Sedimentological evidence and archaeological data show that huge tsunami hit the coast of today’s Sultanate of Oman around 1000 CE; the tsunami was almost 50 feet (15 m) tall and was caused by a strong earthquake in the Makran subduction zone, a giant fault that slants beneath the Arabian Sea coast of Pakistan and Iran. Overview of the study sites along the coastline of northern Oman: (a) Makran subduction zone (MSZ) and the Owen fracture zone (OFZ)....
