Тынық мұхитының айналасындағы өрт шеңбері

Region around the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur

The Ring of Fire (also known as the Pacific Ring of Fire, the Rim of Fire, the Girdle of Fire or the Circum Pacific belt) is a tectonic belt of volcanoes and earthquakes. It is about long and up to about wide, and surrounds most of the Pacific Ocean. The Ring of Fire contains between 750 and 915 active or dormant volcanoes, around two thirds of the world total. The exact number of volcanoes within the Ring of Fire depends on which regions are included. About 90% of the world's earthquakes, including most of its largest, occur within the belt. The Ring of Fire is not a single geological structure. It was created by the subduction of different tectonic plates at convergent boundaries around the Pacific Ocean. These include: the Antarctic, Nazca and Cocos plates subducting beneath the South American Plate; the Pacific and Juan de Fuca plates beneath the North American Plate; the Philippine plate beneath the Eurasian plate; and a complex boundary between the Pacific and Australian Plate. The interactions at these plate boundaries have formed oceanic trenches, volcanic arcs, back arc basins and volcanic belts. The inclusion of some areas in the Ring of Fire, such as the Antarctic Peninsula and western Indonesia, is disputed. The Ring of Fire has existed for more than 35 million years but subduction has existed for much longer in some parts of the Ring; many older extinct volcanoes are located within the Ring. while the four largest volcanic eruptions on Earth in the Holocene epoch all occurred at volcanoes in the Ring of Fire. Most of Earth's active volcanoes with summits above sea level are located in the Ring of Fire. Many of these subaerial volcanoes are stratovolcanoes (e. g. Mount St Helens), formed by explosive eruptions of tephra alternating with effusive eruptions of lava flows. Lavas at the Ring of Fire's stratovolcanoes are mainly andesite and basaltic andesite but dacite, rhyolite, basalt and some other rarer types also occur. This historical link between volcanoes and fire is preserved in the name of the Ring of Fire, despite the fact that volcanoes do not burn the Earth with fire. The existence of a belt of volcanic activity around the Pacific Ocean was known in the early 19th century; for example, in 1825 the pioneering volcanologist G. P. Scrope described the chains of volcanoes around the Pacific Ocean's rim in his book "Considerations on Volcanos". Three decades later, a book about the Perry Expedition to Japan commented on the Ring of Fire volcanoes as follows: "They [the Japanese Islands] are in the line of that immense circle of volcanic development which surrounds the shores of the Pacific from Tierra del Fuego around to the Moluccas." (Narrative of the Expedition of an American Squadron to the China Seas and Japan, 1852–54). An article appeared in Scientific American in 1878 with the title "The Ring of Fire, and the Volcanic Peaks of the West Coast of the United States", which outlined the phenomenon of volcanic activity around the boundaries of the Pacific. Early explicit references to volcanoes forming a "ring of fire" around the Pacific Ocean also include Alexander P. Livingstone's book "Complete Story of San Francisco's Terrible Calamity of Earthquake and Fire", published in 1906, in which he describes " the great ring of fire which circles round the whole surface of the Pacific Ocean.". In 1912, geologist Patrick Marshall introduced the term "Andesite Line" to mark a boundary between islands in the southwest Pacific, which differ in volcano structure and lava types. The concept was later extended to other parts of the Pacific Ocean. The Andesite Line and the Ring of Fire closely match in terms of location. The development of the theory of plate tectonics since the early 1960s has provided the current understanding and explanation of the global distribution of volcanoes and earthquakes, including those in the Ring of Fire.

There is consensus among geologists about most of the regions which are included in the Ring of Fire. There are, however, a few regions on which there is no universal agreement. (See: ). Indonesia lies at the intersection of the Ring of Fire and the Alpide belt (which is the Earth's other very long subduction related volcanic and earthquake zone, also known as the Mediterranean–Indonesian volcanic belt, running east–west through southern Asia and southern Europe). Some geologists include all of Indonesia in the Ring of Fire; many geologists exclude Indonesia's western islands (which they include in the Alpide belt). Some geologists include the Antarctic Peninsula and the South Shetland Islands in the Ring of Fire, because the submarine plate boundaries in this part of the Pacific Ocean (the Pacific–Antarctic Ridge, the East Pacific Rise and the Chile Ridge) are divergent instead of convergent. Although some volcanism occurs in this region, it is not related to subduction. Some geologists include the Izu Islands, the Bonin Islands, and the Mariana Islands, other geologists exclude them. and they are not part of the Ring of Fire.

