1001:
2542:. Even then, some eruptions will have no useful warning. An example of this occurred in March 2017, when a tourist group was witnessing a presumed to be predictable Mount Etna eruption and the flowing lava came in contact with a snow accumulation causing a situational phreatic explosion causing injury to ten persons. Other types of significant eruptions are known to give useful warnings of only hours at the most by seismic monitoring. The recent demonstration of a magma chamber with repose times of tens of thousands of years, with potential for rapid recharge so potentially decreasing warning times, under the youngest volcano in central Europe, does not tell us if more careful monitoring will be useful.
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453:
33:
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volcanic activities. While the science of volcanology may not yet be capable of predicting the exact times and dates of eruptions far into the future, on suitably monitored volcanoes the monitoring of ongoing volcanic indicators is often capable of predicting imminent eruptions with advance warnings minimally of hours, and usually of days prior to any eruptions. The diversity of volcanoes and their complexities mean that eruption forecasts for the foreseeable future will be based on
617:
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ability is derived via such volcanic-activity monitoring programs, through the greater abilities of local officials to facilitate timely evacuations based upon the greater modern-day knowledge of volcanism that is now available, and upon improved communications technologies such as cell phones. Such operations tend to provide enough time for humans to escape at least with their lives before a pending eruption. One example of such a recent successful volcanic evacuation was the
1150:
2278:
4123:
1958:
1174:
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3000:
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387:, which are hypothesized to be columns of hot material rising from the core-mantle boundary. As with mid-ocean ridges, the rising mantle rock experiences decompression melting which generates large volumes of magma. Because tectonic plates move across mantle plumes, each volcano becomes inactive as it drifts off the plume, and new volcanoes are created where the plate advances over the plume. The
456:
455:
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460:
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1406:) are highly hazardous products of such volcanoes since they hug the volcano's slopes and travel far from their vents during large eruptions. Temperatures as high as 850 °C (1,560 °F) are known to occur in pyroclastic flows, which will incinerate everything flammable in their path, and thick layers of hot pyroclastic flow deposits can be laid down, often many meters thick.
461:
458:
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1156:
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2431:) with major historical volcanic eruptions in the 19th and 20th century (VEI 5, 6 and 7). From left to right: Yellowstone 2.1 Ma, Yellowstone 1.3 Ma, Long Valley 6.26 Ma, Yellowstone 0.64 Ma . 19th century eruptions: Tambora 1815, Krakatoa 1883. 20th century eruptions: Novarupta 1912, St. Helens 1980, Pinatubo 1991.
1157:
5555:
Wieczorek, Mark A.; Jolliff, Bradley L.; Khan, Amir; Pritchard, Matthew E.; Weiss, Benjamin P.; Williams, James G.; Hood, Lon L.; Righter, Kevin; Neal, Clive R.; Shearer, Charles K.; McCallum, I. Stewart; Tompkins, Stephanie; Hawke, B. Ray; Peterson, Chris; Gillis, Jeffrey J.; Bussey, Ben (January 1,
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Although volcanic eruptions pose considerable hazards to humans, past volcanic activity has created important economic resources. Tuff formed from volcanic ash is a relatively soft rock, and it has been used for construction since ancient times. The Romans often used tuff, which is abundant in Italy,
1896:
in 2008. Modern volcanic activity monitoring techniques, and improvements in the modelling of the factors that produce eruptions, have helped the understanding of why volcanoes may remain dormant for a long time, and then become unexpectedly active again. The potential for eruptions, and their style,
1477:
rises into the overlying mantle, lowering its melting point, particularly for the more silica-rich minerals. Fractional crystallization further enriches the magma in silica. It has also been suggested that intermediate magmas are produced by the melting of sediments carried downwards by the subducted
1887:
pointed out that the term "dormant" in reference to volcanoes has been deprecated over the past few decades and that "he term "dormant volcano" is so little used and undefined in modern volcanology that the
Encyclopedia of Volcanoes (2000) does not contain it in the glossaries or index", however the
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words. Ê»AÊ»a is characterized by a rough, clinkery surface and is the typical texture of cooler basalt lava flows. PÄhoehoe is characterized by its smooth and often ropey or wrinkly surface and is generally formed from more fluid lava flows. PÄhoehoe flows are sometimes observed to transition to Ê»aÊ»a
1015:
Epoch has been documented at only 119 submarine volcanoes, but there may be more than one million geologically young submarine volcanoes on the ocean floor. In shallow water, active volcanoes disclose their presence by blasting steam and rocky debris high above the ocean's surface. In the deep ocean
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Volcanic ash and weathered basalt produce some of the most fertile soil in the world, rich in nutrients such as iron, magnesium, potassium, calcium, and phosphorus. Volcanic activity is responsible for emplacing valuable mineral resources, such as metal ores. It is accompanied by high rates of heat
2033:
The three common popular classifications of volcanoes can be subjective and some volcanoes thought to have been extinct have erupted again. To help prevent people from falsely believing they are not at risk when living on or near a volcano, countries have adopted new classifications to describe the
1698:
Vulcanian eruptions are characterized by yet higher viscosities and partial crystallization of magma, which is often intermediate in composition. Eruptions take the form of short-lived explosions for several hours, which destroy a central dome and eject large lava blocks and bombs. This is followed
1355:
The form and style of an eruption of a volcano is largely determined by the composition of the lava it erupts. The viscosity (how fluid the lava is) and the amount of dissolved gas are the most important characteristics of magma, and both are largely determined by the amount of silica in the magma.
