Cave

They are beautiful and sometimes otherworldly. Existing beneath the surface of the planet, caves have attracted humans for hundreds of thousands of years. Considered by some cultures as sacred, caves have been used in rituals and ceremonies. They have served both as shelter and burial tombs. The human remains and artifacts found in them have aided archaeologists in learning about early humans. Pictographs (rock paintings) in caves, some estimated to be more than 30,000 years old, attest to the creativity of early humans and their relationship to the natural world.

The shape of the land

The scientific study of caves is called speleology (pronounced speelee-AH-luh-jee; from the Greek words spelaion, meaning "cave," and logos, meaning "study of"). A cave is generally defined as a naturally formed cavity or hollow beneath the surface of Earth that is beyond the zone of light and is large enough to be entered by humans. Some sources use the word cavern interchangeably with cave. Technically, a cavern is a large chamber within a cave. A series of caves connected by passages is a cave system.

Individual caverns and cave systems may be immense. In the Chiquibul (pronounced chee-ke-BOOL) Cave System in Belize and Guatemala, the Belize Chamber measures nearly 1,600 feet (490 meters) long by 600 feet (180 meters) wide. It is the largest cavern in the Western Hemisphere. The largest recorded cave system in the world is Mammoth Cave System. It extends for more than 345 miles (555 kilometers) in south-central Kentucky.

There are different types of caves, formed in different areas by different geologic processes, that do not meet the general definition of a cave.

Glacier caves are formed inside glaciers by meltwater (water from melted ice or snow) that runs through cracks in the ice, producing tunnels and cavities. Sea caves are formed in cliffs and ledges along the shores of oceans and other large bodies of water where the constant pounding of waves wears away rock. Lava tube caves are formed when the outer surface of a lava flow begins to cool and harden while lava inside remains hot. Once the stream of molten lava inside drains out, a tube or tunnel remains. Kazumura Cave in Hawaii, measuring approximately 38 miles (61 kilometers) in length, is the longest lava tube cave in the world.

The most common, largest, and most spectacular caves, however, are solution caves. These caves are formed through the chemical interaction of air, water, soil, and rock. They usually form in areas where the dominant rock is limestone, a type of sedimentary rock (rock formed by the accumulation and compression of sediment, which may consist of rock fragments, remains of microscopic organisms, and minerals). Many solution caves feature streams and lakes and unusual mineral formations. These formations are known as speleothems (pronounced SPEE-lee-ohthems; from the Greek words spelaion, meaning "cave," and thema, meaning "deposit"). Because of the way they form, speleothems are also commonly known as dripstone.

The primary speleothems are stalactites, stalagmites, columns, curtains, and flowstones. A stalactite (pronounced sta-LACK-tite) is an icicle-shaped formation that hangs from the ceiling of a cave. A similarly shaped deposit, though often not as pointy, that projects upward from the floor of a cave is a stalagmite (pronounced sta-LAG-mite). Stalagmites generally form underneath stalactites. The two deposits often grow until they join, forming a stout, singular deposit known as a column. A curtain (sometimes called drapery) is a mineral deposit that forms a thin, wavy or folded sheet that hangs from the ceiling of a cave. Any mineral deposit that forms sheets on a wall or floor of a cave is known by the general term flowstone. Although normally whitish or off-white in color, speleothems may contain traces of different minerals that add shades of brown, orange, yellow, red, pink, green, black, and other colors.

Cave ceilings often collapse. As they do, the rock or ground above them also collapses. If the cave is located near Earth's surface, a bowl-like depression known as a sinkhole can develop on the surface. Sinkholes may also form above areas where limestone or other sedimentary rock has been eroded away (erosion is the gradual wearing away of Earth surfaces through the action of wind and water). Sinkholes may range in diameter from a few feet to a few thousand feet.

A landscape dominated by sinkholes on the surface and extensive cave systems underneath is known as karst topography or karst terrain. Karst (Kras in Serbo-Croatian) is the name of a limestone plateau in the Dinaric Alps in northwest Slovenia that is marked by such geological formations. It was the first area to be studied based on these formations. Karst topography also features losing streams, which are streams on Earth's surface that are diverted underground through sinkholes or caves, and springs, which are areas where water from underground flows out almost continuously through an opening at Earth's surface.

