Sinkholes (or dolines)

Modified from the BGS Engineering Geology (Superfical) map of the UK, 2011; adapted from Waltham, A C, Bell, F G and Culshaw, M G. 2005. Sinkholes and subsidence: karst and cavernous rocks in engineering and construction. Springer Berlin.

Sinkhole over gypsum, Sutton Howgrave, North Yorkshire.

Sinkholes formed on Chalk due to a burst water pipe at Fontwell, Sussex.

Collapse of four garages into subsidence hollow caused by the dissolution of gypsum at Ripon, North Yorkshire, 1997.

Soluble rocks in the UK.

The study of sinkholes has attracted considerable media attention since the tragic death of a man at Seffner near Tampa, Florida, on 1 March 2013 — Sinkhole swallows up Florida man Jeffrey Bush | BBC News

A sinkhole, that had formed beneath Mr Bush's house, 'swallowed' him when the house floor collapsed.

Later in March 2013, a golfer was injured when a sinkhole opened up on the fairway of an Illinois golf course.

Recent events

Increased incidence of sinkholes and collaspse subsidence features:

UAV aerial view of Ripon sinkhole in November 2016Magdalen Road, Ripon sinkhole November 2016

An account of the most recent sinkhole to appear in the Ripon area.

Figure 1: Surface depression remnant from sinkhole adjacent to the A38 at Caton, DevonCaton Karst, Devon Monday 6 June 2016

An account of the most recent sinkhole to appear in the Devon area.

Denehole at Rainham Mark Grammar School 2014Deneholes

An example of how ancient mine workings can lead to collapse subsidence.
‘Sinkhole’ in the middle of the M2: February 2014

Sinkhole in Ripon 1997Increased incidence of sinkholes and subsidence collapse features in 2014

The sustained period of wet weather is suspected to be the trigger for the recent spate of sinkholes and collapse subsidence features that have been reported in the south and south-east.

Sinkhole in Ripon 2014Sinkhole at Magdalen's Close, Ripon, Monday 17 February 2014

Dr Anthony Cooper, gives an account of the most recent sinkhole to appear in the Ripon area.

Report a sinkhole

Report a sinkhole or share other geological observations using our iGeology mobile app!

What causes sinkholes and where do they occur in the UK?

There are several different types of sinkhole — sometimes called dolines:

Some result from the surface dissolution of the soluble rock (solution sinkholes) — for example limestone rocks dissolve when attacked by rainfall or groundwater that is acidic.

Sinkholes also occur where a thin covering of loose superficial material such as sand, clay or soil covers the soluble rocks beneath. In this setting, the soil can be washed into solutionally widened fissures below, leading to the development of a cavity within the overlying material.

If the cover material is sandy, it will tend to gradually slump into the fissures, slowly creating a sinkhole over time (suffosion sinkhole).

However, if the material is more cohesive, like clay, then the cavity can grow quite large before suddenly collapsing; a process termed a 'drop out' sinkhole. It is these more spectacular collapses that sometimes hit the headlines.

Gradual cave collapse

In other cases, it is the gradual collapse of a cave passage at depth that can trigger a sinkhole.

The collapse can gradually propagate up through the overlying strata to cause subsidence at the surface (a 'collapse sinkhole'). These sometimes extend up into rocks that are not themselves prone to dissolution, creating a 'caprock sinkhole'.

These are common in parts of South Wales where sandstone rocks overlie cavernous limestone and in Ripon where sandstone and limestone overlie gypsum. Others may be buried by more recent deposits.

Underground water flow

Some sinkholes are caused not by dissolution of limestone, but the erosion of weak unconsolidated material by flowing water. Loose material can removed by a process called ‘soil piping’, creating large voids within the sediment.

One of the most spectacular examples of this type of collapse is the event that occurred in May 2010 in Guatemala City. Here, cavities developed in weak, unconsolidated, volcanic deposits following a tropical storm. These then collapsed, creating a shaft approximately 100 m deep and 20 m wide.

What triggers sinkholes?

Several things can trigger sinkholes. The simple process of gradual dissolution can cause a sinkhole to form at the surface.

