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In a press release Saturday, Aba Al-Khail said that SGS’s Geologic Hazards Center continuously follows — around the clock — the seismic activity in the central Red Sea region along the groove rift, and that the seismic magnitude is from weak to medium, where there is a region of tectonic tension due to the divergence of the African tectonic plate from the Arabian tectonic plate, which is characterized by mostly weak to moderate seismic activity.