Posted: February 13th, 2022

Natural Disaster

Earthquake, shaking of the Earth’s floor attributable to fast motion of the Earth’s rocky outer layer. Earthquakes happen when vitality saved inside the Earth, normally within the type of pressure in rocks, instantly releases. This vitality is transmitted to the floor of the Earth by earthquake waves. The destruction an earthquake causes is determined by its magnitude and period, or the quantity of shaking that happens. A construction’s design and the supplies utilized in its building additionally have an effect on the quantity of injury the construction incurs. Earthquakes fluctuate from small, imperceptible shaking to massive shocks felt over 1000’s of kilometers.
Earthquakes can deform the bottom, make buildings and different buildings collapse, and create tsunamis (massive sea waves). Lives could also be misplaced within the ensuing destruction. Within the final 500 years, a number of million folks have been killed by earthquakes all over the world, together with over 240,000 within the 1976 T’ang-Shan, China, earthquake. Worldwide, earthquakes have additionally brought on extreme property and structural harm. Satisfactory precautions, corresponding to training, emergency planning, and setting up stronger, extra versatile, safely designed buildings, can restrict the lack of life and reduce the harm attributable to earthquakes.
Focus and Epicenter- The purpose inside the Earth alongside the rupturing geological fault the place an earthquake originates is known as the main focus, or hypocenter. The purpose on the Earth’s floor straight above the main focus is known as the epicenter. Faults- Stress within the Earth’s crust creates faults, leading to earthquakes. The properties of an earthquake rely strongly on the kind of fault slip, or motion alongside the fault, that causes the earthquake. Geologists categorize faults in keeping with the path of the fault slip.

The floor between the 2 sides of a fault lies in a airplane, and the path of the airplane is normally not vertical; fairly it dips at an angle into the Earth. Waves- The sudden motion of rocks alongside a fault causes vibrations that transmit vitality by means of the Earth within the type of waves. Waves that journey within the rocks under the floor of the Earth are known as physique waves, and there are two sorts of physique waves: major, or P, waves, and secondary, or S, waves. The S waves, often known as shearing waves, transfer the bottom forwards and backwards Results Of Earthquake
Floor Shaking and Landslides-Earthquake waves make the bottom transfer, shaking buildings and inflicting poorly designed or weak buildings to partially or completely collapse. The bottom shaking weakens soils and basis supplies below buildings and causes dramatic modifications in fine-grained soils. Throughout an earthquake, water-saturated sandy soil turns into like liquid mud, an impact known as liquefaction. Liquefaction causes harm as the inspiration soil beneath buildings and buildings weakens. Fireplace-One other post-earthquake menace is hearth, such because the fires.
The quantity of injury attributable to post-earthquake hearth is determined by the sorts of constructing supplies used, whether or not water strains are intact, and whether or not pure fuel mains have been damaged. Ruptured fuel mains might result in quite a few fires, and hearth preventing can’t be efficient if the water mains will not be intact to move water to the fires. Tsunami Waves and Flooding- Alongside the coasts, sea waves known as tsunamis that accompany some massive earthquakes centered below the ocean may cause extra demise and harm than floor shaking.
Tsunamis are normally made up of a number of oceanic waves that journey out from the slipped fault and arrive one after the opposite on shore. They will strike with out warning, usually in locations very distant from the epicenter of the earthquake. Tsunami waves are typically inaccurately known as tidal waves, however tidal forces don’t trigger them. Fairly, tsunamis happen when a serious fault below the ocean flooring instantly slips. The displaced rock pushes water above it like an enormous paddle, producing highly effective water waves on the ocean floor.
The ocean waves unfold out from the neighborhood of the earthquake supply and transfer throughout the ocean till they attain the shoreline, the place their peak will increase as they attain the continental shelf, the a part of the Earth’s crust that slopes, or rises, from the ocean flooring as much as the land. Illness-Catastrophic earthquakes can create a danger of widespread illness outbreaks, particularly in underdeveloped international locations. Harm to water provide strains, sewage strains, and hospital services in addition to lack of housing might result in circumstances that contribute to the unfold of contagious illnesses, corresponding to influenza (the flu) and different viral infections.
