Sinkholes
Groundwater Data for the Nation
The USGS National Water Information System (NWIS) contains extensive groundwater data for thousands of sites nationwide.
It is a frightening thought to imagine the ground below your feet or house suddenly collapsing and forming a big hole in the ground. Sinkholes rarely happen, but when they strike, tragedy can occur. Sinkholes happen when the ground below the land surface cannot support the land surface. They happen for many reasons; read on to educate yourself about sinkholes.
• Water Science School HOME • Groundwater topics •
Sinkholes
![Image: Sinkholes in West-central Florida, Freeze Event of 2010](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/side_image/public/Sinkholes-Freeze_2010_-_063.jpg?itok=2yFwZp1A)
Credit: Ann Tihansky, USGS
Sinkholes are common where the rock below the land surface is limestone, carbonate rock, salt beds, or rocks that can naturally be dissolved by groundwater circulating through them. As the rock dissolves, spaces and caverns develop underground. Sinkholes are dramatic because the land usually stays intact for a while until the underground spaces just get too big. If there is not enough support for the land above the spaces, then a sudden collapse of the land surface can occur. These collapses can be small, or, as this picture shows, or they can be huge and can occur where a house or road is on top.
The most damage from sinkholes tends to occur in Florida, Texas, Alabama, Missouri, Kentucky, Tennessee, and Pennsylvania.
What is a "sinkhole"?
A sinkhole is an area of ground that has no natural external surface drainage--when it rains, the water stays inside the sinkhole and typically drains into the subsurface. Sinkholes can vary from a few feet to hundreds of acres and from less than 1 to more than 100 feet deep. Some are shaped like shallow bowls or saucers whereas others have vertical walls; some hold water and form natural ponds.
Typically, sinkholes form so slowly that little change is noticeable, but they can form suddenly when a collapse occurs. Such a collapse can have a dramatic effect if it occurs in an urban setting.
Areas prone to collapse sinkholes
The map below shows areas of the United States where certain rock types that are susceptible to dissolution in water occur. In these areas the formation of underground cavities can form, and catastrophic sinkholes can happen. These rock types are evaporites (salt, gypsum, and anhydrite) and carbonates (limestone and dolomite). Evaporite rocks underlie about 35 to 40 percent of the United States, though in many areas they are buried at great depths.
![Map of U.S. showing karst areas, which are prone to land subsidence and sinkholes.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/full_width/public/thumbnails/image/wss-gw-sinkhole-karst-map-us.jpg?itok=uh38lRoX)
Types of sinkholes
Since Florida is prone to sinkholes, it is a good place to use to discuss some different types of sinkholes and the geologic and hydrologic processes that form them. The processes of dissolution, where surface rock that are soluble to weak acids, are dissolved, and suffusion, where cavities form below the land surface, are responsible for virtually all sinkholes in Florida.
DISSOLUTION SINKHOLES
Dissolution of the limestone or dolomite is most intensive where the water first contacts the rock surface. Aggressive dissolution also occurs where flow is focused in preexisting openings in the rock, such as along joints, fractures, and bedding planes, and in the zone of water-table fluctuation where groundwater is in contact with the atmosphere.
Rainfall and surface water percolate through joints in the limestone. Dissolved carbonate rock is carried away from the surface and a small depression gradually forms. On exposed carbonate surfaces, a depression may focus surface drainage, accelerating the dissolution process. Debris carried into the developing sinkhole may plug the outflow, ponding water and creating wetlands. Gently rolling hills and shallow depressions caused by solution sinkholes are common topographic features throughout much of Florida.
![Diagram showing how dissolution sinkholes form as subsurface rock dissolves by water.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/full_width/public/thumbnails/image/wss-gw-sinkholes-dissolution.gif?itok=qq46FMEN)
COVER-SUBSIDENCE SINKHOLES
Cover-subsidence sinkholes tend to develop gradually where the covering sediments are permeable and contain sand. In areas where cover material is thicker, or sediments contain more clay, cover-subsidence sinkholes are relatively uncommon, are smaller, and may go undetected for long periods.
- Granular sediments spall into secondary openings in the underlying carbonate rocks.
- A column of overlying sediments settles into the vacated spaces (a process termed “piping”).
