Геологические провалы и карстовые воронки.

Geologically formed topological depression

A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are also known as shakeholes, and to openings where surface water enters into underground passages known as ponor, swallow hole or swallet. A cenote is a type of sinkhole that exposes groundwater underneath. Sinkholes are usually circular and vary in size from tens to hundreds of meters both in diameter and depth, and vary in form from soil lined bowls to bedrock edged chasms. Sinkholes may form gradually or suddenly, and are found worldwide. The formation of sinkholes involves natural processes of erosion or gradual removal of slightly soluble bedrock (such as limestone) by percolating water, the collapse of a cave roof, or a lowering of the water table. Sinkholes often form through the process of suffosion. For example, groundwater may dissolve the carbonate cement holding the sandstone particles together and then carry away the lax particles, gradually forming a void. Occasionally a sinkhole may exhibit a visible opening into a cave below. In the case of exceptionally large sinkholes, such as the Minyé sinkhole in Papua New Guinea or Cedar Sink at Mammoth Cave National Park in Kentucky, an underground stream or river may be visible across its bottom flowing from one side to the other. Sinkholes are common where the rock below the land surface is limestone or other carbonate rock, salt beds, or in other soluble rocks, such as gypsum, that can be dissolved naturally by circulating ground water. Sinkholes also occur in sandstone and quartzite terrains. As the rock dissolves, spaces and caverns develop underground. These sinkholes can be dramatic, because the surface land usually stays intact until there is not enough support. Then, a sudden collapse of the land surface can occur.

On 2 July 2015, scientists reported that active pits, related to sinkhole collapses and possibly associated with outbursts, were found on the comet 67P/Churyumov Gerasimenko by the Rosetta space probe.

Collapses, commonly incorrectly labeled as sinkholes, also occur due to human activity, such as the collapse of abandoned mines and salt cavern storage in salt domes in places like Louisiana, Mississippi and Texas, in the United States of America. More commonly, collapses occur in urban areas due to water main breaks or sewer collapses when old pipes give way. They can also occur from the overpumping and extraction of groundwater and subsurface fluids. Sinkholes can also form when natural water drainage patterns are changed and new water diversion systems are developed. Some sinkholes form when the land surface is changed, such as when industrial and runoff storage ponds are created; the substantial weight of the new material can trigger a collapse of the roof of an existing void or cavity in the subsurface, resulting in development of a sinkhole.

Solution or dissolution sinkholes form where water dissolves limestone under a soil covering. Dissolution enlarges natural openings in the rock such as joints, fractures, and bedding planes. Soil settles down into the enlarged openings forming a small depression at the ground surface.

Cover subsidence sinkholes form where voids in the underlying limestone allow more settling of the soil to create larger surface depressions. Soil collapse sinkholes, which are characterized by the collapse of cavities in soil that have developed where soil falls down into underlying rock cavities, pose the most serious hazards to life and property. Fluctuation of the water level accelerates this collapse process. When water rises up through fissures in the rock, it reduces soil cohesion. Later, as the water level moves downward, the softened soil seeps downwards into rock cavities. Flowing water in karst conduits carries the soil away, preventing soil from accumulating in rock cavities and allowing the collapse process to continue. Induced sinkholes occur where human activity alters how surface water recharges groundwater. Many human induced sinkholes occur where natural diffused recharge is disturbed and surface water becomes concentrated. Activities that can accelerate sinkhole collapses include timber removal, ditching, laying pipelines, sewers, water lines, storm drains, and drilling. These activities can increase the downward movement of water beyond the natural rate of groundwater recharge. Where large cavities exist in the limestone large surface collapses can occur, such the Winter Park, Florida sinkhole collapse. The greatest amount of karst sinkhole damage in the United States occurs in Florida, Texas, Alabama, Missouri, Kentucky, Tennessee, and Pennsylvania. The largest recent sinkhole in the USA is possibly one that formed in 1972 in Montevallo, Alabama, as a result of man made lowering of the water level in a nearby rock quarry. This "December Giant" or "Golly Hole" sinkhole measures 425 feet (130 m) long, 350 feet (107 m) wide and 150 feet (46 m) deep. Other areas of significant karst hazards include the Ebro Basin in northern Spain; the island of Sardinia; the Italian peninsula; the Chalk areas in southern England; Sichuan, China; Jamaica; France;Croatia; Bosnia and Herzegovina; Slovenia; and Russia, where one third of the total land area is underlain by karst.