Blizzard Blizzard, extreme storm characterised by excessive chilly, sturdy winds, and a heavy snowfall. These storms are most typical to the western United States however typically happen in different elements of the nation. In response to the U. S. Nationwide Climate Service, winds of 35 mph (56. Three km/h) or extra and visibility of zero. 25 mi (zero. 40 km) or much less are circumstances that, in the event that they endure for 3 hours, outline a blizzard. The nice blizzard of March 11-14, 1888, which coated the jap U. S. , was maybe probably the most paralyzing of any storm on file.
Cyclone Cyclone, in strict meteorological terminology, an space of low atmospheric strain surrounded by a wind system blowing, within the northern hemisphere, in a counterclockwise path. A corresponding high-pressure space with clockwise winds is named an anticyclone. Within the southern hemisphere these wind instructions are reversed. Cyclones are generally known as lows and anticyclones highs. The time period cyclone has usually been extra loosely utilized to a storm and disturbance attending such strain methods, significantly the violent tropical hurricane and the storm, which middle on areas of unusually low strain.
Hurricane Hurricane, identify given to violent storms that originate over the tropical or subtropical waters of the Atlantic Ocean, Caribbean Sea, Gulf of Mexico, or North Pacific Ocean east of the Worldwide Date Line. Such storms over the North Pacific west of the Worldwide Date Line are known as typhoons; these elsewhere are generally known as tropical cyclones, which is the overall identify for all such storms together with hurricanes and typhoons. These storms may cause nice harm to property and lack of human life attributable to excessive winds, flooding, and huge waves crashing in opposition to shorelines.
How Hurricanes Kind-Tropical cyclones kind and develop over heat ocean water, drawing their vitality from latent warmth. Latent warmth is the vitality launched when water vapor in rising scorching, humid air condenses into clouds and rain. As warmed air rises, extra air flows into the world the place the air is rising, creating wind. The Earth’s rotation causes the wind to comply with a curved path over the ocean (the Coriolis impact), which helps give tropical cyclones their round look. Hurricanes and tropical cyclones kind, keep their power, and develop solely when they’re over ocean water that’s roughly 27°C (80°F).
Such heat causes massive quantities of water to evaporate, making the air very humid. This heat water requirement accounts for the existence of tropical cyclone seasons, which happen usually throughout a hemisphere’s summer time and autumn. As a result of water is gradual to heat up and funky down, oceans don’t turn into heat sufficient for tropical cyclones to happen within the spring. Oceans can turn into heat sufficient in the summertime for hurricanes to develop, and the oceans additionally retain summer time warmth by means of the autumn.
Hurricanes weaken and die out when lower off from heat, humid air as they transfer over cooler water or land however can stay harmful as they weaken. Hurricanes and different tropical cyclones start as disorganized clusters of showers and thunderstorms. When considered one of these clusters turns into organized with its winds making an entire circle round a middle, it’s known as a tropical melancholy. When a melancholy’s sustained winds attain 63 km/h (39 mph) or extra, it turns into a tropical storm and is given a reputation. By definition, a tropical storm turns into a hurricane when winds attain 119 km/h (74 mph) or extra.
Traits of Hurricane-A hurricane consists of bands of thunderstorms that spiral towards the low-pressure middle, or “eye” of the storm. Winds additionally spiral in towards the middle, rushing up as they method the attention. Massive thunderstorms create an “eye wall” across the middle the place winds are the strongest. Winds within the eye itself are practically calm, and the sky is usually clear. Air pressures within the eye on the floor vary from round 982 hectopascals (29 inches of mercury) in a weak hurricane to decrease than 914 hectopascals (27 inches of mercury) within the strongest storms. Hectopascals are the metric unit of air strain and are the identical as millibars, a time period utilized by many climate forecasters in america. Hectopascals is the popular time period in scientific journals and is getting used extra usually in public forecasts in nations that use the metric system. )In a big, sturdy storm, hurricane-force winds could also be felt over an space with a diameter of greater than 100 km (60 m). The diameter of the world affected by gale winds and torrential rain can lengthen one other 200 km (120 m) or extra outward from the attention of the storm.