As karst topography continues to develop, a variety of landforms may arise on the surface. This is especially true in tropical or humid climate areas. Caves that grow ever larger soon start to collapse. Sinkholes in the area enlarge and merge. Sections of the ground remain elevated as streams and other running water erode the limestone rock mass around them ever deeper. These sections may form hills, known as cone karst, separated by the sinkholes. Eventually, steep limestone landforms called karst towers may remain standing hundreds of feet above the surrounding landscape. With nearly vertical walls, the towers are often bare of vegetation. The world's most impressive karst towers are perhaps those found in the Guangxi (pronounced GWAN-shee) Province in southern China.

Cave: Words to Know

Cave:

A naturally formed cavity or hollow beneath the surface of Earth that is beyond the zone of light and is large enough to be entered by humans.

Cavern:

A large chamber within a cave.

Cave system:

A series of caves connected by passages.

Curtain:

A thin, wavy or folded sheetlike mineral deposit that hangs from the ceiling of a cave.

Erosion:

The gradual wearing away of Earth surfaces through the action of wind and water.

Flowstone:

The general term for a sheetlike mineral deposit on a wall or floor of a cave.

Groundwater:

Freshwater lying within the uppermost parts of Earth's crust, filling the pore spaces in soil and fractured rock.

Karst topography:

A landscape characterized by the presence of sinkholes, caves, springs, and losing streams.

Limestone:

A sedimentary rock composed primarily of the mineral calcite (calcium carbonate).

Losing stream:

A stream on Earth's surface that is diverted underground through a sinkhole or a cave.

Sedimentary rock:

Rock formed by the accumulation and compression of sediment, which may consist of rock fragments, remains of microscopic organisms, and minerals.

Sinkhole:

A bowl-like depression that develops on Earth's surface above a cave ceiling that has collapsed or on an area where the underlying sedimentary rock has been eroded away.

Speleothem:

A mineral deposit formed in a cave.

Stalactite:

An icicle-shaped mineral deposit hanging from the roof of a cave.

Stalagmite:

A cone-shaped mineral deposit projecting upward from the floor of a cave.

Forces and changes: Construction and destruction

Caves are found almost everywhere around the planet. More than 17,000 have been identified in the United States, underlying 20 percent of the country's land surface. They are found in 48 of the 50 states (only Louisiana and Rhode Island lack caves). While the processes that form lava tube caves, glacier caves, sea caves, and other caves are obvious, those that form solution caves—the most common caves of all—are not. Solution caves are not formed by volcanic activity or by the abrasive forces of water or wind. The primary force behind their formation is chemical weathering, which alters the internal structure of minerals by removing or adding elements.

It begins in the sky

The formation of a solution cave begins in Earth's atmosphere. As precipitation (mainly rain) falls to the planet's surface, the water (H₂O) reacts with carbon dioxide (CO₂) in the atmosphere to form weak carbonic acid (H₂CO₃). This is the same acid found in soda pop that produces its "fizz." Once this water and carbonic acid solution reaches Earth's surface and begins to percolate down through the soil, it reacts with carbon dioxide given off by decaying plants and animal matter to form even more carbonic acid solution.

The main mineral in limestone is calcite (calcium carbonate). Most seashells are made of this mineral. Limestone is almost insoluble (unable to be dissolved) in water. Carbonic acid, however, dissolves calcite from limestone. Over hundreds of thousands to millions of years, as carbonic acid moves downward through cracks and fractures in limestone, it dissolves the rock and forms crevices. Over time, these crevices widen to become passages and caverns.

A Sinking State

The entire state of Florida lies on limestone. Much of this underlying rock is weathered, featuring cavities exceeding 100 feet (30 meters) in height and width. Although many are buried beneath sediments, sinkholes dot the land surface. This is especially true in central Florida, an area prone to sinkhole formation. The water table in this area is often only 5 to 10 feet (1.5 to 3 meters) below the surface of the ground.

The largest sinkhole to have formed in Florida in recorded history appeared suddenly in May 1981 in the city of Winter Park. In the span of one day, a hole measuring 350 feet (107 meters) wide and 110 feet (34 meters) deep opened up. The Winter Park sinkhole, as it became known afterward, swallowed a house, five cars from a nearby parking lot, and part of a city swimming pool. The city later stabilized and sealed the sinkhole, converting it into an urban lake.

