limestone. It is created through the recrystallization of the original carbonate mineral grains. Marble often contains other minerals that give it its distinctive color and veining patterns.


What kind of rock is formed by metamorphism of limestone or dolomite?

marble


What causes marble to be different colors?

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.


How did marble start out?

Marble is a metamorphic rock that begins as limestone, a sedimentary rock composed mostly of calcite. Over time, the limestone is subjected to heat and pressure deep within the Earth's crust, causing it to recrystallize and form marble.