The Ring of Fire has existed for more than 35 million years. The current configuration of the Pacific Ring of Fire has been created by the development of the present day subduction zones, initially (by about 115 million years ago) in South America, North America and Asia. As plate configurations gradually changed, the current subduction zones of Indonesia and New Guinea were created (about 70 million years ago), followed finally by the New Zealand subduction zone (about 35 million years ago). The Pacific Plate came into existence in the Early Jurassic about 190 million years ago, far from the margins of the then Paleo Pacific Ocean. Until the Pacific Plate grew large enough to reach the margins of the ocean basin, other older plates were subducted ahead of it at the ocean basin margins. For example, subduction has been occurring at the coast of South America since the Jurassic Period more than 145 million years ago, and remnants of Jurassic and Cretaceous volcanic arcs are preserved there. At about 120 to 115 million years ago, the Farallon Plate was subducting under South America, North America and north east Asia while the Izanagi Plate was subducting under east Asia. By 85 to 70 million years ago, the Izanagi Plate had moved north eastwards and was subducting under east Asia and North America, while the Farallon Plate was subducting under South America and the Pacific Plate was subducting under east Asia. About 70 to 65 million years ago, the Farallon plate was subducting under South America, the Kula Plate was subducting under North America and north east Asia, and the Pacific Plate was subducting under east Asia and Papua New Guinea. About 35 million years ago, the Kula and Farallon plates had been subducted and the Pacific Plate was subducting around its rim in a configuration closely resembling the outline of the present day Ring of Fire.

The eastern parts of the Ring of Fire result from the collision of a few relatively large plates. The western parts of the Ring are more complex, with a number of large and small tectonic plates in collision. In South America, the Ring of Fire is the result of the Antarctic Plate, the Nazca Plate and the Cocos Plate being subducted beneath the South American Plate. In Central America, the Cocos Plate is being subducted beneath the Caribbean Plate. A portion of the Pacific Plate and the small Juan de Fuca Plate are being subducted beneath the North American Plate. Along the northern portion, the northwestward moving Pacific Plate is being subducted beneath the Aleutian Islands arc. Farther west, the Pacific Plate is being subducted at the Kamchatka Peninsula and Kuril arcs. Farther south, at Japan, Taiwan and the Philippines, the Philippine Plate is being subducted beneath the Eurasian Plate. The southwest section of the Ring of Fire is more complex, with a number of smaller tectonic plates in collision with the Pacific Plate at the Mariana Islands, the Philippines, eastern Indonesia, Papua New Guinea, Tonga, and New Zealand; this part of the Ring excludes Australia, because that landmass lies in the center of its tectonic plate far from subduction zones. In North America, there is a gap in subduction related volcanic activity in northern Mexico and southern California, due partly to a divergent boundary in the Gulf of California and due partly to the San Andreas Fault (a non volcanic transform boundary). Another North American gap in subduction related volcanic activity occurs in northern British Columbia, Yukon and south east Alaska, where volcanism is caused by intraplate continental rifting.

