Roughly 90% of the world's earthquakes occur along this 40,000-kilometre horseshoe
Including every recorded magnitude-9 event: Chile 1960, Alaska 1964, Sumatra 2004, Tohoku 2011
Geography · Physical geography
The Pacific Ocean rim — from New Zealand through Asia and the Americas to Chile
A horseshoe of subduction zones, volcanic arcs and deep trenches some 40,000 kilometres long around the rim of the Pacific. About three-quarters of the world's active and dormant volcanoes lie along it and roughly 90% of the world's earthquakes happen there, including every recorded magnitude-9 quake. It is a horseshoe rather than a ring: it is broken at the Drake Passage and around the Antarctic.
Roughly 90% of the world's earthquakes occur along this 40,000-kilometre horseshoe
Including every recorded magnitude-9 event: Chile 1960, Alaska 1964, Sumatra 2004, Tohoku 2011
About three-quarters of the world's active and dormant volcanoes stand on it
Fuji, Krakatoa, Pinatubo, St Helens, Popocatépetl and Rainier among them
It exists because oceanic plates are being forced under continental ones all round one ocean
Subduction melts the descending slab's overlying mantle, feeding the volcanic arcs above
The inclined plane of earthquakes that traces each descending slab bears a 20th-century seismologist's name
The Wadati–Benioff zone, after Kiyoo Wadati and Hugo Benioff
The largest earthquake ever instrumentally recorded, magnitude 9.5 in 1960, struck on it (1960)
The Valdivia earthquake in Chile, which sent a tsunami across the Pacific to Japan
The world's deepest ocean trenches lie along its western side
The Mariana, Tonga, Kuril–Kamchatka and Philippine trenches
Despite the name it is not closed — a gap in the south breaks the circuit
The Drake Passage and the Scotia Sea interrupt it between South America and Antarctica