The diameter of the attention could also be lower than 16 km (10 m) in a powerful hurricane to greater than 48 km (30 m) in a weak storm. The smaller the diameter of the attention, the stronger the hurricane winds can be. A hurricane’s power is rated from Class 1, which has winds of at the least 119 km/h (74 mph), to Class 5, which has winds of greater than 249 km/h (155 mph). These classes, generally known as the Saffir-Simpson hurricane scale, have been developed within the 1970s. Twister Twister, violently rotating column of air extending from ithin a thundercloud all the way down to floor degree. The strongest tornadoes might sweep homes from their foundations, destroy brick buildings, toss vehicles and faculty buses by means of the air, and even elevate railroad vehicles from their tracks. Tornadoes fluctuate in diameter from tens of meters to just about 2 km (1 mi), with a median diameter of about 50 m (160 ft). Most tornadoes within the northern hemisphere create winds that blow counterclockwise round a middle of extraordinarily low atmospheric strain. Within the southern hemisphere the winds usually blow clockwise.
Peak wind speeds can vary from close to 120 km/h (75 mph) to nearly 500 km/h (300 mph). The ahead movement of a twister can vary from a close to standstill to nearly 110 km/h (70 mph). A twister turns into seen when a condensation funnel made from water vapor (a funnel cloud) types in excessive low pressures, or when the twister lofts mud, filth, and particles upward from the bottom. A mature twister could also be columnar or tilted, slender or broad—typically so broad that it seems as if the dad or mum thundercloud itself had descended to floor degree. Some tornadoes resemble a swaying elephant’s trunk.
Others, particularly very violent ones, might break into a number of intense suction vortices—intense swirling plenty of air—every of which rotates close to the dad or mum twister. A suction vortex could also be just a few meters in diameter, and thus can destroy one home whereas leaving a neighboring home comparatively unscathed. Formation-Many tornadoes, together with the strongest ones, develop from a particular kind of thunderstorm generally known as a supercell. A supercell is a long-lived, rotating thunderstorm 10 to 16 km (6 to 10 mi) in diameter which will final a number of hours, journey lots of of miles, and produce a number of tornadoes.
Supercell tornadoes are sometimes produced in sequence, in order that what seems to be a really lengthy harm path from one twister may very well be the results of a brand new twister that types within the space the place the earlier twister died. Typically, twister outbreaks happen, and swarms of supercell storms might happen. Every supercell might spawn a twister or a sequence of tornadoes. The entire means of twister formation in supercells continues to be debated amongst meteorologists. Scientists usually agree that the primary stage in twister formation is an interplay between the storm updraft and the winds.
An updraft is a present of heat, moist air that rises upward by means of the thunderstorm. The updraft interacts with the winds, which should change with peak in favorable methods for the interplay to happen. This interplay causes the updraft to rotate on the center ranges of the ambiance. The rotating updraft, generally known as a mesocyclone, stabilizes the thunderstorm and provides it its long-lived supercell traits. The following stage is the event of a powerful downdraft (a present of cooler air that strikes in a downward path) on the bottom of the storm, generally known as a rear-flank downdraft.
It’s not clear whether or not the rear-flank downdraft is induced by rainfall or by strain forces arrange within the storm, though it turns into progressively colder because the rain evaporates into it. This chilly air strikes downward as a result of it’s denser than heat air. The velocity of the downdraft will increase and the air plunges to the bottom, the place it followers out at speeds that may exceed 160 km/h (100 mph). The favored location for the event of a twister is on the space between this rear-flank downdraft and the primary storm updraft.
Nonetheless, the main points of why a twister ought to kind there are nonetheless not clear. The identical condensation course of that creates tornadoes makes seen the widely weaker sea-going tornadoes, known as waterspouts. Waterspouts happen most incessantly in tropical waters. OccurrenceThe United States has the best common annual variety of tornadoes on the planet, about 800 per yr. Exterior america, Australia ranks second in twister frequency. Tornadoes additionally happen in lots of different international locations, together with China, India, Russia, England, and Germany.
Bangladesh has been struck a number of occasions by devastating killer tornadoes. In america, tornadoes happen in all 50 states. Nonetheless, the area with probably the most tornadoes is “Twister Alley,” a swath of the Midwest extending from the Texas Gulf Coastal Plain northward by means of jap South Dakota. One other space of excessive focus is “Dixie Alley,” which extends throughout the Gulf Coastal Plain from south Texas eastward to Florida. Tornadoes are most frequent within the Midwest, the place circumstances are most favorable for the event of the extreme thunderstorms that produce tornadoes.
