The occurrence of land subsidence in the Kingdom Saudi Arabia is eithe
r natural or manmade. Natural land subsidence occurs due to the develo
pment of subterranean voids by a solution of host rocks in carbonate a
nd evaporite terrains, over many areas of Saudi Arabia. Man-induced la
nd subsidence is either due to the removal of groundwater in the agric
ultural areas or to wetting of unstable soils. Therefore, earth fissur
es and a lowering of the ground surface in unconsolidated sediments to
ok place in alluvial plains and volcanic vent terrains. Unstable soils
include Sabkha soils and loess sediments. These types of soils occur
in coastal plains, desert areas and volcanic terrains. When this soil
is wetted either during agricultural activities, waste disposal or eve
n during a rain storm, subsidence takes place due to either the remova
l of salts from the Sabkha soil or the rearrangement of soil particles
in loess sediments.