What is Marble?
Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism.
It is composed primarily of the mineral calcite (CaCO3) and usually contains other minerals such as: clay minerals, micas, quartz, pyrite, iron oxides and graphite. Under the conditions of metamorphism the calcite in the limestone recrystallizes to form a rock that is a mass of interlocking calcite crystals. A related rock, dolomitic marble, is produced when
dolostone is subjected to heat and pressure.
Photo Gallery: The Many Uses of Marble
How Does Marble Form?
Most marble forms at convergent plate boundaries where large areas of Earth's crust are exposed to regional
metamorphism. Some marble also forms by contact metamorphism when a hot magma body heats adjacent limestone or
Before metamorphism, the calcite in the limestone is often in the form of lithified fossil material and biological debris.
During metamorphism, this calcite recrystallizes and the texture of the rock changes. In the early stages of the
limestone-to-marble transformation the calcite crystals in the rock are very small. In a freshly-broken hand
specimen they might only be recognized as a sugary sparkle of light reflecting from their tiny cleavage faces when the rock is played in the light.
As metamorphism progresses the crystals grow larger and become easily recognizable as interlocking crystals of calcite.
Recrystallization obscures the original fossils and sedimentary structures of the limestone. It also occurs without forming
foliation which normally is found in rocks that are altered by the directed pressure of a convergent plate boundary.
Recrystallization is what marks the separation between limestone and marble. Marble that has been exposed to low levels of
metamorphism will have very small calcite crystals. The crystals become larger as the level of metamorphism progresses.
Clay minerals within the marble will alter to micas and more complex silicate structures as the level of metamorphism increases.
Physical Properties and Uses of Marble
Marble occurs in large deposits that can be hundreds of feet thick and geographically extensive. This allows it to be
economically mined on a large scale with some mines and quarries producing millions of tons per year.
Most marble is made into either crushed stone or dimension stone. Crushed stone is used as an aggregate in highways, railroad beds, building foundations and other types of construction. Dimension stone is produced by sawing marble into pieces of specific dimensions. These are used in monuments, buildings, sculptures, paving and
We have an article about "the uses of marble" that includes photos and descriptions of marble in many types of use.
Color: Marble is usually a light-colored rock. When it is formed from a limestone with very few
impurities it will be white in color. Marble that contains impurities such as clay minerals, iron oxides or bituminous
material can be bluish, gray, pink, yellow or black in color.
Marble of extremely high purity with a bright white color is very useful. It is often mined, crushed to a powder and then
processed to remove as many impurities as possible. The resulting product is called "whiting". This powder is used as a
coloring agent and filler in paint, whitewash, putty, plastic, grout, cosmetics, paper and other manufactured products.
Acid Reaction: Being composed of calcium carbonate, marble will react in contact with many acids,
neutralizing the acid. It is one of the most effective acid neutralization materials. Marble is often crushed and used for
acid neutralization in streams, lakes and soils.
It is used for acid neutralization in the chemical industry. A pharmaceutical product known as "Tums" is a small calcium
carbonate pill, sometimes made from powdered marble, that is used by people who suffer from acid reflux or acid indigestion.
Powdered marble is used as an inert filler in other pills.
Hardness: Being composed of calcite, marble has a hardness of three on the
Mohs hardness scale. As a result, marble is easy to
carve and that makes it useful for producing sculptures and ornamental objects. The translucence of marble makes it
especially attractive for many types of sculptures.
The low hardness and solubility of marble allows it to be used as a calcium additive in animal feeds. Calcium additives are especially important for dairy cows and egg-producing chickens. It is also used as a low
hardness abrasive for scrubbing bathroom and kitchen fixtures.
Ability to Accept a Polish: After being sanded with progressively finer abrasives, marble can be
polished to a high luster. This allows attractive pieces of marble to be cut, polished and used as floor tiles, architectural
panels, facing stone, window sills, stair treads, columns and many other pieces of decorative stone.
Another Definition of Marble
The name "marble" is used in a different way in the dimension stone trade. Any crystalline carbonate rock that has an
ability to accept a polish is called "marble". The name is sometimes used for other soft rocks such as travertine, verd antique,
serpentine and some limestones.
Contributor: Hobart King
Find it on Geology.com
More from Geology.com
|Free Google Earth software allows you to browse seamless world satellite images. Free.
|Gems from Space A number of materials from space have been used as attractive gems.
|Spodumene - an ore of lithium and the mineral of the gems kunzite and hiddenite.
|Ant Hill Garnets are tiny garnets that ants haul to the surface and discard on their anthill. Honest!
|Wall Maps - World maps, United States maps, continent maps, maps of individual states.
|Fee Mining sites are mines that you can enter, pay a fee, and keep anything that you find.
|Pink Marble: A piece of pink marble about four inches (ten centimeters) across. The pink color is most likely derived from iron. Image by NASA.
|Ruby in Marble: Marble is often the host rock for corundum, spinel and other gem minerals. This specimen is a piece of white marble with a large red ruby crystal from Afghanistan. Specimen is about 1 1/4 inches across (about 3 centimeters). Specimen and photo by Arkenstone / www.iRocks.com.
|Gray Marble: This specimen has calcite cleavage faces up to several millimeters in size that are reflecting light. This specimen shown is about two inches (five centimeters) across.|