This activity occurs in an area beneath Earth's surface where freshwater fills all pore spaces and microscopic openings in rocks and sediment. These openings include the spaces between grains of sand as well as cracks

and fractures in rocks. As rain or melted snow seeps through the ground, some of it clings to particles of soil or to roots of plants. The remaining water moves deeper, drawn downward by gravity, until it reaches a layer of rock or sediment, such as clay, through which it cannot easily pass. It then fills the empty spaces and cracks above that layer. This water is known as groundwater, and the area where it fills all the spaces and pores underground is the zone of saturation. The top surface of this zone is called the water table. Above it, the pores and spaces in rock hold mainly air, along with some water. This is called the zone of aeration.

Caves initially form just below the water table. Filled with water, the cavities and fractures in the limestone are enlarged by the continuous movement of water and carbonic acid through them. Air enters a cave only when the water table is lowered through some geologic event, such as erosion of the land surface above or uplift of the rock beneath the cave. When this occurs, the cave stops enlarging and water begins to drain out of the cave down through cracks and other passages in the surrounding limestone. Areas of the cave may continue to lie below the water table and, therefore, are still water-filled. An underground stream, whose water source lies farther away, may still flow through the cave.

Drip by drip

The air-filled sections of the cave provide the perfect environment for the development of speleothems. Even though the water table may have dropped, water weaving its way downward from Earth's surface still enters a cave through cracks and crevices in its ceiling and walls. When this water and carbonic acid solution enters the cave, some of the carbon dioxide in the solution escapes into the air (much like a soda pop that loses carbon dioxide and goes "flat" when left uncovered). This changes the chemical structure of the solution, and it can no longer hold the dissolved calcite. The calcite is then deposited in crystallized form as a speleothem. Its shape depends on where and how quickly water enters the cave. Though growth rates of speleothems vary from cave to cave, it may take 120 years or longer for 1 cubic inch (16.4 cubic centimeters) of calcite to be deposited on a cave formation.

The Largest Enclosed Space on Earth

The largest cavern in the world is the Sarawak Chamber of the Good Luck Cave in Sarawak, Malaysia. It measures approximately 1,970 feet (600 meters) in length, 1,310 feet (400 meters) in width, and 330 feet (100 meters) in height. It has a total area of 1,751,300 square feet (162,700 square meters). The cavern is large enough to hold eight Boeing 747 aircraft lined up nose to tail.

By comparison, the largest cavern in the United States is the Big Room in the Carlsbad Caverns cave system in New Mexico. Covering an area of 357,472 square feet (33,210 square meters), it is just over one-fifth the size of the Sarawak Chamber.

Water slowly dripping from a small opening in the ceiling of the cave initially forms a soda straw. This tubelike formation develops when each drop evaporates, leaving behind a small amount of calcite around its border. As more drops fall, more calcite is deposited and the tube grows downward. Even though they are quite fragile and have the diameter of a drop of water, soda straws may grow to 3 feet (1 meter) or more in length. If the tube becomes blocked and more drops begin to fall, then a stalactite forms around the soda straw. If drops of water increase even further from the ceiling, they may fall off a stalactite before evaporating and form a stalagmite. Because the drops spread when they hit the floor or ledge of a cave, a stalagmite is often wider than the stalactite under which it often grows. An extremely rapid drip from a ceiling may form a pool of water on the floor of a cave. As the water evaporates along the edges of the pool, calcite may form terraces.

If water drips from various points in a crack in a cave ceiling, stalactites may grow in a row. Eventually, they may grow together, forming a continuous sheet. A flowing sheet may also develop if water seeps slowly along the length of a thin slit in the ceiling. When a crack appears in a cave wall, a film of the water may flow down the wall and over ledges, forming sheets of flowstone.

The multitude of speleothems that develop in caves vary widely. In fact, no two caves are ever alike. The air temperature of the cave, the amount and chemical composition of the water entering it, and the size of the joints and cracks in its ceiling and walls are just a few of the factors that determine a cave's particular appearance.

