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The Mesopotamian Geomorphology researches..
Sedimentological and Geomorphological Study of Sand
Dunes
in Najaf, Samawa, And Nasiriya Area
Ra'ad Abdul-Albaqi
Al-Ani
Abstract
There are many sand dunes belts distributed in south
and southwestern parts of the Western Desert ; Najaf,
Samawa, and Nasiriya fields. One hundred samples were
collected from the three field, 40 from Najaf, and 60
samples from Samawa and from Nasiryia.
Geomorphological study shows there are two types of
dunes; the barchan dune in Nasiriya area from by the
action of uni-directional wind and fixed dune in Samawa
area, that contains the domed- shape and elongated type
of dunes that form due to variation in the prevailing
wind direction.
Mechanical analysis showed that sand grains in Najaf
field to be well-moderately sorted ( 0.38-1.2), strongly
coarse to strongly fine skewed (- 0.81- to 0.39) and
very –laty to leptokurtic ( 0.1-1.3). Samawa dunes are
well to poorly sorted (0.04 – 1.44 ), strongly coarse to
strongly fine slewed (- 0.48 to 1.120, very platy to
very leptokurtic (0.49 – 1.69). In Najaf dune sands are
very well sorted near symmetrical to stongly fine skewed
(-0.1 to 0.5), and meso to very leptokurtic (0.9-2.3),
the distribution of these sediments is unimodal in Najaf
and Nasiriya and bimodal in Samawa area.
The identification of heavy and light minerals, clay
minerals analysis, and the morphology test by SEM
suggest that the sediments under study were transported
from geological formations and alluvial deposits of
Euphrates River.
The average value of roundness are 0.49 and
sphericity 0.85 that include, the texture of the dune
sand are immaturity and transported few distance.
Generally, the topography, geology, wind direction
and the vegetation cover affected the shape and
arrangement of dunes and their extention in a NW-SE
orientation in the three studied dune fields.
MSc.
Thesis submitted by Ra'ad Abdul-Albaqi Al-Ani, Dept.
Geology. College of Science, Baghdad University, 1979.
Supervisedby; Dr. Ali Jawad Ali
Dr. Mudafer Ahmed Mahmmod
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