+Distribution of Ring of Fire volcanoes active in the Holocene Epoch (last 11,700 years)ContinentCountryRegionVolcanoes (subduction zone)Volcanoes (other)CommentsConsensus for inclusionAntarcticaAntarctic Peninsula (Graham Land)03 intraplate NoAntarcticaSouth Shetland Islands04 intraplateintraplate rift volcanoes associated with back arc rifting linked to subductionNoSouth AmericaChile710excluding Easter Island (oceanic rift)YesSouth AmericaChile Argentina180border shared by two countriesYesSouth AmericaArgentina154 intraplateno coast on the Pacific OceanNoSouth AmericaChile Bolivia60border shared by two countriesYesSouth AmericaBolivia50no coast on the Pacific OceanNoSouth AmericaChile Peru10border shared by two countriesYesSouth AmericaPeru160YesSouth AmericaEcuador210excluding the Galápagos Islands (hotspot)YesSouth AmericaEcuador Colombia10border shared by two countriesYesSouth AmericaColombia130YesNorth AmericaPanama20YesNorth AmericaCosta Rica100YesNorth AmericaNicaragua170YesNorth AmericaHonduras40YesNorth AmericaEl Salvador180YesNorth AmericaEl Salvador Guatemala20border shared by two countriesYesNorth AmericaGuatemala210YesNorth AmericaGuatemala Mexico10border shared by two countriesYesNorth AmericaMexico268 riftexcluding 3 oceanic rift volcanoes; 8 continental rift volcanoes in Baja CaliforniaYesNorth AmericaUnited StatesCalifornia, Oregon, Washington229 rift9 continental rift volcanoes (6 in southern California and 3 in Oregon)YesNorth AmericaCanada616 intraplateexcluding 2 oceanic rift volcanoesYesNorth AmericaUnited StatesAlaska804 intraplate in southeast Alaskaincluding 39 volcanoes in the Aleutian Islands; excluding 4 intraplate volcanoes in western Alaska far from subduction zoneYesAsiaRussiaKamchatka670including 1 submarine volcano (Piip) in the Aleutian arcYesAsiaRussiaKuril Islands440including 3 submarine volcanoes; 15 volcanoes claimed by JapanYesAsiaJapan810excluding the Izu Islands and the Bonin IslandsYesAsiaTaiwan40including 2 submarine volcanoesYesJapanIzu Islands and Bonin Islands260including 13 submarine volcanoesNoUnited StatesNorthern Mariana Islands and Guam250including 16 submarine volcanoesNoAsiaPhilippines410including 1 submarine volcanoYesAsiaIndonesiawestern islands70Sumatra (27 volcanoes), Krakatoa, Java (36 volcanoes), Bali (3 volcanoes), Lombok, Sumbawa and Sangeang (i. e. the Sunda Arc, north of the Sunda subduction zone between the Australian Plate and the Sunda Plate)NoAsiaIndonesiaeastern islands54Sulawesi, Lesser Sunda Islands (excluding Bali, Lombok, Sumbawa and Sangeang), Halmahera, Banda Islands, Sangihe IslandsYesPapua New Guinea471 riftincluding 2 submarine volcanoesYesSolomon Islands80including 4 submarine volcanoesYesVanuatu140Yesclaimed by Vanuatu and France (New Caledonia)21 riftHunter Island and Matthew Island; East Gemini Seamount is a seamount at an oceanic riftYesFiji30YesFranceWallis and Futuna10mantle plume and subductionNoSamoa20mantle plume and subduction including 1 submarine seamountNoTonga173 riftincluding 13 submarine volcanoes, 3 of which are subduction related back arc rift volcanoesYesbetween Tonga and Kermadec Islands10Monowai submarine seamount (between the exclusive economic zones of Tonga and New Zealand)YesNew ZealandKermadec Islands60including 4 submarine volcanoesYesNew Zealand200excluding the Kermadec Islands; including 8 submarine volcanoesYesTotal91359

The four largest volcanic eruptions on Earth in the Holocene Epoch (the last 11,700 years) occurred at volcanoes in the Ring of Fire. They are the eruptions at Fisher Caldera (Alaska, 8700 BC), Kuril Lake (Kamchatka, 6450 BC), Kikai Caldera (Japan, 5480 BC) and Mount Mazama (Oregon, 5677 BC). They are presumed to have been megathrust earthquakes at subduction zones, The Antarctic Peninsula (Graham Land) is also sometimes included in the Ring. Volcanoes south of the Antarctic Circle (e. g. the volcanoes of Victoria Land including Mount Erebus, and the volcanoes of Mary Byrd Land) are not related to subduction; therefore, they are not part of the Ring of Fire. therefore, they are not part of the Ring of Fire.

The world's highest active volcano is Ojos del Salado , which is in the Andes Mountains section of the Ring of Fire. It forms part of the border between Argentina and Chile and it last erupted in AD 750. Another Ring of Fire Andean volcano on the Argentina Chile border is Llullaillaco , which is the world's highest historically active volcano, last erupting in 1877.

Bolivia hosts active and extinct volcanoes across its territory. The active volcanoes are located in western Bolivia where they make up the Cordillera Occidental, the western limit of the Altiplano plateau. Some of the active volcanoes are international mountains shared with Chile. All Cenozoic volcanoes of Bolivia are part of the Central Volcanic Zone (CVZ) of the Andean Volcanic Belt that results due to processes involved in the subduction of the Nazca Plate under the South American Plate. The Central Volcanic Zone is a major late Cenozoic volcanic province.