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found in East
African volcanic ash dated at 3.66 million years old. The association of volcanoes with fire and disaster is found in many oral traditions and had religious and thus social significance before the first written record of concepts related to volcanoes. Examples are: (1) the stories in
1928:
was an inconspicuous volcano, unknown to most people in the surrounding areas, and initially not seismically monitored before its unanticipated and catastrophic eruption of 1991. Two other examples of volcanoes that were once thought to be extinct, before springing back into eruptive activity were
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The USGS defines a dormant volcano as any volcano that is not showing any signs of unrest such as earthquake swarms, ground swelling, or excessive noxious gas emissions, but which shows signs that it could yet become active again. Many dormant volcanoes have not erupted for thousands of years, but
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is a common eruptive product of submarine volcanoes and is characterized by thick sequences of discontinuous pillow-shaped masses which form underwater. Even large submarine eruptions may not disturb the ocean surface, due to the rapid cooling effect and increased buoyancy in water (as compared to
2024:
can have eruptive lifespans sometimes measured in millions of years, a caldera that has not produced an eruption in tens of thousands of years may be considered dormant instead of extinct. An individual volcano in a monogenetic volcanic field can be extinct but that does not mean a completely new
909:
A supervolcano is defined as a volcano that has experienced one or more eruptions that produced over 1,000 cubic kilometers (240 cu mi) of volcanic deposits in a single explosive event. Such eruptions occur when a very large magma chamber full of gas-rich, silicic magma is emptied in a
2549:
Thus in many cases, while volcanic eruptions may still cause major property destruction, the periodic large-scale loss of human life that was once associated with many volcanic eruptions, has recently been significantly reduced in areas where volcanoes are adequately monitored. This life-saving
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Many volcanoes near human settlements are heavily monitored with the aim of providing adequate advance warnings of imminent eruptions to nearby populations. Also, a better modern-day understanding of volcanology has led to some better informed governmental and public responses to unanticipated
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are widespread and forms of volcanism not present on Earth occur as well. Changes in the planet's atmosphere and observations of lightning have been attributed to ongoing volcanic eruptions, although there is no confirmation of whether or not Venus is still volcanically active. However, radar
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707:(both resemble cinders, hence the name of this volcano type) that build up around the vent. These can be relatively short-lived eruptions that produce a cone-shaped hill perhaps 30 to 400 meters (100 to 1,300 ft) high. Most cinder cones erupt only once and some may be found in
473:
A volcano needs a reservoir of molten magma (e.g. a magma chamber), a conduit to allow magma to rise through the crust, and a vent to allow the magma to escape above the surface as lava. The erupted volcanic material (lava and tephra) that is deposited around the vent is known as a
1633:(shattered volcanic material) make up more of the volume of many volcanoes than do lava flows. Volcaniclastics may have contributed as much as a third of all sedimentation in the geologic record. The production of large volumes of tephra is characteristic of explosive volcanism.
1822:, but the definitions of these terms are not entirely uniform amongst volcanologists. The level of activity of most volcanoes falls upon a graduated spectrum, with much overlap between categories, and does not always fit neatly into only one of these three separate categories.
