Tectonic Features of World with Subduction Zones Highlighted. (modified from This Dynamic Planet)
What is the "Ring of Fire"?
Most earthquakes and volcanic eruptions do not strike randomly but occur in specific areas, such as along plate boundaries. One such area is the circum-Pacific Ring of Fire, where the Pacific Plate meets many surrounding tectonic plates. The Ring of Fire is the most seismically and volcanically active zone in the world.
Learn more: USGS Volcano Hazards Program
Related
Can an eruption at one volcano trigger an eruption at another volcano?
How many active volcanoes are there on Earth?
How much of the Earth is volcanic?
Where does the United States rank in the number of volcanoes?
Which volcanoes in the contiguous United States have erupted since the Nation was founded?
What was the largest volcanic eruption in the 20th century?
Which volcanic eruptions were the deadliest?

Tectonic Features of World with Subduction Zones Highlighted. (modified from This Dynamic Planet)

Redoubt Volcano viewed from the northwest following the April 4, 2009 eruption (Event 19). Steam rises from the summit crater, pyroclastic flow and surge deposits drape the flanks, and lahar deposits cover the Drift River Valley.
Redoubt Volcano viewed from the northwest following the April 4, 2009 eruption (Event 19). Steam rises from the summit crater, pyroclastic flow and surge deposits drape the flanks, and lahar deposits cover the Drift River Valley.
Listen to hear the answer.

A gas plume arising from Augustine Volcano during it's eruptive phase 2005-06. This photo was taken during a FLIR/maintenance flight on January 24, 2006.
A gas plume arising from Augustine Volcano during it's eruptive phase 2005-06. This photo was taken during a FLIR/maintenance flight on January 24, 2006.

Oceanic crust forms by eruptions along the Juan de Fuca ridge. As the Juan de Fuca plate drifts eastward, it cools, becomes more dense, and eventually dives under the less dense continental plate at the Cascadia trench.
Oceanic crust forms by eruptions along the Juan de Fuca ridge. As the Juan de Fuca plate drifts eastward, it cools, becomes more dense, and eventually dives under the less dense continental plate at the Cascadia trench.
Volcanoes of American Samoa
It begins with curiosity—How do scientists learn from volcanoes?
Reducing risk where tectonic plates collide
This dynamic earth: the story of plate tectonics
Related
Can an eruption at one volcano trigger an eruption at another volcano?
How many active volcanoes are there on Earth?
How much of the Earth is volcanic?
Where does the United States rank in the number of volcanoes?
Which volcanoes in the contiguous United States have erupted since the Nation was founded?
What was the largest volcanic eruption in the 20th century?
Which volcanic eruptions were the deadliest?

Tectonic Features of World with Subduction Zones Highlighted. (modified from This Dynamic Planet)
Tectonic Features of World with Subduction Zones Highlighted. (modified from This Dynamic Planet)

Redoubt Volcano viewed from the northwest following the April 4, 2009 eruption (Event 19). Steam rises from the summit crater, pyroclastic flow and surge deposits drape the flanks, and lahar deposits cover the Drift River Valley.
Redoubt Volcano viewed from the northwest following the April 4, 2009 eruption (Event 19). Steam rises from the summit crater, pyroclastic flow and surge deposits drape the flanks, and lahar deposits cover the Drift River Valley.
Listen to hear the answer.

A gas plume arising from Augustine Volcano during it's eruptive phase 2005-06. This photo was taken during a FLIR/maintenance flight on January 24, 2006.
A gas plume arising from Augustine Volcano during it's eruptive phase 2005-06. This photo was taken during a FLIR/maintenance flight on January 24, 2006.

Oceanic crust forms by eruptions along the Juan de Fuca ridge. As the Juan de Fuca plate drifts eastward, it cools, becomes more dense, and eventually dives under the less dense continental plate at the Cascadia trench.
Oceanic crust forms by eruptions along the Juan de Fuca ridge. As the Juan de Fuca plate drifts eastward, it cools, becomes more dense, and eventually dives under the less dense continental plate at the Cascadia trench.