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A detailed gamma ray spectrometry survey was carried out to make an action in environmental impact assessment of urbanization and industrialization on Port Said city, Egypt. The concentrations of the measured radioelements U-238, Th-232 in ppm, and K-40 %, in addition to the total counts of three selected randomly dumping sites (A, B, and C) were mapped. The concentration maps represent a base line for the radioactivity in the study area in order to detect any future radioactive contamination. These concentrations are ranging between 0.2 and 21 ppm for U-238 and 0.01 to 13.4 ppm for Th-232 as well as 0.15 to 3.8 % for K-40, whereas the total count values range from 8.7 to 123.6 uR. Moreover, the dose rate was mapped using the same spectrometer and survey parameters in order to assess the radiological effect of these radioelements. The dose rate values range from 0.12 to 1.61 mSv/year. Eighteen soil samples were collected from the sites with high radioelement concentrations and dose rates to determine the activity concentrations of Ra-226, Th-232, and K-40 using HPGe spectrometer. The activity concentrations of Ra-226, Th-232, and K-40 in the measured samples range from 18.03 to 398.66 Bq kg(-1), 5.28 to 75.7 Bq kg(-1), and 3,237.88 to 583.12 Bq kg(-1), respectively. In addition to analyze heavy metal for two high reading samples (a 1 and a 10) which give concentrations of Cd and Zn elements (a 1 40 ppm and a 10 42 ppm) and (a 1 0.90 ppm and a 10 0.97 ppm), respectively, that are in the range of phosphate fertilizer products that suggested a dumped man-made waste in site A. All indicate that the measured values for the soil samples in the two sites of three falls within the world ranges of soil in areas with normal levels of radioactivity, while site A shows a potential radiological risk for human beings, and it is important to carry out dose assessment program with a specifically detailed monitoring program periodically.

The current survey aimed to relocate the so-called granitic 'stela' inscribed for King Pepi I. The monument was originally discovered in 1897-98 by British Egyptologists excavating on an ancient mound located in the floodplain at the archaeological site of Hierakonpolis (modern Kom el-Ahmar), in the Aswan Governorate of Egypt. The original excavators were unable to remove it owing to its great weight and the monument was therefore left at the site. It remained partly exposed until 1989, when it was reburied in order to provide some protection from seasonal fluctuations in the water table. The exact location of the 'stela' was then lost, as the site is situated in the center of the modern village of Kom el-Gemuwia and is covered with halfa grass and other debris. As part of a new project to conserve and record this historic monument and other stone relics on this waterlogged site by the Hierakonpolis Expedition of the Ashmolean Museum, University of Oxford, UK, a geophysical approach was used to establish their current locations. A detailed Gamma Ray Spectrometry survey was conducted across the area suggested by the archeologists. The measurements were analyzed and plotted in the form of maps, which were helpful in selecting certain locations for examination. The results of limited field excavations confirmed that the localized high Thorium concentration anomalies were mainly related to the presence of the buried granite block. These results suggest that this method could be useful in for the detection of granitic monuments at similar sites.