Sabancaya is an active stratovolcano in the Andes of southern Peru, about northwest of Arequipa. It is the most active volcano in Peru, with an ongoing eruption that started in 2016. Ubinas is another active volcano of in southern Peru; its most recent eruption occurred in 2019. Volcanoes in Peru are monitored by the Peruvian Geophysical Institute.

Cotopaxi is a stratovolcano in the Andes, located about south of Quito, Ecuador, South America. It is the second highest summit in the country, reaching a height of Since 1738, Cotopaxi has erupted more than 50 times, resulting in the creation of numerous valleys formed by mudflows around the volcano. In October 1999, Pichincha Volcano erupted in Quito and covered the city with several inches of ash. Prior to that, the last major eruptions were in 1553 and in 1660, when about 30 cm of ash fell on the city. At , Sangay Volcano is an active stratovolcano in central Ecuador, one of the highest active volcanoes in the world and is one of Ecuador's most active volcanoes. It exhibits mostly strombolian activity; An eruption, which started in 1934, ended in 2011. More recent eruptions have occurred. Geologically, Sangay marks the southern bound of the Northern Volcanic Zone, and its position straddling two major pieces of crust accounts for its high level of activity. Sangay's roughly 500,000 year history is one of instability; two previous versions of the mountain were destroyed in massive flank collapses, evidence of which still litters its surroundings today. Sangay is one of two active volcanoes located within the namesake Sangay National Park, the other being Tungurahua to the north. As such, it has been listed as a UNESCO World Heritage Site since 1983. Reventador is an active stratovolcano that lies in the eastern Andes of Ecuador. Since 1541, it has erupted over 25 times, with its most recent eruption starting in 2008 and, as of 2020, still ongoing, but the largest historical eruption occurred in 2002. During that eruption, the plume from the volcano reached a height of , and pyroclastic flows reached from the cone. On March 30, 2007, the volcano erupted ash again, which reached a height of about 2 mile (3 km). In Ecuador, EPN monitors volcanic activity.

Poás Volcano is an active stratovolcano located in central Costa Rica; it has erupted 39 times since 1828. The Volcanological and Seismological Observatory of Costa Rica (OVSICORI, Observatorio Vulcanológico y Sismológico de Costa Rica) at the National University of Costa Rica has a dedicated team in charge of researching and monitoring the volcanoes, earthquakes, and other tectonic processes in the Central America Volcanic Arc.

In 1902, the Santa Maria Volcano erupted violently in Guatemala, with the largest explosions occurring over two days, ejecting an estimated of magma. The eruption was one of the largest of the 20th century, only slightly less in magnitude to that of Mount Pinatubo in 1991. The eruption had a volcanic explosivity index of 6. Today, Santiaguito is one of the world's most active volcanoes.

Volcanoes of Mexico related to subduction of the Cocos and Rivera plates occur in the Trans Mexican Volcanic Belt, which extends from west to east across central southern Mexico. Popocatépetl, lying in the eastern half of the Trans Mexican Volcanic Belt, is the second highest peak in Mexico after the Pico de Orizaba. It is one of the most active volcanoes in Mexico, having had more than 20 major eruptions since the arrival of the Spanish in 1519. The 1982 eruption of El Chichón, which killed about 2,000 people who lived near the volcano, created a 1 km wide caldera that filled with an acidic crater lake. Before 1982, this relatively unknown volcano was heavily forested and of no greater height than adjacent nonvolcanic peaks.

