The impact of mining subsidence on the environment can occasionally be very
catastrophic, destroying property and even leading to the loss of life. Us
ually, however, such subsidence gives rise to varying degrees of structural
damage that can range from slight to very severe. Different types of miner
al deposits have been mined in different ways and this determines the natur
e of the associated subsidence. Some mining methods result in contemporaneo
us subsidence whereas, with others, subsidence A number of different minera
l deposits have been chosen to illustrate the different types of associated
subsidence that result and the problems that arise. The examples provided
are gold mining in the Johannesburg area; bord and pillar mining of coal in
the Witbank Coalfield, South Africa; long-wall mining of coal in the Ruhr
district; mining of chalk and limestone in Suffolk and the West Midlands, r
espectively; and solution mining of salt in Cheshire. These mineral deposit
s have often been worked for more than 100 years and, therefore, a major pr
oblem results from abandoned mines, especially those at shallow depth, the
presence of which is unrecorded. Abandoned mines at shallow depth can repre
sent a serious problem in areas that are being developed or redevdoped. Abs
traction of natural brine has given rise to subsidence with its own particu
lar problems and cannot be predicted. Although such abstraction is now inco
nsequential in Cheshire, dereliction associated with past subsidence still
remains.