Qhafor Ameen Hamasur
Qhafor Ameen Hamasur
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 />
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