The Cascade Volcanic Arc lies in the western United States. This arc includes nearly 20 major volcanoes, among a total of over 4,000 separate volcanic vents including numerous stratovolcanoes, shield volcanoes, lava domes, and cinder cones, along with a few isolated examples of rarer volcanic forms such as tuyas. Volcanism in the arc began about 37 million years ago, but most of the present day Cascade volcanoes are less than 2 million years old, and the highest peaks are less than 100,000 years old. The arc is formed by the subduction of the Gorda and Juan de Fuca plates at the Cascadia subduction zone. This is a 680 mile (1094 km) fault, running 50 mile (80 km) off the coast of the Pacific Northwest from northern California to Vancouver Island, British Columbia. The plates move at a relative rate of over per year at an oblique angle to the subduction zone. Because of the very large fault area, the Cascadia subduction zone can produce very large earthquakes, magnitude 9.0 or greater, if rupture occurred over its whole area. When the "locked" zone stores energy for an earthquake, the "transition" zone, although somewhat plastic, can rupture. Thermal and deformation studies indicate that the locked zone is fully locked for down dip from the deformation front. Further down dip, a transition from fully locked to aseismic sliding occurs. Unlike most subduction zones worldwide, no oceanic trench is present along the continental margin in Cascadia. Instead, terranes and the accretionary wedge have been lifted up to form a series of coast ranges and exotic mountains. A high rate of sedimentation from the outflow of the three major rivers (Fraser River, Columbia River, and Klamath River) which cross the Cascade Range contributes to further obscuring the presence of a trench. However, in common with most other subduction zones, the outer margin is slowly being compressed, similar to a giant spring. When the stored energy is suddenly released by slippage across the fault at irregular intervals, the Cascadia subduction zone can create very large earthquakes such as the magnitude 9 Cascadia earthquake of 1700. Geological evidence indicates that great earthquakes may have occurred at least seven times in the last 3,500 years, suggesting a return time of 400 to 600 years. Also, evidence of accompanying tsunamis with every earthquake is seen, as the prime reason these earthquakes are known is through "scars" the tsunamis left on the coast, and through Japanese records (tsunami waves can travel across the Pacific). The 1980 eruption of Mount St. Helens was the most significant to occur in the contiguous 48 U. S. states in recorded history (VEI = 5, of material erupted), exceeding the destructive power and volume of material released by the 1915 eruption of California's Lassen Peak. The eruption was preceded by a two month series of earthquakes and steam venting episodes caused by an injection of magma at shallow depth below the mountain that created a huge bulge and a fracture system on Mount St. Helens' north slope. An earthquake at 8:32 am on May 18, 1980, caused the entire weakened north face to slide away, suddenly exposing the partly molten, gas rich rock in the volcano to lower pressure. The rock responded by exploding into a very hot mix of pulverized lava and older rock that sped toward Spirit Lake so fast that it quickly passed the avalanching north face. Alaska is known for its seismic and volcanic activity, holding the record for the second largest earthquake in the world, the Good Friday earthquake, and having more than 50 volcanoes which have erupted since about 1760. Volcanoes are found not only in the mainland, but also in the Aleutian Islands. The United States Geological Survey and the National Earthquake Information Center monitor volcanoes and earthquakes in the United States.

British Columbia and Yukon are home to a region of volcanoes and volcanic activity in the Pacific Ring of Fire. More than 20 volcanoes have erupted in the western Canada during the Holocene Epoch but only 6 are directly related to subduction: Bridge River Cones, Mount Cayley, Mount Garibaldi, Garibaldi Lake, Silverthrone Caldera, and Mount Meager massif. There are hot springs at some volcanoes. Since 1975, seismic activity appears to have been associated with some volcanoes in British Columbia including the six subduction related volcanoes as well as intraplate volcanoes such as Wells Gray Clearwater volcanic field. The Garibaldi Volcanic Belt in southwestern British Columbia is the northern extension of the Cascade Volcanic Arc in the United States (which includes Mount Baker and Mount St. Helens) and contains the most explosive young volcanoes in Canada. It formed as a result of subduction of the Juan de Fuca Plate (a remnant of the much larger Farallon Plate) under the North American Plate along the Cascadia subduction zone. The Chilcotin Group is a north–south range of volcanoes in southern British Columbia running parallel to the Garibaldi Volcanic Belt. The majority of the eruptions in this belt happened either 6–10 million years ago (Miocene) or 2–3 million years ago (Pliocene), although with some slightly more recent eruptions (in the Pleistocene). It is thought to have formed as a result of back arc extension behind the Cascadia subduction zone. The Public Safety Geo science Program at the Natural Resources Canada undertakes research to support risk reduction from the effects of space weather, earthquakes, tsunamis, volcanoes, and landslides.