However, other factors, including humans can induce sinkholes to form, such as:

  • Heavy rain or surface flooding can initiate the collapse of normally stable cavities, especially those developed within superficial deposits.
  • Leaking drainage pipes, burst water mains, irrigation or even the act of emptying a swimming pool are all documented examples of sinkhole triggers.

Building works

Construction and development are also potential triggers. Modifying surface drainage or altering the loads imposed on the ground without adequate support can caused sinkholes to develop.

Changes in water table level

In some parts of the world, drought or groundwater abstraction can cause sinkholes by changing the level of the water-table. This removes the buoyant support water provides to a cavity. Draining these cavities can cause them to collapse.


Mining can be a factor in causing sinkholes, either by dewatering and lowering of the water-table, or by intercepting clay filled voids which subsequently collapse. Several sinkholes in Norwich have been caused by old chalk mines intercepting otherwise stable sediment-filled voids.

Sinkholes in the UK

Areas prone to sinkhole formation occur throughout the UK, although most are relatively small or are in upland rural locations.

These include areas underlain by Carboniferous limestones, notably the Mendips, parts of Wales, the Peak District, and the northern Pennines including the Yorkshire Dales.

The Chalk is also susceptible, especially where it is covered by younger clay and sand deposits (the 'Clay-with Flints' and Palaeogene strata), notably in parts of Dorset, Hampshire and the Chilterns.

Gypsum areas at most risk

However, the most susceptible area in the UK is the Permian gypsum deposits of north-east England, particularly around Ripon.

Many large sinkholes have developed around Ripon, some of which have affected property and infrastructure. This is because gypsum is far more soluble than limestone, and thus dissolves more rapidly.


Sinkholes also occur over salt deposits, commonly in areas such as Cheshire where brine has been extracted making it difficult to separate naturally formed sinkholes from those created by man.

In Scotland, sinkholes are generally rare except in parts of Assynt underlain by the Cambrian Durness limestone.

Dealing with sinkholes

The hazards associated with sinkholes can be mitigated by appropriate planning, good site investigation (with geophysics and boreholes), appropriate design and proper maintenance of infrastructure such as drains and services.

Care is required when installing any structures that could affect the local groundwater flow or groundwater levels including soakaways (sustainable drainage systems or SUDs) and open loop ground source heat pumps; in some places on soluble rocks these may be impractical.

  • Ensure that areas and a safety perimeter are cordoned off and keep people away
  • Notify the landowner and/ or emergency services as appropriate
  • If services pipes, e.g. gas or water are left suspended ensure that infrastructure managers are contacted, e.g. Safety and emergencies (National Grid) and Emergencies (United Utilities)
  • Ensure that any triggering processes, e.g. leaking drains are managed to minimise the potential for ongoing subsidence
  • Contact your local council/building control to notify them; find out if there is a history of such features in the area, and request a list of consulting engineers that are able to give appropriate advice on the correct procedures for stabilising them
  • The BGS can be approached for more information on sinkholes (contacts details below) or read our specific home owner advice
  • If the concern is about whether a sinkhole is developing on a specific property monitor any suspect depressions, check that there are no obvious potential triggering mechanisms, e.g. leaking pipes, check for any associated cracks in adjacent buildings and seek guidance from your council/building control as indicated above.

More information

The BGS provides information regarding the susceptibility of the ground to dissolution and mining. This does not include information on the associated likelihood. The likelihood of occurrence is also linked to the history of the development of a site, for example many sites will have been remediated. Additionally, the distribution of medieval workings is poorly documented and the available information on mines is limited.

If you wish to know whether your area is prone to sinkholes, you can find out by visiting our Caves, subsidence and soluble rocks pages or by using BGS GeoSure data to access information on these geological hazards.

The methodology behind the development of the BGS GeoSure dissolution hazard layer is outlined in the document below:

Farrant, A R, and Cooper, A.  2008  Karst geohazards in the UK: the use of digital data for hazard management.  Quarterly Journal of Engineering Geology and Hydrogeology, 41 (3), 339–356. 

Contact the Sinkhole Response Team

British Geological Survey
NG12 5GG
E-mail: Sinkhole team