- Dissolution and infilling continue, forming a noticeable depression in the land surface.\
- The slow downward erosion eventually forms small surface depressions 1 inch to several feet in depth and diameter.
In areas where cover material is thicker, or sediments contain more clay, cover-subsidence sinkholes are relatively uncommon, are smaller, and may go undetected for long periods.
COVER-COLLAPSE SINKHOLES
Cover-collapse sinkholes may develop abruptly (over a period of hours) and cause catastrophic damages. They occur where the covering sediments contain a significant amount of clay. Over time, surface drainage, erosion, and deposition of sinkhole into a shallower bowl-shaped depression. Over time, surface drainage, erosion, and deposition of sediment transform the steep-walled sinkhole into a shallower bowl-shaped depression.
- Sediments spall into a cavity
- As spalling continues, the cohesive covering sediments form a structural arch.
- The cavity migrates upward by progressive roof collapse.
- The cavity eventually breaches the ground surface, creating sudden and dramatic sinkholes.
![Diagram showing how cover-collapse types of sinkholes develop.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/full_width/public/thumbnails/image/wss-gw-sinkholes-cover-collapse.gif?itok=jvxooDzE)
Sinkholes can be human-induced
New sinkholes have been correlated to land-use practices, especially from groundwater pumping and from construction and development practices. 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 an underground collapse of supporting material, thus causing a sinkhole.
The overburden sediments that cover buried cavities in the aquifer systems are delicately balanced by groundwater fluid pressure. The water below ground is actually helping to keep the surface soil in place. Groundwater pumping for urban water supply and for irrigation can produce new sinkholes in sinkhole-prone areas. If pumping results in a lowering of groundwater levels, then underground structural failure, and thus, sinkholes, can occur.
![Water Science School Quiz](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/side_image/public/thumbnails/image/wss-icon-small-quiz1.gif?itok=ZNFqSSjm)
Do you think you know about groundwater?
Take our Groundwater true/false quiz, part of our Activity Center.
Sources and more information
- Sinkholes, USGS Fact Sheet 2007-3060
- Land Subsidence in the United States, USGS Circular 1182
- Land Subsidence in the United States, USGS Fact Sheet-165-00
- Karst in the United States: A Digital Map Compilation and Database, USGS Open-File Report 2014–1156
- Carbonate-rock aquifers, USGS Aquifer Basics website
Quiz icon made by mynamepong from www.flaticon.com
![Follow Drippy to learn more about current USGS research](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/side_image/public/thumbnails/image/Drippy_chalkboard_wma.png?itok=JF4fiofQ)
Want to learn more about sinkholes? Follow me to the Land Subsidence website!
Below are other science topics associated with sinkholes and land subsidence.
Groundwater Information by Topic
Aquifers and Groundwater
Infiltration and the Water Cycle
Land Subsidence
Groundwater True/False Quiz
Groundwater Storage and the Water Cycle
How the U.S. Geological Survey Monitors Water
Groundwater Flows Underground
Below are publications associated with groundwater, sinkholes and land subsidence.
A primer on ground water
Land subsidence in the United States
Measuring land subsidence from space
Land subsidence in the United States
Ground water and the rural homeowner
Below are news stories associated with sinkholes and land subsidence.
Below are FAQ associated with sinkholes and land subsidence.
What is the difference between a sinkhole and land subsidence?
Sinkholes are just one of many forms of ground collapse, or subsidence. Land subsidence is a gradual settling or sudden sinking of the Earth’s surface owing to subsurface movement of earth materials. The principal causes of land subsidence are aquifer-system compaction, drainage of organic soils, underground mining, hydrocompaction, natural compaction, sinkholes, and thawing permafrost. Land...
What is a sinkhole?
A sinkhole is a depression in the ground that has no natural external surface drainage. Basically, this means that when it rains, all of the water stays inside the sinkhole and typically drains into the subsurface. Sinkholes are most common in what geologists call, “ karst terrain .” These are regions where the types of rock below the land surface can naturally be dissolved by groundwater...
How many sinkholes open up in a year?
