Limestone
What is Limestone?
Limestone is a sedimentary rock composed primarily of calcium carbonate (CaCO3) in the form of the mineral calcite.
It most commonly forms in clear, warm, shallow marine waters. It is usually an organic sedimentary rock that forms from the
accumulation of shell, coral, algal and fecal debris. It can also be a chemical sedimentary rock formed by the precipitation of
calcium carbonate from lake or ocean water.
|
Limestone: The specimen shown is about two inches (five centimeters) across.
|
Limestone-Forming Environments:
|
| A NASA satellite image of the Bahamas Platform where active limestone formation occurs today. The main platform is over 100 miles wide and a great thickness of calcium carbonate sediments have accumulated there. In this image the dark blue areas are deep ocean waters. The shallow Bahamas Platform appears as light blue. Enlarge image. |
|
|
Most limestones form in shallow, calm, warm marine waters. That type of environment is where organisms capable of forming calcium carbonate
shells and skeletons can easily extract the needed ingredients from ocean water. When these animals die their shell
and skeletal debris accumulate as a sediment that might be lithified into limestone. Their waste products can also contribute
to the sediment mass. Limestones formed from this type of sediment are biological sedimentary rocks.
Their biological origin is often revealed in the rock by the presence of fossils.
Some limestones can form by direct precipitation of calcium carbonate from marine or fresh water. Limestones formed this way are chemical sedimentary rocks.
They are thought to be less abundant than biological limestones.
Today Earth has many limestone-forming environments. Most of them are found in shallow water areas between 30 degrees north latitude and 30 degrees south latitude.
Limestone is forming in the Caribbean Sea, Indian Ocean, Persian Gulf, Gulf of Mexico, around Pacific Ocean islands and within the Indonesian archipelago.
One of these areas is the Bahamas Platform, located in the Atlantic Ocean about 100 miles southeast of southern Florida (see satellite image at right). There abundant corals, shellfish, algae and other organisms produce vast amounts of calcium carbonate skeletal debris that completely blankets the platform. This is producing an extensive limestone deposit.
|
A Limestone-Forming Environment: An underwater view of a coral reef system from the Kerama Islands in the East
China Sea southwest of Okinawa. Here the entire seafloor is covered by a wide variety of corals which produce calcium
carbonate skeletons. A United States Geological Survey image by Curt Storlazzi.
|
|
| A drop of water hangs and evaporates on the tip of a stalactite. National Park Service image. |
|
|
Limestone can also form through evaporation. Stalactites, stalagmites and other cave formations (often called "speleothems") are
examples of limestone that formed through evaporation. In a cave, droplets of water seeping down from above enter the cave through
fractures or other pore spaces in the cave ceiling. There they might evaporate before falling to the cave floor.
When the water evaporates, any calcium carbonate that was dissolved in the water will be deposited on the cave ceiling. Over time this
evaporative process can result in an accumulation of icicle-shaped calcium carbonate on the cave ceiling. These deposits are known as
stalactites. If the droplet falls to the floor and evaporates there a stalagmite could grow upwards from the cave floor.
The limestone that makes up these cave formations is known as "travertine" and is a chemical sedimentary rock. A rock known as "tufa" is a limestone formed by
evaporation at a hot spring, lake shore, or other area.
Composition of Limestone
Limestone is by definition a rock that contains at least 50% calcium carbonate in the form of calcite by weight. All
limestones contain at least a few percent other materials. These can be small particles of quartz, feldspar, clay
minerals, pyrite, siderite and other minerals. It can also contain large nodules of chert, pyrite or siderite.
The calcium carbonate content of limestone gives it a property that is often used in rock identification - it effervesces in contact with a cold solution of 5% hydrochloric acid.
Varieties of Limestone
There are many different names used for limestone. These names are based upon how the rock formed, its
appearance or its composition and other factors. Here are some of the more commonly used.
Chalk: A soft limestone with a very fine texture that is usually white or light gray in color. It is formed mainly from the calcareous shell remains of microscopic marine organisms such as foraminifers or the calcareous remains from numerous types of marine algae.
Coquina: A poorly-cemented limestone that is composed mainly of broken shell debris. It often forms on beaches where wave action segregates shell fragments of similar size.
Fossiliferous Limestone: A limestone that contains obvious and abundant fossils. These are normally shell and skeletal fossils of the organisms that produced the limestone.