Fragile Features

Caves are environments that contain not only fantastic mineral formations but rare and unusual animals. These include blind fish, colorless spiders, and many other troglobites (pronounced TROG-lah-bites), animals that live in caves and cannot survive outside of them. Troglobites have evolved over millions of years, becoming adapted to the absolute blackness and meager food offerings of cave life. Caves are also home to animals that venture out periodically in search of food. Beetles, crickets, frogs, salamanders, and others are of this type. Finally, caves serve as temporary homes to animals that move freely in and out of them. Bats, bears, moths, and skunks are examples of these.

For many people, cave exploration is a fascinating and fun activity. Spelunking (pronounced spi-LUNG-king) is the term given to such exploration. Spelunking societies, organizations, and groups exist across the country, helping people explore the more than 100 caves that are open to the public for study and enjoyment.

Although caves are carved out of rock, they are fragile. Vandalism, property development, and air and water pollution have all had a devastating effect on caves and cave life. Even oil left on a speleothem by the accidental touch of a human hand can alter its formation, eventually destroying it. Of the more than 130 species that inhabit the Mammoth Cave System in Kentucky, dozens are considered threatened or endangered. For the continued study and exploration of caves and the life they harbor, great care must be taken.

Most caves are constantly changing. Some are still enlarging, with new passages being formed below the water table (in a cave system, the oldest caves and passages are closest to Earth's surface). Many caves are still wet, with calcite being deposited on various formations. Other caves and cave systems, however, are dry and are no longer enlarging or growing speleothems. Eventually, in a dry cave, the thin ceiling may lose support and collapse, exposing the cave to the surface through a sinkhole.

Spotlight on famous forms

Lechuguilla Cave, New Mexico

The deepest limestone cave in the United States is Lechuguilla (pronounced lech-uh-GEE-yah) Cave. Part of the Carlsbad Caverns cave system in southeast New Mexico, it extends to a depth of 1,571 feet (479 meters). The cave was discovered by a group of cavers in 1986. Scientists estimate that the cave has existed beneath Earth's surface for at least 2 million years.

The cave is notable not only for its size, but for its fantastic array of rare speleothems. Unlike other solution caves, Lechuguilla was not formed by carbonic acid. Rather, rising hydrogen sulfide from nearby oil fields reacted with groundwater to form sulfuric acid. This acid dissolved the limestone and created a cave filled with lemon-yellow sulfur formations. Among those is a 24-foot (7.3-meter) soda straw, the longest in the world.

In addition to unusual speleothems, Lechuguilla contains rare bacteria that feed on the sulfur, iron, and manganese minerals present in the cave. Scientists believe these bacteria may have played a part in the formation of the cave and its speleothems. They also believe the sulfur-laden environment of Lechuguilla may be similar to that on the surface of Mars, so they have studied the cave's bacteria to determine how life may exist on that planet.

Mammoth Cave System, Kentucky

The Mammoth Cave System, properly known as the Mammoth Cave-Flint Ridge System, is the largest cave system in the world. Lying beneath the surface in south-central Kentucky, the system extends for more than 345 miles (555 kilometers) and to a depth of 379 feet (116 meters). Geologists believe there may be an additional 600 miles (965 kilometers) of undiscovered passageways connected to the system.

Scientists estimate the system began to form in the limestone rocks underlying the area some 30 million years ago. Archaeologists have found evidence that early Native Americans inhabited the cave system as many as 4,000 years ago.

The land surface above Mammoth Cave System is marked by sinkholes and losing streams. Underneath this karst topography lie tunnels, passages, caverns, and almost every type of speleothem. Underground rivers flow through some of the system's deepest caverns. Mammoth Dome

is a cavity in the system that measures 192 feet (59 meters) in height. Another extraordinary feature is Frozen Niagara, a mass of flowstone 75 feet (23 meters) tall and 4 feet (1.2 meters) wide.

Voronya Cave, Republic of Georgia

On January 6, 2001, a team of Ukrainian and Russian cavers exploring a cave in the Abkhazia region of the Republic of Georgia reached a depth of 5,610 feet (1,710 meters). This event confirmed Voronya Cave (also known as Krubera Cave) as the world's deepest cave. The previous record holder had been Lamprechtsofen-Vogelshacht Cave in Austria, which measures 5,355 feet (1,632 meters) in depth.