There is no database of sinkhole collapses for the United States, so these data are unavailable. Some individual state geologic surveys track reported collapses within their state. Many sinkhole collapses are not reported to authorities or news organizations, and many occur in rural areas where they are unobserved. Learn more: USGS Water Science School - Sinkholes
It is a frightening thought to imagine the ground below your feet or house suddenly collapsing and forming a big hole in the ground. Sinkholes rarely happen, but when they strike, tragedy can occur. Sinkholes happen when the ground below the land surface cannot support the land surface. They happen for many reasons; read on to educate yourself about sinkholes.
• Water Science School HOME • Groundwater topics •
Sinkholes
![Image: Sinkholes in West-central Florida, Freeze Event of 2010](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/side_image/public/Sinkholes-Freeze_2010_-_063.jpg?itok=2yFwZp1A)
Credit: Ann Tihansky, USGS
Sinkholes are common where the rock below the land surface is limestone, carbonate rock, salt beds, or rocks that can naturally be dissolved by groundwater circulating through them. As the rock dissolves, spaces and caverns develop underground. Sinkholes are dramatic because the land usually stays intact for a while until the underground spaces just get too big. If there is not enough support for the land above the spaces, then a sudden collapse of the land surface can occur. These collapses can be small, or, as this picture shows, or they can be huge and can occur where a house or road is on top.
The most damage from sinkholes tends to occur in Florida, Texas, Alabama, Missouri, Kentucky, Tennessee, and Pennsylvania.
What is a "sinkhole"?
A sinkhole is an area of ground that has no natural external surface drainage--when it rains, the water stays inside the sinkhole and typically drains into the subsurface. Sinkholes can vary from a few feet to hundreds of acres and from less than 1 to more than 100 feet deep. Some are shaped like shallow bowls or saucers whereas others have vertical walls; some hold water and form natural ponds.
Typically, sinkholes form so slowly that little change is noticeable, but they can form suddenly when a collapse occurs. Such a collapse can have a dramatic effect if it occurs in an urban setting.
Areas prone to collapse sinkholes
The map below shows areas of the United States where certain rock types that are susceptible to dissolution in water occur. In these areas the formation of underground cavities can form, and catastrophic sinkholes can happen. These rock types are evaporites (salt, gypsum, and anhydrite) and carbonates (limestone and dolomite). Evaporite rocks underlie about 35 to 40 percent of the United States, though in many areas they are buried at great depths.
![Map of U.S. showing karst areas, which are prone to land subsidence and sinkholes.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/full_width/public/thumbnails/image/wss-gw-sinkhole-karst-map-us.jpg?itok=uh38lRoX)
Types of sinkholes
Since Florida is prone to sinkholes, it is a good place to use to discuss some different types of sinkholes and the geologic and hydrologic processes that form them. The processes of dissolution, where surface rock that are soluble to weak acids, are dissolved, and suffusion, where cavities form below the land surface, are responsible for virtually all sinkholes in Florida.
DISSOLUTION SINKHOLES
Dissolution of the limestone or dolomite is most intensive where the water first contacts the rock surface. Aggressive dissolution also occurs where flow is focused in preexisting openings in the rock, such as along joints, fractures, and bedding planes, and in the zone of water-table fluctuation where groundwater is in contact with the atmosphere.
Rainfall and surface water percolate through joints in the limestone. Dissolved carbonate rock is carried away from the surface and a small depression gradually forms. On exposed carbonate surfaces, a depression may focus surface drainage, accelerating the dissolution process. Debris carried into the developing sinkhole may plug the outflow, ponding water and creating wetlands. Gently rolling hills and shallow depressions caused by solution sinkholes are common topographic features throughout much of Florida.
![Diagram showing how dissolution sinkholes form as subsurface rock dissolves by water.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/full_width/public/thumbnails/image/wss-gw-sinkholes-dissolution.gif?itok=qq46FMEN)
COVER-SUBSIDENCE SINKHOLES
Cover-subsidence sinkholes tend to develop gradually where the covering sediments are permeable and contain sand. In areas where cover material is thicker, or sediments contain more clay, cover-subsidence sinkholes are relatively uncommon, are smaller, and may go undetected for long periods.
- Granular sediments spall into secondary openings in the underlying carbonate rocks.
- A column of overlying sediments settles into the vacated spaces (a process termed “piping”).
- Dissolution and infilling continue, forming a noticeable depression in the land surface.\
- The slow downward erosion eventually forms small surface depressions 1 inch to several feet in depth and diameter.
