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Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or Dolomite (mineral), dolomite. Marble is typically not Foliation (geology), foliated (layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. Marble is commonly used for Marble sculpture, sculpture and as a building material.
The word "marble" derives from the Ancient Greek (), from (), "crystalline rock, shining stone", perhaps from the verb (), "to flash, sparkle, gleam"; Robert S. P. Beekes, R. S. P. Beekes has suggested that a "Pre-Greek origin is probable".
This Stem (linguistics), stem is also the ancestor of the English language, English word "marmoreal," meaning "marble-like." While the English term "marble" resembles the French language, French , most other European languages (with words like "marmoreal") more closely resemble the original Ancient Greek.
Examples of historically notable marble varieties and locations:
According to the United States Geological Survey, U.S. domestic marble production in 2006 was 46,400 tons valued at about $18.1 million, compared to 72,300 tons valued at $18.9 million in 2005. Crushed marble production (for aggregate and industrial uses) in 2006 was 11.8 million tons valued at $116 million, of which 6.5 million tons was finely ground calcium carbonate and the rest was construction aggregate. For comparison, 2005 crushed marble production was 7.76 million tons valued at $58.7 million, of which 4.8 million tons was finely ground calcium carbonate and the rest was construction aggregate. U.S. dimension marble demand is about 1.3 million tons. The DSAN World Demand for (finished) Marble Index has shown a growth of 12% annually for the 2000–2006 period, compared to 10.5% annually for the 2000–2005 period. The largest dimension marble application is tile.
In 1998, marble production was dominated by 4 countries that accounted for almost half of world production of marble and decorative stone. Italy and China were the world leaders, each representing 16% of world production, while Spain and India produced 9% and 8%, respectively.
In 2018 Turkey was the world leader in marble export, with 42% share in global marble trade, followed by Italy with 18% and Greece with 10%. The largest importer of marble in 2018 was China with a 64% market share, followed by India with 11% and Italy with 5%.
As the favorite medium for Greek and Roman sculptors and architects (see classical sculpture), marble has become a cultural symbol of tradition and refined taste. Its extremely varied and colorful patterns make it a favorite decorative material, and it is often imitated in background patterns for computer displays, etc.
Places named after the stone include Marblehead, Massachusetts; Marblehead, Ohio; Marble Arch, London; the Sea of Marmara; India's Marble Rocks; and the towns of Marble, Minnesota; Marble, Colorado; Marble Falls, Texas, and Marble Hill, Manhattan, New York. The Elgin Marbles are marble sculptures from the Parthenon in Athens that are on display in the British Museum. They were brought to Britain by the Thomas Bruce, 7th Earl of Elgin, Earl of Elgin.
File:Nike of Samothrake Louvre Ma2369 n4.jpg, The Winged Victory of Samothrace, Nike of Samothrace is made of Parian marble (c. 220–190 BC)
File:Laocoon Pio-Clementino Inv1059-1064-1067.jpg, ''Laocoön and His Sons'' in the Vatican Museums, Vatican
File:Treasury_Gate,_Dolmabahçe_Palace,_Istanbul,_Turkey_001.jpg, Dolmabahçe Palace in Istanbul
File:Lens - Inauguration du Louvre-Lens le 4 décembre 2012, la Galerie du Temps, n° 058.JPG, The Praetorians Relief, made from grey veined marble, AD
File:Imgp7544.jpg, Ancient marble columns in the prayer hall of the Mosque of Uqba, in Kairouan, Tunisia
File:Cleopatra by William Wetmore Story 03.jpg, ''Cleopatra'' by William Wetmore Story was described and admired in Nathaniel Hawthorne's romance, ''The Marble Faun'', and is on display at The Metropolitan Museum of Art in New York City.
File:Per Hasselberg Näckrosen Rottneros Park.jpg, ''Näckrosen'' (Water Lily), Stockholm 1892, by Swedish sculptor Per Hasselberg (1850-1894). Here a copy from 1953 in marble by Giovanni Ardini (Italy) placed in Rottneros Park near Sunne, Sweden, Sunne in Värmland/Sweden.
