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Qhafor Ameen Hamasur

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Chapter One<br />

Introduction<br />

different rock units (Formations) on the surface and the main geological<br />

structures in the area (folds, faults and attitudes of strata).<br />

(3)- Investigating the topography of the area by constructing topographic profile at<br />

various sites to find the optimum profile for dam site selection.<br />

(4)-Integrating all the various geotechnical, geological and topographic (slope)<br />

data and preparing rock mass – valley section models (for the first time) for<br />

different sites and comparing them to find the most suitable site for dam<br />

construction.<br />

1-5 Research methods<br />

1-5-1 Field work<br />

The field work started in Feb.-2007 and extended to March-2008 for the<br />

period of 160 days (104 days for general survey of the study area and detailed<br />

study at and near the proposed dam site, 54 days for drilling three boreholes in<br />

the left side of the proposed dam site).<br />

As there is no precise geological map about the area, a detailed geological<br />

survey of the area was conducted, using a topographic maps with a scale of<br />

1:20000 (Maps No. 71/670 and 71/680 after the directorate general of surveys,<br />

Baghdad – Iraq) as a base map for preparing a geological map of the area.<br />

The geological survey included a description of the existing formations,<br />

measuring the dip and strike of all contacts between formations at numerous<br />

locations in the area. The altitude, latitudes, longitudes of the mentioned locations<br />

and along the axes of anticlines and synclines were recorded using GPSMAP<br />

60CSx. Finally, the obtained data were projected on the topographic map to draw<br />

the geological map of the area.<br />

Detailed information at the proposed dam site was collected for rock mass<br />

evaluation. To achieve this task, three surface stratigraphic sections and three<br />

boreholes were selected, Fig (1-2).<br />

Each section or borehole was divided into a number of rock mass units<br />

depending on the lithological (change in rock type) and structural properties (such<br />

5

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