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Scientists are known to perceive risk, with its social elements, differently from local populations and those that undertake social risk assessments on their behalf, so that both disruptive false alarms and retrospective blame, when disasters occur, will continue to happen.
929:, and about 60 historical VEI 8 eruptions have been identified in the geologic record over millions of years. A supervolcano can produce devastation on a continental scale, and severely cool global temperatures for many years after the eruption due to the huge volumes of
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Citizens who may be concerned about their own exposure to risk from nearby volcanic activity should familiarize themselves with the types of, and quality of, volcano monitoring and public notification procedures being employed by governmental authorities in their areas.
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posed the greatest volcanic hazard to civilizations. The lavas of stratovolcanoes are higher in silica, and therefore much more viscous, than lavas from shield volcanoes. High-silica lavas also tend to contain more dissolved gas. The combination is deadly, promoting
245:
During the development of geological theory, certain concepts that allowed the grouping of volcanoes in time, place, structure and composition have developed that ultimately have had to be explained in the theory of plate tectonics. For example, some volcanoes are
1443:
Felsic magmas are formed within the crust, usually through the melting of crust rock from the heat of underlying mafic magmas. The lighter felsic magma floats on the mafic magma without significant mixing. Less commonly, felsic magmas are produced by extreme
5012:
Aiuppa, Alessandro; Moretti, Roberto; Federico, Cinzia; Giudice, Gaetano; Gurrieri, Sergio; Liuzzo, Marco; Papale, Paolo; Shinohara, Hiroshi; Valenza, Mariano (2007). "Forecasting Etna eruptions by real-time observation of volcanic gas composition".
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and may progress to the point where a tectonic plate is completely split. A divergent plate boundary then develops between the two halves of the split plate. However, rifting often fails to completely split the continental lithosphere (such as in an
627:
Shield volcanoes, so named for their broad, shield-like profiles, are formed by the eruption of low-viscosity lava that can flow a great distance from a vent. They generally do not explode catastrophically but are characterized by relatively gentle
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Magmatic eruptions are driven primarily by gas release due to decompression. Low-viscosity magma with little dissolved gas produces relatively gentle effusive eruptions. High-viscosity magma with a high content of dissolved gas produces violent
457:
2078:(IAVCEI) as being worthy of particular study in light of their history of large, destructive eruptions and proximity to populated areas. They are named Decade Volcanoes because the project was initiated as part of the United Nations-sponsored
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is constantly being resurfaced. Its lavas are the hottest known anywhere in the Solar System, with temperatures exceeding 1,800 K (1,500 °C). In
February 2001, the largest recorded volcanic eruptions in the Solar System occurred on Io.
1891:
Previously a volcano was often considered to be extinct if there were no written records of its activity. Such a generalisation is inconsistent with observation and deeper study, as has occurred recently with the unexpected eruption of the
2639:, indicating that volcanism played a major role in shaping its surface. The planet may have had a major global resurfacing event about 500 million years ago, from what scientists can tell from the density of impact craters on the surface.
1682:
Strombolian eruptions are characterized by moderate viscosities and dissolved gas levels. They are characterized by frequent but short-lived eruptions that can produce eruptive columns hundreds of meters high, which can also be seen in
501:
at its summit; however, this describes just one of the many types of volcano. The features of volcanoes are varied. The structure and behavior of volcanoes depend on several factors. Some volcanoes have rugged peaks formed by
325:
zones are places where two plates, usually an oceanic plate and a continental plate, collide. The oceanic plate subducts (dives beneath the continental plate), forming a deep ocean trench just offshore. In a process called
3568:
Lawrence, S.J.; Stopar, J.D.; Hawke, B.R.; Greenhagen, B.T.; Cahill, J.T.S.; Bandfield, J.L.; Jolliff, B.L.; Denevi, B.W.; Robinson, M.S.; Glotch, T.D.; Bussey, D.B.J.; Spudis, P.D.; Giguere, T.A.; Garry, W.B. (2013).
1140:
Mud volcanoes (mud domes) are formations created by geo-excreted liquids and gases, although several processes may cause such activity. The largest structures are 10 kilometers in diameter and reach 700 meters high.
1613:(long dimension is several mm): the curved shapes of altered glass shards (ash fragments) are well preserved, although the glass is partly altered. The shapes were formed around bubbles of expanding, water-rich gas.