Voronya Cave was so-named because of the large number of crows that gather around its entrance (voron is Russian for "crow"). Discovered in the late 1960s, the cave is located in a valley in the western Caucasus Mountains. Meandering downward through dense limestone, the cave features one entrance that leads to three branches. When first explored in the 1980s, the cave was thought to end in a narrow passage 1,110 feet (3,335 meters) beneath the surface. In 1999, an expedition found new passages that led to deeper pits.

For More Information

Books

Aulenbach, Nancy Holler, and Hazel A. Barton. Exploring Caves: Journeys into the Earth. Washington, D.C.: National Geographic, 2001.

Gillieson, David S. Caves: Processes, Development, and Management. Cambridge, MA: Blackwell Publishers, 1996.

Moore, George W., and Nicholas Sullivan. Speleology: Caves and the Cave Environment. Third ed. St. Louis, MO: Cave Books, 1997.

Palmer, Arthur N., and Kathleen H. Lavoie. Introduction to Speleology. St. Louis, MO: Cave Books, 1999.

Taylor, Michael Ray. Caves: Exploring Hidden Realms. Washington, D.C.: National Geographic, 2001.

Web Sites

"Cave Facts." American Cave Conservation Association. http://www.cavern.org/CAVE/ACCA_index.htm (accessed on August 14, 2003).

"Caves Theme Page." Gander Academy. http://www.stemnet.nf.ca/CITE/cave.htm (accessed on August 14, 2003).

"Karst Topography Teacher's Guide and Paper Model." U.S. Geological Survey. http://wrgis.wr.usgs.gov/docs/parks/cave/karst.html (accessed on August 14, 2003).

"NOVA: Mysterious Life of Caves." WGBH Educational Foundation. http://www.pbs.org/wgbh/nova/caves/ (accessed on August 14, 2003).

"Park Geology Tour of Cave and Karst Parks." National Park Service, Geologic Resources Division. http://www.aqd.nps.gov/grd/tour/caves.htm (accessed on August 14, 2003).

Cave

A cave is a naturally occurring hollow area inside the earth. Most caves are formed by some type of erosional process. The most notable exception is hollow lava tubes such as those found in the Hawaiian Islands. The formation of caves depends upon geologic, topographic, and hydrologic factors. These factors determine where and how caves develop, as well as their structure and shape. The study of caves is called speleology. Some caves may be small hillside openings, while others consist of large chambers and interconnecting tunnels and mazes. Openings to the surface may be large gaping holes or small crevices.

Caves hosted in rocks other than limestone are usually formed by water erosional processes. For example, rivers running through canyons with steep walls erode the rock at points where the current is strong. Such caves usually have large openings and are not too deep. Caves of this type can be found in the southwestern United States and were at one time inhabited by prehistoric American Indians known as Cliff Dwellers. Sea caves are formed by waves continually crashing against cliffs or steep walls. Often these caves can only be entered at low tide. Ice caves are also formed in glaciers and icebergs by meltwater that drains down crevices in the ice.

Lava caves, which are often several miles long, form when the exterior of a lava flow hardens and cools to form a roof, but lava below the surface flows out, leaving a hollow tube. Wind or aeolian caves usually form in sandstone cliffs as wind-blown sand abrades the cliff face. They are found in desert areas, and occur in a bottleneck shape with the entrance much smaller than the chamber. Talus caves are formed by boulders that have piled up on mountain slopes. The most common, largest, and spectacular caves are solution caves.

Solution caves form by chemical weathering of the surrounding bedrock as groundwater moves along fractures in the rock. These caves produce a particular type of terrain called karst. Karst terrain primarily forms in bedrock of calcium carbonate, or limestone, but can develop in any soluble sedimentary rock such as dolomite , rock gypsum , or rock salt. The host rock extends from near the earth's surface to below the water table . Several distinctive karst features make this terrain easy to identify. The most common are sinkholes , circular depressions where the underlying rock has been dissolved away. Disappearing streams and natural bridges are also common clues. Entrances to solution caves are not always obvious, and their discovery is sometimes quite by accident.