Sinkholes tend to occur in karst landscapes. Karst landscapes can have up to thousands of sinkholes within a small area, giving the landscape a pock marked appearance. These sinkholes drain all the water, so there are only subterranean rivers in these areas. Examples of karst landscapes with numerous massive sinkholes include Khammouan Mountains (Laos) and Mamo Plateau (Papua New Guinea). The largest known sinkholes formed in sandstone are Sima Humboldt and Sima Martel in Venezuela. Powerful underground rivers may form on the contact between limestone and underlying insoluble rock, creating large underground voids. In such conditions, the largest known sinkholes of the world have formed, like the Xiaozhai Tiankeng (Chongqing, China), giant sótanos in Querétaro and San Luis Potosí states in Mexico and others. Unusual processes have formed the enormous sinkholes of Sistema Zacatón in Tamaulipas (Mexico), where more than 20 sinkholes and other karst formations have been shaped by volcanically heated, acidic groundwater. This has produced not only the formation of the deepest water filled sinkhole in the world—Zacatón—but also unique processes of travertine sedimentation in upper parts of sinkholes, leading to sealing of these sinkholes with travertine lids. The Murge area in southern Italy also has numerous sinkholes. Sinkholes can be formed in retention ponds from large amounts of rain. On the Arctic seafloor, methane emissions have caused large sinkholes to form.

Sinkholes have been used for centuries as disposal sites for various forms of waste. A consequence of this is the pollution of groundwater resources, with serious health implications in such areas. The Maya civilization sometimes used sinkholes in the Yucatán Peninsula (known as cenotes) as places to deposit precious items and human sacrifices. When sinkholes are very deep or connected to caves, they may offer challenges for experienced cavers or, when water filled, divers. Some of the most spectacular are the Zacatón cenote in Mexico (the world's deepest water filled sinkhole), the Boesmansgat sinkhole in South Africa, Sarisariñama tepuy in Venezuela, the Sótano del Barro in Mexico, and in the town of Mount Gambier, South Australia. Sinkholes that form in coral reefs and islands that collapse to enormous depths are known as blue holes and often become popular diving spots.

Large and visually unusual sinkholes have been well known to local people since ancient times. Nowadays sinkholes are grouped and named in site specific or generic names. Some examples of such names are listed below. Aven – In the south of France (this name means pit cave in the Occitan language). Black holes (not to be confused with cosmic black holes) – This term refers to a group of unique, round, water filled pits in the Bahamas. These formations seem to be dissolved in carbonate mud from above, by the sea water. The dark color of the water is caused by a layer of phototropic microorganisms concentrated in a dense, purple colored layer at depth; this layer "swallows" the light. Metabolism in the layer of microorganisms causes heating of the water. One of them is the Black Hole of Andros. Blue holes – This name was initially given to the deep underwater sinkholes of the Bahamas but is often used for any deep water filled pits formed in carbonate rocks. The name originates from the deep blue color of water in these sinkholes, which is created by the high clarity of the water and the great depth of the sinkholes; only the deep blue color of the visible spectrum can penetrate such depth and return after reflection. Cenotes – This refers to the characteristic water filled sinkholes in the Yucatán Peninsula, Belize and some other regions. Many cenotes have formed in limestone deposited in shallow seas created by the Chicxulub meteorite's impact. Dolina – Slavic toponym (from Slovene language dòla:"valley" or "dale"). The name is widely used in various slavic regions of Eastern Europe for sinkholes, including Romania. Foiba – Friulan Italian dialect word (from the Latin fŏvea: "pit" or "chasm"). The name, is given to sinkholes in the frontier zone between the Italian region of Friuli Venezia Giulia, Croatia and Slovenia, in the Karst Plateau. Sótanos – This name is given to several giant pits in several states of Mexico. Tiankengs – These are extremely large sinkholes, typically deeper and wider than , with mostly vertical walls, most often created by the collapse of caverns. The term means sky holes in Chinese; many of this largest type of sinkhole are located in China. Tomo – This term is used in New Zealand karst country to describe sinkholes. Vrtače – Used in Yugoslavia.

The 2010 Guatemala City sinkhole formed suddenly in May of that year; torrential rains from Tropical Storm Agatha and a bad drainage system were blamed for its creation. It swallowed a three story building and a house; it measured approximately wide and deep. A similar hole had formed nearby in February 2007. This large vertical hole is not a true sinkhole, as it did not form via the dissolution of limestone, dolomite, marble, or any other water soluble rock. Instead, they are examples of "piping pseudokarst", created by the collapse of large cavities that had developed in the weak, crumbly Quaternary volcanic deposits underlying the city. Although weak and crumbly, these volcanic deposits have enough cohesion to allow them to stand in vertical faces and to develop large subterranean voids within them. A process called "soil piping" first created large underground voids, as water from leaking water mains flowed through these volcanic deposits and mechanically washed fine volcanic materials out of them, then progressively eroded and removed coarser materials. Eventually, these underground voids became large enough that their roofs collapsed to create large holes. Examples have included, instances above World War I trenches in Ypres, Belgium; near mines in Nitra, Slovakia; and above an old gypsum mine in Magheracloone, Ireland. Lake Kashiba – Zambia. About in area and about deep.

