02 — WATER AND TIME
A horizon
in motion
The geological separation of South America and Antarctica gradually opened a marine corridor. The Drake Passage belongs to that deep history: tectonic shifts and ocean circulation changed the connection between continents and helped reshape the climate of the far south.
Today, the Antarctic Circumpolar Current flows through the passage, connecting the major ocean basins around Antarctica. Its strength reflects the winds and a complex interplay of water density, seabed topography and pressure differences.
At the surface, the cape faces swells and weather systems that travel across vast stretches of sea. Limited shelter, powerful gusts and rapidly changing conditions help explain its reputation among sailors.
Imagining a visible line dividing two oceans here makes a continuous system look deceptively simple. Pacific and Atlantic waters communicate through currents, water masses and eddies. Their names organise the map; the sea keeps moving.
Deep time: British Antarctic Survey · Ocean circulation: Marshall and colleagues, 2015.