2075:
1495:. These lavas are usually hotter and much less viscous than felsic lavas. Mafic magmas are formed by partial melting of the dry mantle, with limited fractional crystallization and assimilation of crustal material.
2034:
various levels and stages of volcanic activity. Some alert systems use different numbers or colors to designate the different stages. Other systems use colors and words. Some systems use a combination of both.
152:
Other planets besides Earth have volcanoes. For example, volcanoes are very numerous on Venus. In 2009, a paper was published suggesting a new definition for the word 'volcano' that includes processes such as
1152:
632:. Since low-viscosity magma is typically low in silica, shield volcanoes are more common in oceanic than continental settings. The Hawaiian volcanic chain is a series of shield cones, and they are common in
1617:
Tephra is made when magma inside the volcano is blown apart by the rapid expansion of hot volcanic gases. Magma commonly explodes as the gas dissolved in it comes out of solution as the pressure decreases
5274:
Marcari, G., G. Fabbrocino, and G. Manfredi. "Shear seismic capacity of tuff masonry panels in heritage constructions." Structural
Studies, Repairs and Maintenance of Heritage Architecture X 95 (2007):
5713:
Robinson, Cordula A.; Thornhill, Gill D.; Parfitt, Elisabeth A. (1995). "Large-scale volcanic activity at Maat Mons: Can this explain fluctuations in atmospheric chemistry observed by
Pioneer Venus?".
3636:
Berger, Melvin, Gilda Berger, and
Higgins Bond. "Volcanoes-why and how ." Why do volcanoes blow their tops?: Questions and answers about volcanoes and earthquakes. New York: Scholastic, 1999. 7. Print.
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Plinian eruptions are the most violent of all volcanic eruptions. They are characterized by sustained huge eruption columns whose collapse produces catastrophic pyroclastic flows. They are named after
877:
like the one that destroyed the city of Saint-Pierre in
Martinique in 1902. They are also steeper than shield volcanoes, with slopes of 30â35° compared to slopes of generally 5â10°, and their loose
2616:
has no large volcanoes and no current volcanic activity, although recent evidence suggests it may still possess a partially molten core. However, the Moon does have many volcanic features such as
242:, and most volcanic activity on Earth takes place along plate boundaries, where plates are converging (and lithosphere is being destroyed) or are diverging (and new lithosphere is being created).
1551:, when the planet's heat flow was higher. They are (or were) the hottest lavas, and were probably more fluid than common mafic lavas, with a viscosity less than a tenth that of hot basalt magma.
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1830:
The USGS defines a volcano as "erupting" whenever the ejection of magma from any point on the volcano is visible, including visible magma still contained within the walls of the summit crater.
936:
Because of the enormous area they cover, and subsequent concealment under vegetation and glacial deposits, supervolcanoes can be difficult to identify in the geologic record without careful
5812:
1741:
are characterized by superheating of groundwater that comes in contact with hot rock or magma. They are distinguished from phreatomagmatic eruptions because the erupted material is all
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with a central fire connected to numerous others depicting volcanoes as a type of safety valve. Edward Jorden, in his work on mineral waters, challenged this view; in 1632 he proposed
1799:(the last 11,700 years) lists 9,901 confirmed eruptions from 859 volcanoes. The database also lists 1,113 uncertain eruptions and 168 discredited eruptions for the same time interval.
838:
that gives rise to the name. They are also known as composite volcanoes because they are created from multiple structures during different kinds of eruptions. Classic examples include
1968:
Extinct volcanoes are those that scientists consider unlikely to erupt again because the volcano no longer has a magma supply. Examples of extinct volcanoes are many volcanoes on the
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monitoring agencies all over the world. They took the form of unusual humming sounds, and some of the signals detected in
November of that year had a duration of up to 20 minutes. An
2869:'s migration through the Hawarian island chain, ability to destroy forests and manifestations of the god's temper, and (3) the association in Javanese folklore of a king resident in
6539:
6125:
Troll, VR; Deegan, FM; Jolis, EM; Budd, DA; Dahren, B; Schwarzkopf, LM (2015). "Ancient oral tradition describes volcanoâearthquake interaction at Merapi volcano, Indonesia".
3498:
Meresse, S.; Costard, F.O.; Mangold, N.; Masson, P.; Neukum, G. (2008). "Formation and evolution of the chaotic terrains by subsidence and magmatism: Hydraotes Chaos, Mars".