Dean's Blue Hole – Bahamas. The second deepest known sinkhole under the sea, depth Popular location for world championships of free diving, as well as recreational diving.

Hranice Abyss, in the Moravia region of the Czech Republic, is the deepest known underwater cave in the world. The lowest confirmed depth (as of 27 September 2016) is 473 m (404 m below the water level). Maqluba, in Malta is a sinkhole with a surface area of around 4,765 square metres (51,290 sq ft) situated in the village of Qrendi in Malta. The diameter is around 50m, the depth is around 15m, and the perimeter 300m. Pozzo del Merro, near Rome, Italy. At the bottom of an conical pit, and approximately deep, it is among the deepest sinkholes in the world (see Sótano del Barro below). Red Lake – Croatia. Approximately deep pit with nearly vertical walls, contains an approximately deep lake. Gouffre de Padirac – France. It is deep, with a diameter of Visitors descend 75 m via a lift or a staircase to a lake allowing a boat tour after entering into the cave system which contains a 55 km subterranean river. Vouliagmeni – Greece. The sinkhole of Vouliagmeni is known as "The Devil Well", because it is considered extremely dangerous. Four scuba divers have died in it. Maximum depth of and horizontal penetration of Pouldergaderry – Ireland. This sinkhole is located in the townland of Kilderry South near Milltown, County Kerry at The sinkhole, which is located in an area of karst bedrock, is approximately in diameter and deep with many mature trees growing on the floor of the hole. At the level of the surrounding ground, the sinkhole covers an area of approximately 1.3 acres. Its presence is indicated on Ordnance Survey maps dating back to 1829.

Cave of Swallows – San Luis Potosí. deep, round sinkhole with overhanging walls. Puebla sinkhole – Santa Maria Zacatepec, Puebla. 400 feet (122 m) diameter and 50 feet (15 m) deep, it is still growing as of June 2021. 2021. Sima de las Cotorras – Chiapas. across, deep, with thousands of green parakeets and ancient rock paintings. Zacatón – Tamaulipas. Deepest water filled sinkhole in world, deep.

Amberjack Hole – blue hole located 30 mile (48 km) off the coast of Sarasota, Florida. Bayou Corne sinkhole – Assumption Parish, Louisiana. About 25 acres in area and 750 feet (229 m) deep. The Blue Hole – Santa Rosa, New Mexico. The surface entrance is only 80 feet (24 m) in diameter, it expands to a diameter of 130 feet (40 m) at the bottom. Daisetta Sinkholes – Daisetta, Texas. Several sinkholes have formed, the most recent in 2008 with a maximum diameter of 620 feet (189 m) and maximum depth of 150 feet (46 m). Devil's Millhopper – Gainesville, Florida. 120 feet (37 m) deep, 500 feet (152 m) wide. Twelve springs, some more visible than others, feed a pond at the bottom. Golly Hole or December Giant – Calera, Alabama. Appeared 2 December 1972. Approximately and 120 feet (37 m) deep. Grassy Cove – Cumberland County, Tennessee. in area and deep, a National Natural Landmark. Green Banana Hole – a blue hole located 50 mile (80 km) off the coast of Sarasota, Florida. Gypsum Sinkhole – Utah, in Capitol Reef National Park. Nearly in diameter and approximately deep. Kingsley Lake – Clay County, Florida. in area, deep and almost perfectly round. Lake Peigneur – New Iberia, Louisiana. Original depth 11 feet (3 m), currently 1300 feet (396 m) at Diamond Crystal Salt Mine collapse. Winter Park Sinkhole – Winter Park, Florida. Appeared 8 May 1981. It was approximately 350 feet (107 m) wide and 75 feet (23 m) deep. It was notable as one of the largest recent sinkholes to form in the United States. It is now known as Lake Rose.

Harwoods Hole – Abel Tasman National Park, New Zealand. deep.

Sima Humboldt – Bolívar, Venezuela. Largest sinkhole in sandstone, deep, with vertical walls. Unique, isolated forest on bottom. In the western part of Cerro Duida, Venezuela, there is a complex of canyons with sinkholes. Deepest sinkhole is deep (from lowest rim within canyon); total depth .