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This study analyzes the tectonic activity of the Wadi Araba Basin in the Gulf of Suez, Egypt, using geospatial analytics to assess landscape features such as mountain front sinuosity and stream gradients. The findings indicate varying levels of tectonic activity across different fault segments, with eastern segments showing higher seismic signals. The research emphasizes the need for further studies to evaluate seismic hazards in the region due to significant construction and population growth.

Author

Heinmin

Language

EN