Limestone facts for kids

Limestone rocks in the form of a karst

Cotswold stone cottages in Bibury, England. They were built in 1380 as a monastic wool store and converted into weavers' cottages in the 17th century

Limestone is a sedimentary rock, made up mostly of the mineral calcite, a form of calcium carbonate, CaCO₃.

The calcium carbonate is originally produced by living organisms. Later, some of it goes into solution in sea water. Limestone rocks include mainly organic remains and precipitated carbonate.

Limestone is about 10% of the total volume of all sedimentary rocks.

Formation

Limestones are mostly made of calcium carbonate. It is originally made by small photosynthetic protists like certain bacteria, coccolithophores, and algae. Then the carbonate gets used by various animals, like bivalves and the polyps which make coral reefs. They build their shells or framework out of CaCO₃ crystals.

"[Coccolithophores] were the first organisms to bring about a steady rain of calcium carbonate from the upper, illuminated zone of the ocean towards the deep sea".^p144

Carbonates are rocks formed from these sources, plus any CaCO₃ which is precipitated out of solution. Some carbonate dissolves in the water. It gets precipitated when the physical condition of the water changes. For example, if the concentration of CaCO₃ is high, then a temperature drop, or a pH (acidity) change, can cause precipitation.

Florida Bay

Florida Bay, the shallow lagoon behind the Florida Keys, is a model for the conditions which produced limestones on the continental shelf. Of course, all the species were somewhat different then but, as an ecosystem, it is similar.

In Florida Bay there is a lot of a type of flowering plant called sea grass. There is also a lot of white, milky water full of calcium carbonate. This is mainly formed by Melobesia, a small red alga which lives on the sea grass.^p151 Finally, the organisms produce huge amounts of slime, which is a polysaccharide. There is good reason to think the slime is produced by microorganisms to control the way their carbonate skeletons are formed.^p139 As a side-effect the slime limits the amount of carbonate which goes into solution.^p155

Florida Bay is a flat platform which has laid down a huge amount of carbonate rock.

"You have to drill for more than 3000 feet before you reach a different rock type, and that is of Cretaceous age—some 70 million years ago".^p158

Fossiliferous limestones

Many limestones contain fossils, and some are made up almost entirely of skeletal material. Chalk is ~99% coccoliths; Solnhofen limestone is famous for its animal fossils; and there are many shelly limestones from different periods. Limestone is not found much before the Cambrian period, because shelled animals had not yet evolved.

Limestone as building material

Marble

When limestone is heated to a high temperature, and squeezed at the base of a mountain, it recrystallizes into the metamorphic rock marble. Marbles are fairly dense, relatively easy to cut, or be shaped into blocks, and some forms are white in colour.

Uses

Limestone is hard enough to resist weathering but usually soft enough to be worked (cut and carved) by stonemasons. It is used for building material. Limestone, particularly Portland limestone, became popular in the 19th and 20th centuries for building things such as churches, banks and houses. However, acid rain does slowly erode limestone.

Limestone is used to make glass and cement. It is also used to make iron in a blast furnace, to remove impurities from the iron ore.

Related pages

• Portland limestone

Images for kids

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  This limestone deposit in the karst of Dinaric Alps near Sinj, Croatia was formed in the Eocene.

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  Ooids from a beach on Joulter's Cay, The Bahamas

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  Ooids in limestone of the Carmel Formation (Middle Jurassic) of southwestern Utah.

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  Thin-section view of a Middle Jurassic limestone in southern Utah, U.S. The round grains are ooids; the largest is 1.2 mm (0.05 in) in diameter. This limestone is an oosparite.

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  Travertine limestone terraces of Pamukkale, Turkey.

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  An aerial view of a whiting event precipitation cloud in Lake Ontario.

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  Akcakoca chert nodules within soft limestone

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  Macrostylolites in a limestone.

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  El Capitan, an ancient limestone reef

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  Mønsted is the largest limestone mine in the world.

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  Coral reef at Nusa Lembongan, Bali, Indonesia

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  The Cudgel of Hercules, a tall limestone rock in Poland (Pieskowa Skała Castle in the background)

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  A limestone plate with a negative map of Moosburg in Bavaria is prepared for a lithography print.

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  Plastic bag "made mainly from limestone"

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  Limestone quarry at Cedar Creek, Virginia, USA

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  Nordkalk's limestone quarry in Pargas, Finland

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  Cutting limestone blocks at a quarry in Gozo, Malta

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  Limestone is used worldwide as building material.

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  A stratigraphic section of Ordovician limestone exposed in central Tennessee, U.S. The less-resistant and thinner beds are composed of shale. The vertical lines are drill holes for explosives used during road construction.

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  Photo and etched section of a sample of fossiliferous limestone from the Kope Formation (Upper Ordovician) near Cincinnati, Ohio, U.S.

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  Biosparite limestone of the Brassfield Formation (Lower Silurian) near Fairborn, Ohio, U.S., showing grains mainly composed of crinoid fragments

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  A concretionary nodular (septarian) limestone at Jinshitan Coastal National Geopark, Dalian, China

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  Limestone from Lake Tai, used in gongshi, a Chinese stone art

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  Folded limestone layers on Cascade Mountain in Provo Canyon, Utah

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  Fossils in limestone from the northern Black Sea region

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  Limestone distribution in Ohio, from "Geography of Ohio," 1923

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  Chalk is a variety of limestone. It is a softer, and more powdery material.