Formation of karst involves the chemical interaction of air, soil , water, and rock. As water flows over and drains into the earth's surface, it mixes with carbon dioxide from the air and soil to form carbonic acid (H₂CO₃). The groundwater becomes acidic and dissolves the calcium carbonate in the bedrock, and seeps or percolates through naturally occurring fractures in the rock. With continual water drainage, the fractures become established passageways. The passageways eventually enlarge and often connect, creating an underground drainage system. Over thousands, perhaps millions of years, these passages evolve into the caves seen today.

During heavy rain or flooding in a well-established karst terrain, very little water flows over the surface in stream channels. Most water drains into the ground through enlarged fractures and sinkholes. This underground drainage system sometimes carries large amounts of water, sand, and mud through the passageways and further erodes the bedrock. Sometimes ceilings fall and passageways collapse, creating new spaces and drainage routes.

Not all solution caves form due to dissolution by carbonic acid. Some caves form in areas where hydrogen sulfide gas is released from the earth's crust or from decaying organic material. Sulfuric acid forms when the hydrogen sulfide comes in contact with water. It chemically weathers the limestone, similar to acid rain .

The deep cave environment is often completely dark, has a stable atmosphere, and the temperature is rather constant, varying only a few degrees throughout the year. The humidity in limestone caves is usually near 100%. Many caves contain unique life forms, underground streams and lakes , and have unusual mineral formations called speleothems.

When groundwater seeps through the bedrock and reaches a chamber or tunnel, it meets a different atmosphere. Whatever mineral is in solution reacts with the surrounding atmosphere, precipitates out, and is deposited in the form of a crystal on the cave ceiling or walls. Calcite, and to a lesser degree, aragonite, are the most common minerals of speleothems. The amount of mineral that precipitates out depends upon how much gas was dissolved in the water. For example, water that must pass through a thick layer of soil becomes more saturated with carbon dioxide than water that passes through a thin layer. This charges the water with more carbonic acid and causes it to dissolve more limestone from the bedrock. Later, it will form a thicker mineral deposit in the cave interior as a result.

Water that makes its way to a cave ceiling hangs as a drop. When the drop of water gives off carbon dioxide and reaches chemical equilibrium with the cave atmosphere, calcite starts to precipitate out. Calcite deposited on the walls or floors in layers is called flowstone.

Sometimes water runs down the slope of a wall, and as the calcite is deposited, a low ridge is formed. Subsequent drops of water follow the ridge, adding more calcite. Constant buildup of calcite in this fashion results in the formation of a large sheet-like formation, called a curtain, hanging from the ceiling. Curtain formations often have waves and folds in them and have streaks of various shades of off-white and browns. The streakiness results from variations in the mineral and iron content of the precipitating solution.

Often, a hanging drop falls directly to the ground. Some calcite is deposited on the ceiling before the drop falls. When the drop falls, another takes its place. As with a curtain formation, subsequent drops will follow a raised surface and a buildup of calcite in the form of a hanging drop develops. This process results in icicle-shaped speleothems called stalactites. The water that falls to the floor builds up in the same fashion, resembling an upside down icicle called a stalagmite.

Of course, there are variations in the shape of speleothems depending on how much water drips from the ceiling, the temperature of the cave interior, rates and directions of air flow in the cave, and how much dissolved limestone the water contains. Speleothems occur as tiered formations, cylinders, cones, some join together, and occasionally stalactites and stalagmites meet and form a tower. Sometimes, when a stalactite is forming, the calcite is initially deposited in a round ring. As calcite builds up on the rim and water drips through the center, a hollow tube called a straw develops. Straws are often transparent or opaque and their diameter may be only that of a drop of water.

Stalagmites and stalactites occur in most solution caves and usually, wherever a stalactite forms, there is also a stalagmite. In caves where there is a great deal of seepage, water may drip continuously. Speleothems formed under a steady drip of water are typically smooth. Those formed in caves where the water supply is seasonal may reveal growth rings similar to those of a tree trunk. Stalactites and stalagmites grow by only a fraction of an inch or centimeter in a year, and since some are many yards or meters long, one can appreciate the time it takes for these speleothems to develop.