The Gulf of Mexico ensures a provide of moist, heat air that allows the storms to outlive. Climate circumstances that set off extreme thunderstorms are incessantly in place right here: convergence (flowing collectively) of air alongside boundaries between dry and moist air plenty, convergence of air alongside the boundaries between heat and chilly air plenty, and low strain methods within the higher ambiance touring eastward throughout the plains. In winter, twister exercise is normally confined to the Gulf Coastal Plain. In spring, probably the most lively twister season, tornadoes sometimes happen in central Twister Alley and astward into the Ohio Valley. In summer time, most tornadoes happen in a northern band stretching from the Dakotas eastward into Pennsylvania and southern New York State. The worst twister disasters in america have claimed lots of of lives. The Tri-State Outbreak of March 18, 1925, had the best demise toll: 740 folks died in 7 tornadoes that struck Illinois, Missouri, and Indiana. The Tremendous Outbreak of April Three-Four, 1974, spawned 148 tornadoes (probably the most in any recognized outbreak) and killed 315 folks from Alabama north to Ohio.
Floods When it rains or snows, among the water is retained by the soil, some is absorbed by vegetation, some evaporates, and the rest, which reaches stream channels, is known as runoff. Floods happen when soil and vegetation can’t take in all of the water; water then runs off the land in portions that can’t be carried in stream channels or retained in pure ponds and constructed reservoirs. About 30 % of all precipitation is runoff, and this quantity could also be elevated by melting snow plenty.
Periodic floods happen naturally on many rivers, forming an space generally known as the flood plain. These river floods usually consequence from heavy rain, typically mixed with melting snow, which causes the rivers to overflow their banks; a flood that rises and falls quickly with little or no advance warning is known as a flash flood. Flash floods normally consequence from intense rainfall over a comparatively small space. Coastal areas are often flooded by unusually excessive tides induced by extreme winds over ocean surfaces, or by tsunamis attributable to undersea earthquakes.
Results of Floods-Floods not solely harm property and endanger the lives of people and animals, however produce other results as properly. Speedy runoff causes soil erosion in addition to sediment deposition issues downstream. Spawning grounds for fish and different wildlife habitat are sometimes destroyed. Excessive-velocity currents improve flood harm; extended excessive floods delay visitors and intrude with drainage and financial use of lands. Bridge abutments, financial institution strains, sewer outfalls, and different buildings inside floodways are broken, and navigation and hydroelectric energy are sometimes impaired.
Monetary losses attributable to floods are generally hundreds of thousands of annually. Drought Drought, situation of abnormally dry climate inside a geographic area the place some rain may normally be anticipated. A drought is thus fairly completely different from a dry local weather, which designates a area that’s usually, or at the least seasonally, dry. The time period drought is utilized to a interval during which an uncommon shortage of rain causes a severe hydrological imbalance: Water-supply reservoirs empty, wells dry up, and crop harm ensues.
The severity of the drought is gauged by the diploma of moisture deficiency, its period, and the dimensions of the world affected. If the drought is transient, it is named a dry spell, or partial drought. A partial drought is normally outlined as greater than 14 days with out considerable precipitation, whereas a drought might final for years. Droughts are usually extra extreme in some areas than in others. Catastrophic droughts usually happen at latitudes of about 15°-20°, in areas bordering the completely arid areas of the world.
Everlasting aridity is a attribute of these areas the place heat, tropical air plenty, in descending to earth, turn into hotter and drier. When a poleward shift within the prevailing westerlies happens , the high-pressure, anticyclonic circumstances of the completely arid areas impinge on areas which might be usually topic to seasonally moist low-pressure climate and a drought ensues. A southward shift within the westerlies brought on probably the most extreme drought of the 20th century, the one which stricken the African area known as the Sahel for a dozen years, starting in 1968.
In North America, archaeological research of Native People and statistics derived from long-term agricultural data present that six or seven centuries in the past entire areas of the Southwest have been deserted by the indigenous agriculturists due to repeated droughts and have been by no means reoccupied. The statistics point out that roughly each 22 years—with a precision of three to 4 years—a serious drought happens in america, most significantly affecting the Prairie and midwestern states.
The disastrous drought of the 1930s, throughout which massive areas of the Nice Plains grew to become generally known as the Mud Bowl, is one instance. The impact of the drought was aggravated by overcropping, overpopulation, and lack of well timed aid measures. In Africa, the Sahel drought was additionally aggravated by nonclimatic determinants corresponding to overcropping, in addition to by issues between nations and peoples unfriendly with each other. Though drought can’t be reliably predicted, sure precautions might be taken in drought-risk areas.
