OPEN
Natural Atlantic–Mediterranean connection, with navigation organised through GIBREP.
View AIS radar → Strait of Gibraltar Observatory
Is the Strait of Gibraltar
closing?
A passage only ≈14 km wide links two seas, separates two continents and concentrates shipping, ports and critical infrastructure. Gibraltar Watch tracks its maritime activity, geology and growing strategic value.
ACTIVE
Africa–Eurasia convergence of approximately 4.5 ± 1 mm/yr across a complex deformation zone.
How the region moves →NOT EXPECTED
There is no scientific basis for saying the strait will close in decades or centuries.
Timescales →—
Loading earthquake catalogue data…
Open seismic monitor →WHY THIS OBSERVATORY EXISTS
A narrow passage with global consequences
Its importance does not depend on the channel physically closing. It comes from its existing narrowness, the concentration of Atlantic–Mediterranean routes and the port system formed by Algeciras, Tanger Med, Gibraltar and Ceuta.
Over the coming years, supply-chain resilience, port expansion, maritime security and fixed-link studies may draw even more attention to this corridor.
Explore its strategic importance
STRATEGIC IMPORTANCE
VERY
HIGH
HIGH
≈14 km at the narrowest point
2 seas linked by one corridor
4 nodes in the immediate port cluster
24/7 traffic monitoring and organisation
THE MISUNDERSTOOD NUMBER
4.5 mm/yr does not mean the channel loses 4.5 mm of width each year
The rate describes regional plate convergence. The boundary is not a single hinge beneath the middle of the strait: it is a distributed system spanning the Gibraltar Arc, Gulf of Cádiz, Betics and Rif.
≈14 kmcurrent minimum width
4,5 ± 1mm/yr regional convergence
no rateof measured direct closure
EUROPE
ATLÁNTICOMEDITERRÁNEO
AFRICA
↓
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Conceptual diagram · not to scaleLIVE
Live AIS maritime traffic
Watch cargo ships, tankers, ferries and other vessels around Tarifa, Algeciras, Ceuta, Gibraltar and Tanger Med.
Open maritime radar
AUTOMATIC UPDATE
Recent earthquakes
The dashboard queries the USGS catalogue for the Gibraltar–Alboran–Gulf of Cádiz region and keeps a daily history.
24 h—
7 days—
Max 30 d—
TWO FLOWS, ONE GATEWAY
The strait breathes in two directions
Relatively fresher Atlantic water enters at the surface; denser Mediterranean water exits toward the Atlantic at depth.
ATLÁNTICO
MEDITERRÁNEO
surface inflow
deep outflow
Camarinal Sill
5.96 MILLION YEARS IN 4 MOMENTS
A gateway that already changed Mediterranean history
Atlantic restriction
The Messinian Salinity Crisis begins.
Extreme change
Large evaporite deposits and Mediterranean level falls.
Reconnection
The Atlantic fully reconnects with the Mediterranean.
Active exchange
The strait remains open and tectonically complex.
KEY QUESTIONS
Without misleading headlines
Is Africa moving toward Europe?
Yes, there is regional convergence. But deformation is diffuse and cannot be directly converted into an annual decrease in strait width.
Could it close one day?
Large reorganisations can occur on geological timescales, but there is no reliable closure forecast or estimated year.
Do earthquakes mean it is closing?
No. Seismicity shows the region is active; a single earthquake cannot establish a closing trend.
Would an empty AIS map prove closure?
No. Coverage, filters, latency and transponders can affect the display. The radar is complementary visual evidence.