In areas where cover material is thicker, or sediments contain more clay, cover-subsidence sinkholes are relatively uncommon, are smaller, and may go undetected for long periods.
COVER-COLLAPSE SINKHOLES
Cover-collapse sinkholes may develop abruptly (over a period of hours) and cause catastrophic damages. They occur where the covering sediments contain a significant amount of clay. Over time, surface drainage, erosion, and deposition of sinkhole into a shallower bowl-shaped depression. Over time, surface drainage, erosion, and deposition of sediment transform the steep-walled sinkhole into a shallower bowl-shaped depression.
- Sediments spall into a cavity
- As spalling continues, the cohesive covering sediments form a structural arch.
- The cavity migrates upward by progressive roof collapse.
- The cavity eventually breaches the ground surface, creating sudden and dramatic sinkholes.
![Diagram showing how cover-collapse types of sinkholes develop.](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/full_width/public/thumbnails/image/wss-gw-sinkholes-cover-collapse.gif?itok=jvxooDzE)
Sinkholes can be human-induced
New sinkholes have been correlated to land-use practices, especially from groundwater pumping and from construction and development practices. 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 an underground collapse of supporting material, thus causing a sinkhole.
The overburden sediments that cover buried cavities in the aquifer systems are delicately balanced by groundwater fluid pressure. The water below ground is actually helping to keep the surface soil in place. Groundwater pumping for urban water supply and for irrigation can produce new sinkholes in sinkhole-prone areas. If pumping results in a lowering of groundwater levels, then underground structural failure, and thus, sinkholes, can occur.
![Water Science School Quiz](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/side_image/public/thumbnails/image/wss-icon-small-quiz1.gif?itok=ZNFqSSjm)
Do you think you know about groundwater?
Take our Groundwater true/false quiz, part of our Activity Center.
Sources and more information
- Sinkholes, USGS Fact Sheet 2007-3060
- Land Subsidence in the United States, USGS Circular 1182
- Land Subsidence in the United States, USGS Fact Sheet-165-00
- Karst in the United States: A Digital Map Compilation and Database, USGS Open-File Report 2014–1156
- Carbonate-rock aquifers, USGS Aquifer Basics website
Quiz icon made by mynamepong from www.flaticon.com
![Follow Drippy to learn more about current USGS research](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/side_image/public/thumbnails/image/Drippy_chalkboard_wma.png?itok=JF4fiofQ)
Want to learn more about sinkholes? Follow me to the Land Subsidence website!
Below are other science topics associated with sinkholes and land subsidence.
Groundwater Information by Topic
Aquifers and Groundwater
Infiltration and the Water Cycle
Land Subsidence
Groundwater True/False Quiz
Groundwater Storage and the Water Cycle
How the U.S. Geological Survey Monitors Water
Groundwater Flows Underground
Below are publications associated with groundwater, sinkholes and land subsidence.
A primer on ground water
Land subsidence in the United States
Measuring land subsidence from space
Land subsidence in the United States
Ground water and the rural homeowner
Below are news stories associated with sinkholes and land subsidence.
Below are FAQ associated with sinkholes and land subsidence.
What is the difference between a sinkhole and land subsidence?
Sinkholes are just one of many forms of ground collapse, or subsidence. Land subsidence is a gradual settling or sudden sinking of the Earth’s surface owing to subsurface movement of earth materials. The principal causes of land subsidence are aquifer-system compaction, drainage of organic soils, underground mining, hydrocompaction, natural compaction, sinkholes, and thawing permafrost. Land...
What is a sinkhole?
A sinkhole is a depression in the ground that has no natural external surface drainage. Basically, this means that when it rains, all of the water stays inside the sinkhole and typically drains into the subsurface. Sinkholes are most common in what geologists call, “ karst terrain .” These are regions where the types of rock below the land surface can naturally be dissolved by groundwater...
How many sinkholes open up in a year?
There is no database of sinkhole collapses for the United States, so these data are unavailable. Some individual state geologic surveys track reported collapses within their state. Many sinkhole collapses are not reported to authorities or news organizations, and many occur in rural areas where they are unobserved. Learn more: USGS Water Science School - Sinkholes