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Volcanoes are not distributed evenly over the Earth's surface but active ones with significant impact were encountered early in human history, evidenced by footprints of
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1924:
Accordingly, it can sometimes be difficult to distinguish between an extinct volcano and a dormant (inactive) one. Long volcano dormancy is known to decrease awareness.
1041:
feeding on dissolved minerals. Over time, the formations created by submarine volcanoes may become so large that they break the ocean surface as new islands or floating
980:
Volcanoes that, though large, are not large enough to be called supervolcanoes, may also form calderas in the same way; they are often described as "caldera volcanoes".
750:
Based on satellite images, it has been suggested that cinder cones might occur on other terrestrial bodies in the Solar system too; on the surface of Mars and the Moon.
3735:
Druitt, T. H.; Costa, F.; Deloule, E.; Dungan, M.; Scaillet, B. (2012). "Decadal to monthly timescales of magma transfer and reservoir growth at a caldera volcano".
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had demonstrated by 1794 that steam explosions could cause explosive eruptions and many geologists held this as the universal cause of explosive eruptions up to the
695:, the youngest volcano in El Salvador. Izalco erupted almost continuously from 1770 (when it formed) to 1958, earning it the nickname of "Lighthouse of the Pacific".
304:(also known as deep sea vents) are evidence of this kind of volcanic activity. Where the mid-oceanic ridge is above sea level, volcanic islands are formed, such as
4124:"Descriptive nomenclature and classification of pyroclastic deposits and fragments: recommendations of the IUGS Subcommission on the Systematics of Igneous Rocks"
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5786:
4775:
1706:
Peléan eruptions are more violent still, being characterized by dome growth and collapse that produces various kinds of pyroclastic flows. They are named after
538:
in New
Zealand. Some volcanoes can be low-relief landform features, with the potential to be hard to recognise as such and be obscured by geological processes.
650:
Lava domes are built by slow eruptions of highly viscous lava. They are sometimes formed within the crater of a previous volcanic eruption, as in the case of
3658:
1448:
of more mafic magmas. This is a process in which mafic minerals crystallize out of the slowly cooling magma, which enriches the remaining liquid in silica.
4892:"Constraints on the pre-eruptive magma storage conditions and magma evolution of the 56â30 ka explosive volcanism of Ciomadul (East Carpathians, Romania)"
2079:
1671:
Hawaiian eruptions are typical of volcanoes that erupt mafic lava with a relatively low gas content. These are almost entirely effusive, producing local
106:
has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the
5459:
1655:
Eruption styles are broadly divided into magmatic, phreatomagmatic, and phreatic eruptions. The intensity of explosive volcanism is expressed using the
1060:
research campaign in May 2019 showed that the previously mysterious humming noises were caused by the formation of a submarine volcano off the coast of
417:
Sustained upwelling of hot mantle rock can develop under the interior of a continent and lead to rifting. Early stages of rifting are characterized by
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volcano and a queen resident at a beach 50 km (31 mi) away on what is now known to be an earthquake fault that interacts with that volcano.
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slab. Another process is magma mixing between felsic rhyolitic and mafic basaltic magmas in an intermediate reservoir before emplacement or lava flow.
5519:
5209:
2821:, which is believed to be a significant source of the methane found in its atmosphere. It is theorized that cryovolcanism may also be present on the
561:, which are structures often not associated with known magmatic activity. Active mud volcanoes tend to involve temperatures much lower than those of
6556:
4890:
Cserép, B.; Szemerédi, M.; Harangi, S.; Erdmann, S.; Bachmann, O.; Dunkl, I.; Seghedi, I.; Mészåros, K.; Kovåcs, Z.; Viråg, A; Ntaflos, T. (2023).
2296:
Volcanic eruptions pose a significant threat to human civilization. However, volcanic activity has also provided humans with important resources.
1473:, by several processes. One process is the hydration melting of mantle peridotite followed by fractional crystallization. Water from a subducting
1622:. These violent explosions produce particles of material that can then fly from the volcano. Solid particles smaller than 2 mm in diameter (
4735:
6604:
1897:
depend mainly upon the state of the magma storage system under the volcano, the eruption trigger mechanism and its timescale. For example, the
5820:
1016:
basins, the tremendous weight of the water prevents the explosive release of steam and gases; however, submarine eruptions can be detected by
670:
was an example; lava beneath the surface of the mountain created an upward bulge, which later collapsed down the north side of the mountain.