The Kamchatka Peninsula in the Russian Far East is one of the most active volcanic areas in the world, with 20 historically active volcanoes. It lies between the Pacific Ocean to the east and the Okhotsk Sea to the west. Immediately offshore along the Pacific coast of the peninsula runs the Kuril–Kamchatka Trench, where subduction of the Pacific Plate fuels the volcanism. Several types of volcanic activity are present, including stratovolcanoes, shield volcanoes, Hawaiian style fissure eruptions and geysers. Active, dormant and extinct volcanoes of Kamchatka are in two major volcanic belts. The most recent activity takes place in the eastern belt, starting in the north at the Shiveluch volcanic complex, which lies at the junction of the Aleutian and Kamchatka volcanic arcs. Just to the south is the Klyuchi volcanic group, comprising the twin volcanic cones of Kliuchevskoi and Kamen, the volcanic complexes of Tolbachik and Ushkovsky, and a number of other large stratovolcanoes. Ichinsky, the only active volcano in the central belt, is located farther to the west. Farther south, the eastern belt of stratovolcanoes continues to the southern tip of Kamchatka, continuing onto the Kuril Islands, with their 32 historically active volcanoes.

About 10% of the world's active volcanoes are found in Japan, which lies in a zone of extreme crustal instability. They are formed by subduction of the Pacific Plate and the Philippine Sea Plate. As many as 1,500 earthquakes are recorded yearly, and magnitudes of 4 to 6 are not uncommon. Minor tremors occur almost daily in one part of the country or another, causing some slight shaking of buildings. Major earthquakes occur infrequently; the most famous in the 20th century were: the Great Kantō earthquake of 1923, in which 130,000 people died; and the Great Hanshin earthquake of January 17, 1995, in which 6,434 people died. On March 11, 2011 a magnitude 9.0 earthquake hit Japan, the country's biggest ever and the fifth largest on record, according to US Geological Survey data. Undersea earthquakes also expose the Japanese coastline to danger from tsunamis. Mount Bandai, one of Japan's most noted volcanoes, rises above the north shore of Lake Inawashiro. Mount Bandai is formed of several overlapping stratovolcanoes, the largest of which is O Bandai, constructed within a horseshoe shaped caldera that formed about 40,000 years ago when an earlier volcano collapsed, forming the Okinajima debris avalanche, which traveled to the southwest and was accompanied by a plinian eruption. Four major phreatic eruptions have occurred during the past 5,000 years, two of them in historical time, in 806 and 1888. Seen from the south, Bandai presents a conical profile, but much of the north side of the volcano is missing as a result of the collapse of Ko Bandai volcano during the 1888 eruption, in which a debris avalanche buried several villages and formed several large lakes. In July 1888, the north flank of Mount Bandai collapsed during an eruption quite similar to the May 18, 1980, eruption of Mount St. Helens. After a week of seismic activity, a large earthquake on July 15, 1888, was followed by a tremendous noise and a large explosion. Eyewitnesses heard about 15 to 20 additional explosions and observed that the last one was projected almost horizontally to the north. Mount Fuji is Japan's highest and most noted volcano, featuring heavily in Japanese culture and serving as one of the country's most popular landmarks. The modern postglacial stratovolcano is constructed above a group of overlapping volcanoes, remnants of which form irregularities on Fuji's profile. Growth of the younger Mount Fuji began with a period of voluminous lava flows from 11,000 to 8,000 years ago, accounting for four fifths of the volume of the younger Mount Fuji. Minor explosive eruptions dominated activity from 8,000 to 4,500 years ago, with another period of major lava flows occurring from 4,500 to 3,000 years ago. Subsequently, intermittent major explosive eruptions occurred, with subordinate lava flows and small pyroclastic flows. Summit eruptions dominated from 3,000 to 2,000 years ago, after which flank vents were active. The extensive basaltic lava flows from the summit and some of the more than 100 flank cones and vents blocked drainage against the Tertiary Misaka Mountains on the north side of the volcano, forming the Fuji Five Lakes. The last eruption of this dominantly basaltic volcano in 1707 ejected andesitic pumice and formed a large new crater on the east flank. Some minor volcanic activity may occur in the next few years.