Lithographic Limestone: A dense limestone with a very fine and very uniform grain size that occurs in thin beds that separate easily to form a very smooth surface. In the late 1700's a printing process (lithography) was developed to reproduce images by drawing them on the stone with an oil-based ink and then using that stone to press multiple copies of the image.
Oolitic Limestone: A limestone composed mainly of calcium carbonate "oolites", small spheres formed by the concentric precipitation of calcium carbonate on a sand grain or shell fragment.
Travertine: A limestone that forms by evaporative precipitation, often in a cave, to produce formations such as stalactites, stalagmites and flowstone.
Tufa: A limestone produced by precipitation of calcium-laden waters at a hot spring, lake shore or other location.
|
Coquina: This photo shows the shell hash known as coquina. The rock shown here is about two inches (five centimeters) across.
|
|
Chalk: A fine-grained, light-colored limestone formed from the calcium carbonate skeletal remains of tiny marine organisms.
|
|
Tufa: A porous limestone that forms from the precipitation of calcium carbonate, often at a hot spring or along the shoreline of a lake where waters are saturated with calcium carbonate.
|
Uses of Limestone
Limestone is a rock with an enormous diversity of uses. It could be the one rock that
is used in more ways than any other. Most limestone is crushed and used as a construction material.
It is used as a crushed stone for road base and railroad ballast. It is used as an
aggregate in concrete. It is fired in a kiln with crushed shale to make cement.
Some varieties of limestone perform well in these uses because they are strong, dense
rocks with few pore spaces. These properties enable them to stand up well to abrasion and freeze-thaw. Although
limestone does not perform as well in these uses as some of the harder silicate rocks it is much easier
to mine and does not exert the same level of wear on mining equipment, crushers, screens and
the beds of the vehicles that transport it.
Some additional but also important uses of limestone include:
Dimension Stone: Limestone is often cut into blocks and slabs of specific dimensions for use in construction and in architecture. It is used for facing stone, floor tiles, stair treads, window sills and many other purposes.
Roofing Granules: Crushed to a fine particle size, crushed limestone is used as a weather and heat-resistant coating on asphalt impregnated shingles and roofing. It is also used as a top coat on built-up roofs.
Flux Stone: Crushed limestone is used in smelting and other metal refining processes. In the heat of smelting, limestone combines with impurities and can be removed from the process as a slag.
Portland Cement: Limestone is heated in a kiln with shale, sand and other materials and ground to a powder that will harden after being mixed with water.
AgLime: Calcium carbonate is one of the most cost-effective acid neutralizing agents. When crushed to sand-size or smaller particles limestone becomes an effective material for treating acidic soils. It is widely used on farms throughout the world.
Lime: If calcium carbonate (CaC03 is heated to high temperature in a kiln the products will be a release of carbon dioxide gas (CO2) and calcium oxide (CaO). The calcium oxide is a powerful acid neutralization agent. It is widely used as a soil treatment agent (faster acting than aglime) in agriculture and as an acid neutralization agent by the chemical industry.
Animal Feed Filler: Chickens need calcium carbonate to produce strong egg shells so calcium carbonate is often offered to them as a dietary supplement in the form of "chicken grits". It is also added to the feed of some dairy cattle who must replace large amounts of calcium lost when the animal is milked.
Mine Safety Dust: Also known as "rock dust". Pulverized limestone is a white powder that can be sprayed onto exposed coal surfaces in an underground mine. This coating improves illumination and reduces
the amount of coal dust that activity stirs up and releases into the
air. This improves the air for breathing and it also reduces the explosion hazard produced by suspended particles of flammable coal dust in the air.
Limestone has many other uses. Powdered limestone is used as a filler in paper, paint, rubber and plastics. Crushed limestone is used as a filter stone in on-site sewage disposal systems. Powdered limestone is also used as a sorbent (a substance that absorbs pollutants) at many coal-burning facilities.
Limestone is not found everywhere. It only occurs in areas underlain by sedimentary rocks. Limestone is needed in other areas and is so important that buyers will pay five times the value of the stone in delivery charges so that limestone can be used in their project or process.
|
The rock photos above were taken by Ann Bryant and are copyright by Geology.com. |
|
|
|
"A Grain of Sand": A gallery of sand grains from around the world as photographed through a microscope by Dr. Gary Greenberg. |
|
Igneous Rocks: Photos and facts about intrusive and extrusive igneous rocks. |
|