6303:
6325:
Berryman, Kelvin; Villamor, Pilar; Nairn, Ian.A.; Begg, John; Alloway, Brent V.; Rowland, Julie; Lee, Julie; Capote, Ramon (July 1, 2022).
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that affected the genetic inheritance of all humans today. Volcanic eruptions may have contributed to major extinction events, such as the
658:. Like stratovolcanoes, they can produce violent, explosive eruptions, but the lava generally does not flow far from the originating vent.
2846:
from the host star very close to the planet and neighboring planets could generate intense volcanic activity similar to that found on Io.
2746:, also appears to have an active volcanic system, except that its volcanic activity is entirely in the form of water, which freezes into
4523:
4104:
226:
Map showing the divergent plate boundaries (oceanic spreading ridges) and recent sub-aerial volcanoes (mostly at convergent boundaries)
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Magma rich in silica is much more viscous than silica-poor magma, and silica-rich magma also tends to contain more dissolved gases.
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7227:
3019:
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structure, partial decompression melting of magma, and magma convection. This eventually led to the acceptance of plate tectonics.
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1422:
in 1912, is an example of a thick pyroclastic flow or ignimbrite deposit. Volcanic ash that is light enough to erupt high into the
4689:
1844:
While there is no international consensus among volcanologists on how to define an active volcano, the USGS defines a volcano as
346:. When it does reach the surface, however, a volcano is formed. Thus subduction zones are bordered by chains of volcanoes called
4099:
3533:
BroĆŸ, P.; Hauber, E. (2012). "A unique volcanic field in
Tharsis, Mars: Pyroclastic cones as evidence for explosive eruptions".
1398:
Because felsic magmas are so viscous, they tend to trap volatiles (gases) that are present, which leads to explosive volcanism.
252:
with more than one period of activity during their history; other volcanoes that become extinct after erupting exactly once are
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5535:
3029:
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6442:
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5863:
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4222:
3621:
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2245:, monitors nine volcanoes, two of which are Decade volcanoes. The focus of the Deep Earth Carbon Degassing Project is to use
5257:
3203:
2944:
proposed the core of Earth was incandescent and, by 1785, the works of Decartes and others were synthesised into geology by
2369:
aerosols that can reflect solar radiation and lower surface temperatures significantly. Sulfur dioxide from the eruption of
1445:
111:
7361:
4313:
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the Athabascan subcultures about humans living inside mountains and a woman who uses fire to escape from a mountain, (2)
2246:
2238:
1969:
6327:"Volcano-tectonic interactions at the southern margin of the Okataina Volcanic Centre, TaupĆ Volcanic Zone, New Zealand"
5346:"Making Moai: Reconsidering Concepts of Risk in the Construction of Megalithic Architecture in Rapa Nui (Easter Island)"
2477:" because of the effect on North American and European weather. The freezing winter of 1740â41, which led to widespread
2257:
ratios in real-time and in high-resolution to allow detection of the pre-eruptive degassing of rising magmas, improving
7313:
7298:
6597:
5345:
3014:
2644:
sounding by the Magellan probe revealed evidence for comparatively recent volcanic activity at Venus's highest volcano
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2420:
blades and alter their shape, disrupting the operation of the turbine. This can cause major disruptions to air travel.
904:
330:, water released from the subducting plate lowers the melting temperature of the overlying mantle wedge, thus creating
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near the summit and on the northern flank. However, the interpretation of the flows as ash flows has been questioned.
1000:
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1993:
1961:
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234:, its rigid outer shell, is broken into sixteen larger and several smaller plates. These are in slow motion, due to
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7308:
6012:
Zaitsev, AN; Chakhmouradian, AR; Musiba, C (2023). "Laetoli: The Oldest Known Hominin Footprints in Volcanic Ash".
5286:
1910:
1718:
94:, and because most of Earth's plate boundaries are underwater, most volcanoes are found underwater. For example, a
6384:
3571:"LRO observations of morphology and surface roughness of volcanic cones and lobate lava flows in the Marius Hills"
2899:
However, others proposed more natural (but still incorrect) causes of volcanic activity. In the fifth century BC,
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More silicic lava flows take the form of block lava, where the flow is covered with angular, vesicle-poor blocks.
