The **Gulf of Aqaba** (Arabic: خليج العقبة, *Khalij al-'Aqabah*) is the **northeastern arm of the Red Sea**, separating Egypt's **Sinai Peninsula** from the **Arabian Peninsula** (Saudi Arabia, Jordan, Israel). It is a geologically young, tectonically active, and strategically vital waterway.
The gulf is the **northern terminus of the Dead Sea Transform (DST) fault system**—a left-lateral strike-slip boundary between the African Plate (Sinai) and Arabian Plate. It's an **active pull-apart basin** forming the southern end of the Jordan Rift Valley. Seafloor spreading is incipient; hydrothermal vents exist at depth.
| Country | Coastline | Major Port/City |
|---|---|---|
| Egypt | Western shore (Sinai) | Taba, Nuweiba, Dahab, Sharm El Sheikh (near Strait of Tiran) |
| Jordan | Northern tip (27 km) | Aqaba — Jordan's only seaport |
| Israel | Northern tip (10 km) | Eilat — Israel's Red Sea port |
| Saudi Arabia | Eastern shore | Haql, NEOM project (future megacity) |
**Fringing coral reefs** line most shores—northernmost tropical reefs globally. High salinity (40–41 PSU), clear water (30+ m visibility), 21–28°C. 500+ fish species, 200+ coral species. Threats: coastal development, diving pressure, warming, pollution.
The Gulf of Aqaba is a rare convergence of **tectonic drama, ecological richness, and geopolitical intensity**—a narrow blue corridor where continents, cultures, and economies meet.