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The Western Desert of Egypt is an area of the Sahara which lies west of the River Nile, up to the Libyan border, and south from the Mediterranean Sea to the border with Sudan. It is mostly rocky desert; the desert covers 2/3 of the land of Egypt. Its highest elevation is 1000 m in the Gilf Kebir plateau to the far south‒west of Egypt, on the borders of Egypt, Sudan and Libya. We used to collect available data of the earthquakes, which occurred in or near the western part of Egypt during the period from 1900 to 2018, to investigate the seismic activity and its relationship to the geology and tectonics of Egypt. The frequency statistical analysis is used to calculate the frequency-magnitude relation for the data in this period. The results indicate that about 28 earthquakes are equal or exceed Richter magnitude M ≥ 4 every 100 years. The whole Western Desert is characterized by low to moderate levels of seismic activity. The southern part of Western Desert is considered to be seismically active. The source mechanism for some earthquakes was estimated using the waveform data recorded from the records of the Egyptian national seismograph stations and our results show the normal faulting mechanism with minor strike-slip component. The NNW trend has been chosen as a preferred rupture plane in consistence with surface and subsurface faults and microearthquake seismicity in the epicentral area as well. [ABSTRACT FROM AUTHOR]

The Gulf of Aqaba is situated along the southern part of the Dead Sea Rift Area transform (DST), 1000 km (620 miles), the boundary between the African plate and the Arabian plate. It is situated toward the east of the Sinai landmass and west of Saudi Arabia. It is one of the joints interfacing the Asian and African landmasses. The Gulf expands 180 km from Eilat and Aqaba and joins the Red Sea in the Strait of Tiran, with the most extensive purpose of 28 km. On November 22, 1995, the biggest seismic tremor estimating 7.0 degrees happened along parts of the dead left line in the Gulf of Aqaba close to the port of Nuweiba in Egypt. This tremor made extraordinary harm Egypt and neighboring nations. Consequently, a few point by point investigations of seismology and geophysics have been led in the Gulf of Aqaba. In the territory researched, the vast majority of the ongoing seismic action revolved around the Gulf of Aqaba is portrayed by the contribution of moderate central quakes, an immediate aftereffect of the relative development between the plates of Africa, Sinai and the Arabian Peninsula. Seismic Energy along the Gulf of Aqaba locale is assessed utilizing a brief period (50 tests for every second) executed by the Egyptian National Seismic Network amid the period 1998‒2017. The connection between the dispatch and greatness of quakes in the Gulf of Aqaba demonstrated that the vast majority of the seismic Energy discharge originates from the biggest occasions and is packed in the inside, while it is moderately low in the southern and northern parts of the Gulf. [ABSTRACT FROM AUTHOR]

Lake Nasser is situated in an area with a very non-recurring earthquake, and revealed the history of Egypt registered 5000 years ago. After seventeen years of filling the Aswan High Dam reservoir began a long series of earthquakes caused. The main shock, Ms. = 5.6, occurred on November 14, 1981, preceded by several factions, followed by a large number of aftershocks. Thirty-three years later, seismic activity remains, but is much lower in frequency and volume. The aim of this paper is to study the effect of the reservoir on the induced seismic and determine the coordination mechanism of some earthquakes that occurred in the northwestern part of High Dam reservoir. These investigations indicate that seismic activity occurred mainly along the Kalabsha fault and small parallel sectors, and there is a range of activities in the Khor al-Ramla area, about 40 km southwest of the High Dam. From 1982 to the end of 2017, seventy-five earthquakes with a magnitude of 3.5 ≤ M < 4.0 and 13 earthquakes of magnitude greater than or equal to 4.0 have occurred. It also shows that these earthquakes occurred during loading and unloading periods. This shows that the effect of the reservoir itself does not produce earthquakes, and there is no direct relationship between changing the daily rate and the magnitude of earthquakes. So it can't be used as a predictor in the case of the Aswan reservoir, which is a unique reservoir in its behavior. The focused coordination mechanism of four different seismic zones in the west of Lake Nasser shows errors in striking the strike with a simple natural element. The P (pressure) and T (tension) stress axes are trending ESE–WNW and NNE–SSW, respectively. [ABSTRACT FROM AUTHOR]