7772:
7255:
6498:
6170:"Geomythology, theodicy, and the continuing relevance of religious worldviews on responses to volcanic eruptions"
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4508:
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1806:
ranging from several times a year to once in tens of thousands of years. Volcanoes are informally described as
1213:
has erupted continuously for thousands of years, giving rise to its nickname "Lighthouse of the Mediterranean".
1111:
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2416:
where the particles can be melted by the high operating temperature; the melted particles then adhere to the
1411:
5653:
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2704:
spacecraft has found evidence that volcanic activity may have occurred on Mars in the recent past as well.
2478:
5516:
5217:
4170:"Tunable diode laser measurements of hydrothermal/volcanic CO2 and implications for the global CO2 budget"
1005:
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volcano might not erupt close by with little or no warning as its field may have an active magma supply.
1642:
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analyzed and so its name has entered the geological literature for this kind of volcanic formation. The
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Pedone, M.; Aiuppa, A.; Giudice, G.; Grassa, F.; Francofonte, V.; Bergsson, B.; Ilyinskaya, E. (2014).
4014:"Episodic massive mud eruptions from submarine mud volcanoes examined through topographical signatures"
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1909:
was described by Roman writers as having been covered with gardens and vineyards before its unexpected
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24:
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Solar radiation graph 1958â2008, showing how the radiation is reduced after major volcanic eruptions
1090:, or (in Iceland) mobergs. Very good examples of this type of volcano can be seen in Iceland and in
7809:
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6090:
Swanson, DA (2008). "Hawaiian oral tradition describes 400 years of volcanic activity at KÄ«lauea".
4626:
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4524:"The Volcanic Explosivity Index (VEI): An Estimate of Explosive Magnitude for Historical Volcanism"
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in California is an example of a volcano formed from felsic lava and is actually a large lava dome.
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is an example. Volcanoes are usually not created where two tectonic plates slide past one another.
123:
118:
in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling
20:
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are at the bottom of the oceans, and so most volcanic activity on Earth is submarine, forming new
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7354:
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6385:"Arthur Holmes: Harnessing the Mechanics of Mantle Convection to the Theory of Continental Drift"
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5314:"The Judicious Selection and Preservation of Tuff and Travertine Building Stone in Ancient Rome*"
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2017:
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157:. It suggested that a volcano be defined as 'an opening on a planet or moon's surface from which
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6487:
This is a reference aimed at geologists, but many articles are accessible to non-professionals.
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Sigurdsson, H; Houghton, B; Rymer, H; Stix, J; McNutt, S (2000). "The history of volcanology".
1778:
1742:
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5409:"A message from the 'underground forge of the gods': History and current eruptions at Mt Etna"
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Thomaidis, K; Troll, VR; Deegan, FM; Freda, C; Corsaro, RA; Behncke, B; Rafailidis, S (2021).
5231:
4834:
Castro, J.; Dingwell, D. (2009). "Rapid ascent of rhyolitic magma at Chaitén volcano, Chile".
3611:
1852:, ground inflation, or unusually high levels of carbon dioxide or sulfur dioxide are present.
1802:
Volcanoes vary greatly in their level of activity, with individual volcanic systems having an
1465:. Intermediate magmas are characteristic of stratovolcanoes. They are most commonly formed at
6626:
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5748:
Mouginis-Mark, Peter J. (October 2016). "Geomorphology and volcanology of Maat Mons, Venus".
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in Alaska, which, before its September 2006 eruption, had not erupted since before 8000 BCE.
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258:(meaning "one life") and such volcanoes are often grouped together in a geographical region.
52:
32:
4664:
4089:
One or more of the preceding sentences incorporates text from a publication now in the
1307:. A large number of minor and trace gases are also found in volcanic emissions, for example
830:
Stratovolcanoes (composite volcanoes) are tall conical mountains composed of lava flows and
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Cryptodomes are formed when viscous lava is forced upward causing the surface to bulge. The
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4806:"Mount Edgecumbe volcanic field changes from 'dormant' to 'active' -- what does that mean?"
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evacuation of 1991. This evacuation is believed to have saved 20,000 lives. In the case of
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2020:. Whether a volcano is truly extinct is often difficult to determine. Since "supervolcano"
1972:
in the Pacific Ocean (although some volcanoes at the eastern end of the chain are active),
1938:
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that may include other features that form when magma comes into contact with water such as
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McGee, Kenneth A.; Doukas, Michael P.; Kessler, Richard; Gerlach, Terrence M. (May 1997).