The 1991 eruption of Mount Pinatubo is the world's second largest eruption of the 20th century. Successful predictions of the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but as the surrounding areas were severely damaged by pyroclastic flows, ash deposits, and later, lahars caused by rainwater remobilising earlier volcanic deposits, thousands of houses were destroyed. Mayon Volcano is the Philippines' most active volcano. It has steep upper slopes that average 35–40° and is capped by a small summit crater. The historical eruptions of this basaltic andesitic volcano date back to 1616 and range from Strombolian to basaltic Plinian eruptions. Eruptions occur predominately from the central conduit and have also produced lava flows that travel far down the flanks. Pyroclastic flows and mudflows have commonly swept down many of the roughly 40 ravines that radiate from the summit and have often devastated populated lowland areas. Taal Volcano has had 33 recorded eruptions since 1572. A devastating eruption occurred in 1911, which claimed more than a thousand lives. The deposits of that eruption consist of a yellowish, fairly decomposed (nonjuvenile) tephra with a high sulfur content. The most recent period of activity lasted from 1965 to 1977, and was characterized by the interaction of magma with the lake water, which produced violent phreatic and phreatomagmatic eruptions. The volcano was dormant from 1977 then showed signs of unrest since 1991 with strong seismic activity and ground fracturing events, as well as the formation of small mud geysers on parts of the island. An eruption occurred in January 2020. Kanlaon Volcano, the most active volcano in the central Philippines, has erupted 25 times since 1866. Eruptions are typically phreatic explosions of small to moderate size that produce minor ash falls near the volcano. On August 10, 1996, Kanlaon erupted without warning, killing 3 persons who were among 24 mountain climbers trapped near the summit.

Indonesia is located where the Ring of Fire around the Pacific Ocean meets the Alpide belt (which runs from Southeast Asia to Southwest Europe). The eastern islands of Indonesia (Sulawesi, the Lesser Sunda Islands (excluding Bali, Lombok, Sumbawa and Sangeang), Halmahera, the Banda Islands and the Sangihe Islands) are geologically associated with subduction of the Pacific Plate or its related minor plates and, therefore, the eastern islands are often regarded as part of the Ring of Fire. The western islands of Indonesia (the Sunda Arc of Sumatra, Krakatoa, Java, Bali, Lombok, Sumbawa and Sangeang) are located north of a subduction zone in the Indian Ocean. Although news media, popular science publications and some geologists include the western islands (and their notable volcanoes such as Krakatoa, Merapi, Tambora and Toba) in the Ring of Fire, geologists often exclude the western islands from the Ring; instead the western islands are often included in the Alpide belt.

New Zealand contains the world's strongest concentration of youthful rhyolitic volcanoes, and voluminous sheets of tuff blanket much of the North Island. The earliest historically dated eruption was at Whakaari/White Island in 1826, followed in 1886 by the country's largest historical eruption at Mount Tarawera. Much of the region north of New Zealand's North Island is made up of seamounts and small islands, including 16 submarine volcanoes. In the last 1.6 million years, most of New Zealand's volcanism is from the Taupō Volcanic Zone. Mount Ruapehu, at the southern end of the Taupō Volcanic Zone, is one of the most active volcanoes in New Zealand. It began erupting at least 250,000 years ago. In recorded history, major eruptions have been about 50 years apart, Between major eruptions, a warm acidic crater lake forms, fed by melting snow. Major eruptions may completely expel the lake water. Where a major eruption has deposited a tephra dam across the lake's outlet, the dam may collapse after the lake has refilled and risen above the level of its normal outlet, the outrush of water causing a large lahar. The most notable lahar caused the Tangiwai disaster on December 24, 1953, when 151 people aboard a Wellington to Auckland express train were killed after the lahar destroyed the Tangiwai rail bridge just moments before the train was due. In 2000, the ERLAWS system was installed on the mountain to detect such a collapse and alert the relevant authorities. The Auckland volcanic field on the North Island of New Zealand has produced a diverse array of explosive craters, scoria cones, and lava flows. Currently dormant, the field is likely to erupt again within the next "hundreds to thousands of years", a very short timeframe in geologic terms. The field contains at least 40 volcanoes, most recently active about 600 years ago at Rangitoto Island, erupting of lava.

The soils of the Pacific Ring of Fire include andosols, also known as andisols; they have formed by the weathering of volcanic ash. Andosols contain large proportions of volcanic glass. The Ring of Fire is the world's main location for this soil type, which typically has good levels of fertility.