The most bizarre of speleothems are called helictites. Helictites are hollow, cylindrical formations that grow and twist in a number of directions and are not simply oriented according to the gravitational pull of a water drop. Other influences such as crystal growth patterns and air currents influence the direction in which these speleothems grow. Helictites grow out from the side of other speleothems and rarely grow larger than 4 in (8.5 cm) in length.

Speleothems called anthodites are usually made of aragonite. Calcite and aragonite are both forms of calcium carbonate, but crystallize differently. Anthodites grow as radiating, delicate, needle-like crystals . Pools of seepage water that drain leave behind round formations called cave popcorn. Cave pearls are formed in seepage pools by grains of sand encrusted with calcite; flowing water moves the grains about and they gather concentric layers of calcite.

See also Erosion; Stalactites and stalagmites

Cave

A cave is a naturally occurring hollow area inside Earth. All caves are formed by some type of erosion process. The study of caves is called speleology (pronounced spee-lee-OL-o-gee). While some caves may be small hillside openings, others may consist of large chambers and inter-connecting tunnels and mazes. Openings to the surface may be large gaping holes or small crevices.

Caves have served as shelter for people throughout history. Many religious traditions have regarded caves as sacred and have used them in rituals and ceremonies. Human remains, artifacts, sculptures, and drawings found in caves have aided archaeologists in learning about early humans. A cave discovered in southeastern France in 1994 contains wall paintings estimated to be more than 30,000 years old.

Cave formation

The most common, largest, and spectacular caves are solution caves. These caves are formed through the chemical interaction of air, soil, water, and rock. As water flows over and drains into Earth's surface, it mixes with carbon dioxide from the air and soil to form a mild solution of carbonic acid. Seeping through naturally occurring cracks and fissures in massive beds of limestone in bedrock (the solid rock that lies beneath the soil), the acidic water eats away at the rock, dissolving its minerals and carrying them off in a solution.

With continual water drainage, the fissures become established passageways. The passageways eventually enlarge and often connect, creating an underground drainage system. Sometimes ceilings fall and passageways collapse, creating new spaces and drainage routes. Over thousands, perhaps millions of years, these passages evolve into the caves we see today.

Several distinctive features in the landscape make cave terrain easy to identify. The most common is a rugged land surface, marred by sinkholes, circular depressions where the underlying rock has been dissolved away. Disappearing streams and natural bridges are also common clues. But entrances to solution caves are not always obvious, and their discovery is sometimes quite by accident.

Words to Know

Speleology: Scientific study of caves and their plant and animal life.

Stalactite: Cylindrical or icicle-shaped mineral deposit projecting downward from the roof of a cave.

Stalagmite: Cylindrical or upside down icicle-shaped mineral deposit projecting upward from the floor of a cave.

Cave environment

A deep cave is completely dark, has a stable atmosphere, and has an almost constant temperature. The humidity in limestone caves is usually near 100 percent. Many caves contain unique life-forms, underground streams and lakes, and unusual mineral formations.

Water that makes its way to a cave ceiling hangs as a drop. The damp atmosphere in a cave reacts with that water, forcing the dissolved mineral out of the water solution. The crystalline material that most often remains is called calcite. Calcite deposited on the ceiling creates a hanging icicle-shaped formation called a stalactite (pronounced sta-LACK-tite). Calcite deposited on the floor of a cave builds up to create an upside down icicle-shaped formation called a stalagmite (pronounced

sta-LAG-mite). Stalactites and stalagmites grow by only a fraction of an inch or centimeter a year. In time, two such formations often merge to form a stout floor-to-ceiling column.

Sometimes the water runs down the slope of the wall, and as the calcite is deposited, a low ridge forms. Subsequent drops of water follow the ridge, adding more calcite. Constant buildup of calcite in this fashion results in the formation of a wavy, folded sheet hanging from the ceiling called a curtain. Curtain formations often have streaks of various shades of off-white and brown.