File:Pažaislis Monastery interior 1, Kaunas, Lithuania - Diliff.jpg, Pažaislis Monastery complex has the most marble-decorated Baroque church of the Grand Duchy of Lithuania
File:Petropolis-Cathedral1.jpg, The tombs of Emperor Pedro II of Brazil and other members of the Brazilian imperial family, made from Carrara marble in the Cathedral of Petrópolis, Brazil
Dimension Stone Statistics and Information
– United States Geological Survey minerals information for dimension stone
USGS 2005 Minerals Yearbook: Stone, CrushedUSGS 2005 Minerals Yearbook: Stone, DimensionUSGS 2006 Minerals Yearbook: Stone, CrushedUSGS 2006 Minerals Yearbook: Stone, DimensionMarble Institute of America
{{Authority control Marble, Sculpture materials Metasedimentary rocks Limestone Stone (material) Symbols of Alabama
Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or Dolomite (mineral), dolomite. Marble is typically not Foliation (geology), foliated (layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphosed limestone, but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. Marble is commonly used for Marble sculpture, sculpture and as a building material.
Etymology
The word "marble" derives from the Ancient Greek (), from (), "crystalline rock, shining stone", perhaps from the verb (), "to flash, sparkle, gleam"; Robert S. P. Beekes, R. S. P. Beekes has suggested that a "Pre-Greek origin is probable".
This Stem (linguistics), stem is also the ancestor of the English language, English word "marmoreal," meaning "marble-like." While the English term "marble" resembles the French language, French , most other European languages (with words like "marmoreal") more closely resemble the original Ancient Greek.
Physical origins
Marble is a rock resulting from metamorphism of sedimentary rock, sedimentary carbonate rocks, most commonly limestone or Dolomite (rock), dolomite (rock). Metamorphism causes variable recrystallization of the original carbonate mineral grains. The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals. Primary sedimentary textures and structures of the original carbonate rock (protolith) have typically been modified or destroyed. Pure white marble is the result of metamorphism of a very pure (Silicate minerals, silicate-poor) limestone or dolomite protolith. The characteristic swirls and Vein (geology), veins of many colored marble varieties are usually due to various mineral impurities such as clay, silt, sand, iron oxides, or chert which were originally present as grains or layers in the limestone. Green coloration is often due to Serpentine group, serpentine resulting from originally magnesium-rich limestone or dolomite with silica impurities. These various impurities have been mobilized and recrystallized by the intense pressure and heat of the metamorphism.Types
Examples of historically notable marble varieties and locations:
Uses
Sculpture
White marble has been prized for its use in marble sculpture, sculptures since Classical antiquity, classical times. This preference has to do with its softness, which made it easier to carve, relative isotropy and homogeneity, and a relative resistance to shattering. Also, the low Refractive index, index of refraction of calcite allows light to penetrate 12.7 to 38 millimeters into the stone before being scattered out, resulting in the characteristic waxy look which brings a lifelike luster to marble sculptures of any kind, which is why many sculptors preferred and still prefer marble for sculpting.Construction
Construction marble is a stone which is composed of calcite, Dolomite (mineral), dolomite or serpentine that is capable of taking a polish. More generally in construction, specifically the dimension stone trade, the term ''marble'' is used for any crystalline calcitic rock (and some non-calcitic rocks) useful as building stone. For example, Tennessee marble is really a dense granular fossiliferous gray to pink to maroon Ordovician limestone, that geologists call the Holston Formation. Ashgabat, the capital city of Turkmenistan, was recorded in the 2013 ''Guinness Book of Records'' as having the world's highest concentration of white marble buildings.Production
According to the United States Geological Survey, U.S. domestic marble production in 2006 was 46,400 tons valued at about $18.1 million, compared to 72,300 tons valued at $18.9 million in 2005. Crushed marble production (for aggregate and industrial uses) in 2006 was 11.8 million tons valued at $116 million, of which 6.5 million tons was finely ground calcium carbonate and the rest was construction aggregate. For comparison, 2005 crushed marble production was 7.76 million tons valued at $58.7 million, of which 4.8 million tons was finely ground calcium carbonate and the rest was construction aggregate. U.S. dimension marble demand is about 1.3 million tons. The DSAN World Demand for (finished) Marble Index has shown a growth of 12% annually for the 2000–2006 period, compared to 10.5% annually for the 2000–2005 period. The largest dimension marble application is tile.
