Location and Geography
The Dead Sea is a hypersaline lake situated in the Jordan Rift Valley. It lies east of the West Bank and west of Jordan, with its northern basin nearly surrounded by these two landmasses. Its surface and shores are 430.5 meters (1,412 feet) below sea level, making it the lowest land elevation on Earth. The sea is fed mainly by the Jordan River and contains no outlet, so water leaves only by evaporation, leaving salts and minerals behind. This geography creates a dense, mineral-rich lake with a stark shoreline that marks a distinct boundary between Jordan and the Palestinian territories.
Exact Coordinates and Borders
Coordinates and Surface Elevation
The Dead Sea’s center sits approximately at 31°30′N 35°30′E. Its surface elevation sits consistently around 430 meters (1,410 feet) below sea level, a benchmark for the planet’s lowest dry land. The northern end lies closest to major regional cities, while the southern basin extends into more remote areas. The shoreline forms the border between Jordan to the east and Israel and the West Bank to the west, with the precise boundary shaped by historical agreements and the management of shared water resources.
| Attribute | Verified Detail | Source Type |
|---|---|---|
| Latitude/Longitude | Approximately 31°30′N, 35°30′E | Geographic reference |
| Surface Elevation | 430.5 meters (1,412 feet) below sea level | Survey and mapping |
| Bordering Territories | Jordan (east), Israel and West Bank (west) | Political geography |
| Primary Inflow | Jordan River | Hydrology |
| Natural Outflow | Evaporation (no river outflow) | Limnology |
Regional Context
Nearby Cities and Regions
On the western side, the Dead Sea is close to Jerusalem, Tel Aviv, and Bethlehem, with travel times of roughly one hour from Jerusalem to the most accessible beaches. Jericho lies to the north, one of the oldest continuously inhabited cities, and serves as a key gateway to the western shore. To the east, Jordanian towns such as Madaba and the industrial zone near the King Hussein Bridge are relatively close to the northern shore. The surrounding area is a mix of desert, agricultural terraces, and significant archaeological sites, reflecting millennia of human settlement in this rift valley landscape.
Climate and Setting
The Dead Sea region is arid, with hot, dry summers and mild winters. Annual rainfall is minimal, and intense sunshine drives high evaporation rates, concentrating salts and shaping the unique environment. The depression in which the sea sits creates its own microclimate, often hotter in summer and more moderate in winter than nearby highland areas. Sparse vegetation, salt flats, and dramatic cliffs frame the water, producing a landscape that is both extreme and serene. These conditions draw visitors for therapeutic bathing and wellness while also supporting specialized microbial and mineral research.
Geological Formation
The Dead Sea lies within the Jordan Rift Valley, part of the larger Great Rift Valley system that runs through eastern Africa and the Middle East. This tectonic setting results from the African and Arabian plates moving apart, dropping the land between them to form a deep graben. Over millions of years, the basin filled with water, then repeatedly evaporated as climate changed, leaving thick layers of salts and minerals. The ongoing subsidence and evaporation make the sea shrink and its salinity rise, a long-term geological process that shapes its current extreme character. Understanding this formation helps explain why the Dead Sea is so saline and why its shoreline continues to retreat.
Human and Environmental Significance
For centuries, the Dead Sea has been a site of therapeutic and commercial activity, prized for its high salinity and mineral-rich mud. Ancient texts describe bathing in the sea and collecting its salts, and modern wellness industries continue this tradition. The surrounding lands hold archaeological sites that illuminate ancient trade and settlement, connecting the region to broader historical networks. Environmentally, the sea’s unique chemistry supports few organisms, yet its mineral crusts and microbial communities are of scientific interest. Water diversion from the Jordan River has reduced inflow, causing the sea to shrink and prompting international discussions about sustainable management. This intersection of health, history, and ecology underscores why the Dead Sea’s location matters beyond simple geography.
Summary of Key Facts
The Dead Sea is a salt lake in the Jordan Rift Valley bordered by Jordan to the east and Israel and the West Bank to the west. Its surface lies about 430 meters below sea level, making it the lowest point on Earth. Coordinates place it near 31°30′N, 35°30′E, with the Jordan River as its main inflow and evaporation as its only natural outflow. The regional climate is arid, hot in summer, and mild in winter, shaping a stark landscape of salt flats and cliffs. The sea’s geology, location, and human uses combine to make it a place of scientific, historical, and therapeutic importance that continues to evolve with environmental and political dynamics.