Cave life

Three different groups of animals use or inhabit caves. Animals in the first group commonly use caves but depend on the outside world for survival. These include bats, birds, bears, and crickets. Those in the second group live their entire life cycle within a cave, generally near the entrance, but are also found living outside caves. Cockroaches, beetles, and millipedes are some examples of this second group. The last group comprises animals that are permanent deep cave dwellers. Because they often live in total darkness, these animals lack skin color and eyes. They rely on their sense of touch to get around. Examples of this group include fish, shrimp, crayfish, salamanders, worms, snails, insects, bacteria, fungi, and algae.

cave a cavity in the earth's surface usually large enough for a person to enter. Caves may be formed by the chemical and mechanical action of a stream upon soluble or soft rock, of rainwater seeping through soluble rock to the groundwater level, or of waves dashed against a rocky shore. Volcanic action (accompanied by the formation of gas pockets in lava or the melting of ice under lava) and earthquakes or other earth movements are also sources of cave formation. Limestone regions almost invariably have caves; some of these are notable for their stalactite and stalagmite formations or for their magnitude and beauty.

The preserved remains of prehistoric humans and animals and indications of early human culture have been discovered in some caves. Caves have served as burial grounds and shelter since prehistoric times. One such cave is Alabama's Russell Cave, where human evidence dates back 9,000 years. Speleology, the scientific study of caves and their plant and animal life, contributes to knowledge of biological adaptation and evolution. Some cave animals lack sight, and both plants and animals living where light is excluded show loss of pigment. Deep cave ecosystems, lacking the sunlight necessary for photosynthesis, depend on bacteria that use chemosynthesis to create energy.

Among famous caves in the United States are Carlsbad Caverns National Park (N.Mex.), Mammoth Cave National Park (Ky.), Wind Cave National Park (Black Hills, S.Dak.), Luray Caverns (Va.), and Wyandotte Cave (Ind.). In Europe there are celebrated caves in Belgium, Dalmatia, Gibraltar, Capri, Sicily, Postojna, and England (Kent's Cavern and Kirkdale). The caves of the Pyrenees and the Dordogne are famed for their prehistoric paintings (see Paleolithic art ), and those of Ajanta, India, and Dunhuang, China, for their Buddhist frescoes. Among the deepest known caves are Krubera in the nation of Georgia, which extends more than 6,500 ft (2,000 m) below the surface, and Lamprechtsofen in Austria.

Bibliography: See C. E. Mohr and T. L. Poulson, The Life of the Cave (1966); D. R. McClurg, The Amateur's Guide to Caves and Caving (1973).

cave. The natural hollow in a mountain, hill, or cliff has been the subject of much speculation in the Celtic imagination. It is often the realm of the fairy or a route to the Otherworld. One tradition has Oisín living in a cave for 300 years. Creatures who live in caves include the ciuthach (see cughtagh of Scottish Gaelic tradition, the buggane and cughtagh on the Isle of Man, and Luchtigern in the famous cave of Dunmore, Co. Kilkenny, Ireland. The name of Forgall Monach's fortress, Lusca, employs an old word for cave. Caves were often entrances to the Otherworld. See John Rhŷs, ‘Welsh Cave Legends’, in Celtic Folklore (Oxford, 1891) 456–96. See also FINGAL'S CAVE; CRUACHAIN; LOUGH DERG (1). ModIr. uaimh; ScG uaimh; Manx ooig; W ogof; Corn. fogo, gogo, ogo; Bre. kev.

cave / ˈkāv/ • n. a large underground chamber, typically of natural origin, in a hillside or cliff. • v. [intr.] 1. explore caves as a sport. 2. short for cave in below. PHRASAL VERBS: cave in (or cave something in) (with reference to a roof or similar structure) subside or collapse or cause something to do this. ∎ fig. yield or submit under pressure: the manager caved in to his demands. DERIVATIVES: cave·like / -ˌlīk/ adj. cav·er n.

cave Natural underground cavity. There are several kinds, including coastal caves, formed by wave erosion, ice caves, formed in glaciers, and lava caves. The largest caves are formed in carbonate rocks such as limestone.

cave 2 fall in over a hollow. XVIII. prob. var. of dial. (esp. eastern) calve (XVIII), cauve, which may be of LG. orig.; cf. WFlem. inkalven fall in, Du. afkalven fall away, uitkalven fall out.

cave 1 underground hollow. XIII. -(O)F. (now ‘cellar’) — L. cava, sb. use of fem. sg. or n. pl. of cavus hollow.

Cave

a small group of politicians who break away from the main party; a splinter party.

Example: cave of Adullam, 1866.

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