An overview of the surface and near-surface geology, geomorphology and natural resources of Kuwait

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The surface and near-surface geology, geomorphology and natural resources of Kuwait have been reviewed based on the published work. The stratigraphy and structure of the near-surface sediments of Kuwait have been mainly controlled by the Tertiary tectonic activity of the Arabian Shield. The shield started separating from the African mainland by the close of the Eocene and drifted northeastward towards the Asian plate, giving rise to the folding and thrusting of the Zagros Mountains of Iran. The tectonic activity superimposed a northwest–southeast trend over an earlier north–south structural trend, and gave rise to parallel ridges and valleys trending northwest–southeast through differential erosion. It has been possible to identify 15 geomorphic zones and 11 morphostructures from analysis of the surface features of Kuwait. Seven of these morphostructures can be attributed to tectonic processes and two to fluvial processes. It has not been possible, however, to explain satisfactorily the origin of the Jal Az-Zor escarpment or the Ad-Dalmaniyah cliff. The whole of Kuwait can be divided into seven drainage zones. Of these, the internal drainage systems of the Ar-Raudhatain-Umm Al-Aish drainage system and the Ad-Dibdibba drainage system are hydrogeologically most important. The clastic deposits of Kuwait Group sediments, often affected by low-temperature carbonate (calcite and dolomite) and sulfate (gypsum) precipitation, form the surface rock of Kuwait. These are covered by recent aeolian and residual deposits; playa deposits in the enclosed basins; and near the coast, oolitic sediments, beach sands and sabkha deposits. The surface and near-surface deposits of Kuwait contain important reserves of construction sand and gravel as well as the only naturally occurring freshwater reserves of the country. An understanding of the nature of these surface deposits is required for the management of environmental issues like sand encroachment, land-use planning, and soil and groundwater pollution.