== Limestone, dolomite and marble are carbonate rocks.
The two rocks that are primarily composed of a mineral that bubbles with acid are limestone and marble.
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.
Calcite is the mineral commonly found in both limestone and marble. Both rocks are formed primarily from calcite crystals.
Marble, the rock, is metamorphic. From limestone.
The parent rock of marble can be composed of calcite or dolomite. Thus, it can be one of several rock types, often limestone (though it can conceivably also be dolomite or travertine, etc.). Limestone is considered to be the most common parent rock of marble. Since it is composed of calcite, it can be tested with dilute hydrochloric acid. If it bubbles, it is composed of calcite, and is probably marble.
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.
Marble is a metamorphic rock. It is a metamorphism of limestone or dolostone and contains calcite and dolomite.
calcite and dolomite.
The protolith of marble was limestone or dolomite.
The protolith of marble was limestone or dolomite.
A metamorphic form of limestone is marble.
Marble is in the carbonate mineral group. Limestone and dolomite are also in the carbonate mineral group. Marble is formed from limestone.
The two rocks that are primarily composed of a mineral that bubbles with acid are limestone and marble.
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.
marble
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.
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.