Subsidence
According to the British Geological Survey, subsidence is defined as ground failure when the earth shrinks downward. When water wears bedrock down, the earth above it collapses into either a big circular pit or a long depressed line. When water, either from under or above ground percolates through the bedrock, the rock (like limestone) can easily be dissolved. We call this process dissolution. (Keller and Devecchio, 258)
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Sink hole in a back garden, St. Alban's, UK
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| The British Geological Survey maps out hazardous areas based on ground stability. Source: BGS |
Certain parts of Britain have proven to be more susceptible to subsidence due to the types of rock found there. Places like Cheshire and the Vale of York in the south east of England, for example is chock full (haha) of gypsum, which is basically chalk, and soft clay.
To decrease hazards, the British Geological survey is constantly working to create maps indicating places where the ground is weak and likely to collapse, and predicts places where the ground is likely to sink in or erode.

