The rapid underground dissolution of gypsum, and the evolution of the gypsu
m karst in Lithuania and England, results in subsidence problems which can
make construction difficult. The natural dissolution yields sulphate-rich g
roundwater of poor quality and the karst is susceptible to the rapid transm
ission of pollutants.
In the north of Lithuania gypsum karst is developed in Devonian gypsum. Her
e the towns of Birai, Pasvalys and the surrounding countryside suffer subsi
dence and some buildings have been damaged. The majority of the potable wat
er in these areas is derived from groundwater extracted from sandstone sequ
ences that underlie the gypsum. In Lithuania conservation measures have bee
n introduced to control agriculture and prevent pollution of the gypsum kar
st. These measures include environmentally-friendly farming, restrictions o
n land use and exclusion zones around subsidence hollows.
In England subsidence caused by the dissolution of Permian gypsum has cause
d severe problems in the vicinity of the town of Ripen. Numerous buildings
have been damaged and new sites are difficult to develop. Here formal plann
ing regulations have recently been introduced to help to protect against th
e worst effects of subsidence resulting from gypsum dissolution. (C) 1999 E
lsevier Science B.V. All rights reserved.