In 1998, marble production was dominated by 4 countries that accounted for almost half of world production of marble and decorative stone. Italy and China were the world leaders, each representing 16% of world production, while Spain and India produced 9% and 8%, respectively.
In 2018 Turkey was the world leader in marble export, with 42% share in global marble trade, followed by Italy with 18% and Greece with 10%. The largest importer of marble in 2018 was China with a 64% market share, followed by India with 11% and Italy with 5%.
Occupational safety
Dust produced by cutting marble could cause lung disease but more research needs to be carried out on whether dust filters and other safety products reduce this risk. In the United States, the Occupational Safety and Health Administration (OSHA) has set the legal limit (permissible exposure limit) for marble exposure in the workplace as 15 mg/m3 total exposure and 5 mg/m3 respiratory exposure over an 8-hour workday. The National Institute for Occupational Safety and Health (NIOSH) has set a recommended exposure limit (REL) of 10 mg/m3 total exposure and 5 mg/m3 respiratory exposure over an 8-hour workday.Degradation by acids
Acids damage marble, because the calcium carbonate in marble reacts with them, releasing carbon dioxide (technically speaking, carbonic acid, but that decomposes quickly to CO2 and H2O) and other soluble salts : :CaCO3(s) + 2H+(aq) → Ca2+(aq) + CO2(g) + H2O (l) Thus, vinegar or other acidic solutions should never be used on marble. Likewise, outdoor marble statues, headstone, gravestones, or other marble structures are damaged by acid rain whether by carbonation, sulfation or the formation of "black-crust" (accumulation of calcium sulphate, nitrates and carbon particles).Crystallization
Crystallization refers to a sometimes controversial method of imparting a glossy more durable finish on to a marble floor (CaCO3). It involves polishing the surface with an acidic solution and a steel wool pad on a flooring machine. The chemical reaction below shows a typical process using magnesium fluorosilicate (MgSiF6) and hydrochloric acid (HCl) taking place. :CaCO3(s) + MgSiF6(l) + 2HCl (l) → MgCl2(s) + CaSiF6(s) + CO2(g) + H2O(l) The resulting calcium hexafluorosilicate (CaSiF6) is bonded to the surface of the marble. This is harder, more glossy and stain resistant compared to the original surface. The other often used method of finishing marble is the use of polishing with oxalic acid (H2C2O4), an organic acid. The resulting reaction is as follows. :CaCO3(s) + H2C2O4(l) → CaC2O4(s) + CO2(g) + H2O(l) In this case the calcium oxalate (CaC2O4) formed in the reaction is washed away with the slurry leaving a surface that has not been chemically changed.Microbial degradation
The haloalkaliphilic methylotrophic bacterium ''Methylophaga murata'' was isolated from deteriorating marble in the Kremlin. Bacterial and fungal degradation was detected in four samples of marble from Milan Cathedral; black ''Cladosporium'' attacked dried acrylic resin using melanin.Cultural associations
As the favorite medium for Greek and Roman sculptors and architects (see classical sculpture), marble has become a cultural symbol of tradition and refined taste. Its extremely varied and colorful patterns make it a favorite decorative material, and it is often imitated in background patterns for computer displays, etc.
Places named after the stone include Marblehead, Massachusetts; Marblehead, Ohio; Marble Arch, London; the Sea of Marmara; India's Marble Rocks; and the towns of Marble, Minnesota; Marble, Colorado; Marble Falls, Texas, and Marble Hill, Manhattan, New York. The Elgin Marbles are marble sculptures from the Parthenon in Athens that are on display in the British Museum. They were brought to Britain by the Thomas Bruce, 7th Earl of Elgin, Earl of Elgin.
Gallery
See also
* Marble sculpture * Marmorino * Paper marbling * Pietra dura, inlaying with marble and other stones * Ruin marble, marble that contains light and dark patterns, giving the impression of a ruined cityscape * Scagliola, imitating marble with plasterwork * Verd antique, sometimes (erroneously) called "serpentine marble", and often confused with Connemara marbleReferences
External links
Dimension Stone Statistics and Information
– United States Geological Survey minerals information for dimension stone
USGS 2005 Minerals Yearbook: Stone, Crushed
{{Authority control Marble, Sculpture materials Metasedimentary rocks Limestone Stone (material) Symbols of Alabama