“…Fault mapping within the gulf has revealed en‐echelon fault patterns with overlapping faults and pull‐apart basins that are far from a single straight fault strand in the middle of the gulf. In the northern gulf, for example, the Eilat and Haql faults bound the Eilat basin on the western and eastern side, respectively, with each fault near the opposing gulf coastlines (Ribot et al., 2020). The BOI results show more interseismic deformation on the western coast (Figure 4), indicating the deformation is rather focused on the Eilat fault than the Haql fault.…”