These embrace building of reservoirs to carry emergency water provides, training to keep away from overcropping and overgrazing, and applications to restrict settlement in drought-prone areas. Volcano Volcano, mountain or hill fashioned by the buildup of supplies erupted by means of a number of openings (known as volcanic vents) within the earth’s floor. The time period volcano may discuss with the vents themselves. Most volcanoes have steep sides, however some might be gently sloping mountains and even flat tablelands, plateaus, or plains.
The volcanoes above sea degree are the perfect recognized, however the overwhelming majority of the world’s volcanoes lie beneath the ocean, fashioned alongside the worldwide oceanic ridge methods that crisscross the deep ocean flooring . In response to the Smithsonian Establishment, 1,511 above-sea volcanoes have been lively throughout the previous 10,000 years, 539 of them erupting a number of occasions throughout written historical past. On common, 50 to 60 above-sea volcanoes worldwide are lively in any given yr; about half of those are continuations of eruptions from earlier years, and the remainder are new.
Volcano Formation-All volcanoes are fashioned by the buildup of magma (molten rock that types under the earth’s floor). Magma can erupt by means of a number of volcanic vents, which is usually a single opening, a cluster of openings, or a protracted crack, known as a fissure vent. It types deep inside the earth, usually inside the higher a part of the mantle (one of many layers of the earth’s crust), or much less generally, inside the base of the earth’s crust. Excessive temperatures and pressures are wanted to kind magma.
The stable mantle or crustal rock should be melted below circumstances sometimes reached at depths of 80 to 100 km (50 to 60 mi) under the earth’s floor. As soon as tiny droplets of magma are fashioned, they start to rise as a result of the magma is much less dense than the stable rock surrounding it. The processes that trigger the magma to rise are poorly understood, nevertheless it usually strikes upward towards decrease strain areas, squeezing into areas between minerals inside the stable rock. As the person magma droplets rise, they be part of to kind ever-larger blobs and transfer towards the floor.
The bigger the rising blob of magma, the better it strikes. Rising magma doesn’t attain the floor in a gradual method however tends to build up in a number of underground storage areas, known as magma reservoirs, earlier than it erupts onto the floor. With every eruption, whether or not explosive or nonexplosive, the fabric erupted provides one other layer to the rising volcano. After many eruptions, the volcanic supplies pile up across the vent or vents. These piles kind a topographic characteristic, corresponding to a hill, mountain, plateau, or crater, that we acknowledge as a volcano.
Many of the earth’s volcanoes are fashioned beneath the oceans, and their areas have been documented in current a long time by mapping of the ocean flooring. Volcanic Supplies- 1-Lava-Lava is magma that breaks the floor and erupts from a volcano. If the magma may be very fluid, it flows quickly down the volcano’s slopes. Lava that’s extra sticky and fewer fluid strikes slower. Lava flows which have a steady, clean, ropy, or billowy floor are known as pahoehoe (pronounced pah HOH ee hoh ee) flows, whereas aa (pronounced ah ah) flows have a jagged floor composed of free, irregularly formed lava chunks.
As soon as cooled, pahoehoe types clean rocks, whereas aa types jagged rocks. The phrases pahoehoe and aa are Hawaiian phrases that describe the feel of the lava. Lava might also be described when it comes to its composition and the kind of rock it types. Basalt, andesite, , and rhyolite are all completely different sorts of rock that kind from lava. Every kind of rock, and the lava from which it types, accommodates a distinct quantity of the compound silicon dioxide. Basaltic lava has the least quantity of silicon dioxide, andesitic and dacitic lava have medium ranges of silicon dioxide, whereas rhyolitic lava has probably the most. -Tephra-Tephra, or pyroclastic materials, is made from rock fragments fashioned by explosive shattering of sticky magma (see Pyroclastic Circulate). The time period pyroclastic is of Greek origin and means ‘fire-broken’ (pyro, “hearth”; klastos, “damaged”). Tephra refers to any airborne pyroclastic materials no matter measurement or form. The perfect-known tephra supplies embrace pumice, cinders, and volcanic ash. These fragments are exploded when gases construct up inside a volcano and produce an explosion. The items of magma are shot into the air throughout the explosion.
