Abstract
The geography, geomorphology, tectonics, stratigraphy and economic
potentials of areas alongside the Tigris River and its tributaries are given
with emphasis on Iraqi parts. The river runs mainly in the Mesopotamian Plain,
whereas its tributaries run in different tectonic zones with different
characters. Accordingly, the Quaternary sediments being dominated by alluvial
plain sediments cover large parts of the river course, whereas the tributaries
run through areas covered mainly by different rocks types of Neogene age. The
main economic potential is the existing oil fields, sulphur and limestone
deposits for cement industry.
Keywords: Tigris River, Quaternary sediments, Mesopotamian Plain,
Economic potential.