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A broad, horseshoe-shaped seismically active band of earthquake epicenters, volcanoes, and tectonic plate boundaries that surrounds the Pacific basin is known as the Ring of Fire, sometimes known as the Circum-Pacific Belt or the Pacific Ring of Fire. The belt follows chains of island arcs like Tonga and New Hebrides, the Indonesian archipelago, the Philippines, Japan, the Kuril Islands, and the Aleutians for the majority of its 40,000 km (24,900 miles) length, as well as other arc-shaped geomorphic features like the western coast of North America and the Andes Mountains.
The belt's whole length is marked by volcanoes, which is why it is known as the "Ring of Fire." The belt is framed by a number of deep ocean troughs on the oceanic side, with continental landmasses behind. The vast majority of earthquakes, most of the greatest earthquakes, and over 75% of the world's volcanoes all take place inside the Ring of Fire.
- The Circum-Pacific Belt, often known as the Ring of Fire, is a region in the Pacific Ocean marked by active volcanoes and frequent earthquakes. The Ring of Fire is where most of Earth's earthquakes and volcanoes occur.
- More than 450 volcanoes, or 75% of all volcanoes on Earth, are found around the Ring of Fire. The majority of the planet's earthquakes, including the most severe and dramatic seismic occurrences, happen along its course.
- The Circum-Pacific Belt, often known as the Ring of Fire, is a region in the Pacific Ocean marked by active volcanoes and frequent earthquakes. It is around 40,000 kilometers long (24,900 miles). The Pacific, Juan de Fuca, Cocos, Indian-Australian, Nazca, North American, and Philippine Plates are among the tectonic plates whose borders it tracks.
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