Karst phenomena exist in areas in the eastern part of Saudi Arabia, fo
rming solution features such as sinkholes, collapsed dolines and solut
ion caverns, as a result of the chemical leaching of the carbonate and
evaporite formations by percolating water. The instability of these k
arst phenomena could produce land subsidence problems. This paper revi
ews the geology of documented karstic rock units in Saudi Arabia and p
roposes a simple engineering classification of the solution features c
haracteristic of limestone. Two case histories in the Dhahran area, ea
stern Saudi Arabia, will be used as examples for the application of a
modified engineering classification.