Ash refers to fragments smaller than 2 mm (zero. 08 in) in diameter. The best ash is known as volcanic mud and is made up of particles which might be lower than zero. 06 mm (zero. 002 in) in diameter. Volcanic blocks, or bombs, are the biggest fragments of tephra, greater than 64 mm (2. 5 in) in diameter (baseball measurement or bigger). Some bombs might be the dimensions of a small automobile. Three-Gases-Gases, primarily within the type of steam, are launched from volcanoes throughout eruptions. All eruptions, explosive or nonexplosive, are accompanied by the discharge of volcanic fuel.
The sudden escape of high-pressure volcanic fuel from magma is the driving pressure for eruptions. Gases come from the magma itself or from the recent magma coming into contact with water within the floor. Volcanic plumes can seem darkish throughout an eruption as a result of the gases are blended with dark-colored supplies corresponding to tephra. Most volcanic gases predominantly encompass water vapor (steam), with carbon dioxide (CO2) and sulfur dioxide (SO2) being the following two most typical compounds together with smaller quantities of chlorine and fluorine gases.
Kinds of Volcano 1-Cinder Cones and Composite Volcanoes-Cinder cones and composite volcanoes have the acquainted conelike form that individuals most frequently affiliate with volcanoes. A few of these kind fantastically symmetrical volcanic hills or mountains corresponding to Paricutin Volcano in Mexico and Mount Fuji in Japan. Though each cinder cones and composite volcanoes are largely the outcomes of explosive eruptions, cinder cones consist solely of fragmental lava. This fragmental lava is erupted explosively and made up of cinders. -Defend Volcanoes-Defend volcanoes (additionally known as volcanic shields) get their identify from their distinctive, gently sloping mound-like shapes that resemble the preventing shields that historic warriors carried into battle.
Their shapes replicate the truth that they’re constructed primarily of numerous fluid basaltic lava flows that erupted nonexplosively. Such flows can simply unfold nice distances from the feeding volcanic vents, much like the spreading out of scorching syrup poured onto a plate. Volcanic shields could also be both small or massive, and the biggest protect volcanoes are many occasions bigger than the biggest composite volcanoes. -Caldera-A caldera is a spherical or oval-shaped low-lying space that types when the bottom collapses due to explosive eruptions. An explosive eruption can explode the highest off of the mountain or eject the entire magma that’s contained in the volcano. Both of those actions might trigger the volcano to break down. Calderas might be greater than the biggest protect volcanoes in diameter. Such volcanic options, if geologically younger, are sometimes outlined by an irregular, steep-walled boundary (a caldera rim), which displays the unique ringlike zone, or fault, alongside which the bottom collapse occurred.
Some calderas have hills and mountains rising inside them, known as resurgent domes, that replicate volcanic exercise after the preliminary collapse. Four-Volcanic Plateaus-A number of the largest volcanic options on earth don’t truly appear to be volcanoes. As an alternative, they kind in depth, practically flat-topped accumulations of erupted supplies. These supplies kind volcanic plateaus or plains overlaying many 1000’s of sq. kilometers. The volcanic supplies might be both very fluid basaltic lava flows or far-traveled pyroclastic flows.
The basaltic lava flows are known as flood or plateau basalts and are erupted from many fissure vents. Volcano Hazards-Eruptions pose direct and oblique volcano hazards to folks and property, each on the bottom and within the air. Direct hazards are pyroclastic flows, lava flows, falling ash, and particles flows. Pyroclastic flows are mixtures of scorching ash, rock fragments, and fuel. They’re particularly lethal due to their excessive temperatures of 850° C (1600° F) or larger and quick speeds of 250 km/h (160 mph) or better.
Lava flows, which transfer far more slowly than pyroclastic flows, are not often life threatening however can produce huge property harm and financial loss. Heavy accumulations of volcanic ash, particularly in the event that they turn into moist from rainfall, can collapse roofs and harm crops. Particles flows known as lahars are composed of moist concretelike mixtures of volcanic particles and water from melted snow or ice or heavy rainfall. Lahars can journey shortly by means of valleys, destroying all the things of their paths. Pyroclastic and volcanic particles flows have brought on probably the most eruption-related deaths within the 20th century.

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