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are not always at the top of a mountain or hill and may be filled with lakes such as with
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Courthouse News Service. By Candace Cheung. August 17, 2022. Downloaded August 17, 2022.
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by an effusive phase that rebuilds the central dome. Vulcanian eruptions are named after
1659:(VEI), which ranges from 0 for Hawaiian-type eruptions to 8 for supervolcanic eruptions.
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Submarine volcanoes are common features of the ocean floor. Volcanic activity during the
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emplaced by such eruptions are the only volcanic product with volumes rivaling those of
889:. Big bombs can measure more than 1.2 meters (4 ft) across and weigh several tons.
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2678:, four of which are vast shield volcanoes far bigger than any on Earth. They include
2666:, "Mount Olympus"), located on the planet Mars, is the tallest known mountain in the
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Bindschadler, D.L. (1995). "Magellan: A new view of Venus' geology and geophysics".
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4943:"Eruptive History of Earth's Largest Quaternary caldera (Toba, Indonesia) Clarified"
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Mazzini, Adriano; Etiope, Giuseppe (May 2017). "Mud volcanism: An updated review".
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and the concepts of the underworld are aligned to volcanoes in that Greek culture.
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2013:
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and highly fluid lava flows but relatively little tephra. They are named after the
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3376:(2nd ed.). Cambridge, UK: Cambridge University Press. pp. 380â384, 390.
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work had brought together the concepts of radioactive generation of heat, Earth's
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Ash thrown into the air by eruptions can present a hazard to aircraft, especially
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air), which often causes volcanic vents to form steep pillars on the ocean floor.
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2698:. These volcanoes have been extinct for many millions of years, but the European
2583:
2558:, a 2021 review found 77 deaths due to eruptions since 1536 but none since 1987.
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2436:
2377:. Chemical reactions of sulfate aerosols in the stratosphere can also damage the
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1997:
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1547:, are very rare; indeed, very few have been erupted at Earth's surface since the
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Lopes, R. M.; Mitchell, K. L.; Williams, D. A.; Mitri, G.; Gregg, T. K. (2009).
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was recently established to protect this unusual landscape, which lies north of
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volcanoes except when the mud volcano is actually a vent of an igneous volcano.
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Video of lava agitating and bubbling in the volcanic eruption of Litli-HrĂștur (
280:
diverge from one another as hot mantle rock creeps upwards beneath the thinned
6512:
5502:
5477:
5287:"Home Away from Home: Ancestral Pueblo Fieldhouses in the Northern Rio Grande"
4941:
Chesner, C.A.; Rose, J.A.; Deino, W.I.; Drake, R.; Westgate, A. (March 1991).
4805:
4413:
4388:
2076:
International Association of Volcanology and Chemistry of the Earth's Interior
1707:
1668:. The range of observed eruption styles is expressed from historical examples.
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may travel hundreds of kilometers before it falls back to ground as a fallout
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2009:
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have still shown signs that they may be likely to erupt again in the future.
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If the erupted magma contains <52% and >45% silica, the lava is called
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1937:, thought to be extinct until activity resumed in 1995 (turning its capital
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LiveScience. By Stephanie Pappas. June 15, 2011. Downloaded July 25, 2022.
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Jackson, M. D.; Marra, F.; Hay, R. L.; Cawood, C.; Winkler, E. M. (2005).
5124:. trans. JĂłhann Hannesson, PĂ©tur Karlsson. ReykjavĂk: Almenna bĂłkafĂ©lagiĂ°.
5050:"The significance of volcanic eruption strength and frequency for climate"
3941:
3117:
724:
518:) and gases (mainly steam and magmatic gases) can develop anywhere on the
137:
Large eruptions can affect atmospheric temperature as ash and droplets of
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Dolan, S.G.; Cates, K.M.; Conrad, C.N.; Copeland, S.R. (March 14, 2019).
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2768:
2754:, and is apparently most common on the moons of the outer planets of the
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2001:
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Mafic lava flows show two varieties of surface texture: ʻAʻa (pronounced
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5169:"Supervolcano eruption â in Sumatra â deforested India 73,000 years ago"
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1957:
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is home to 20 Holocene volcanoes, 3 of which have erupted in last 100yrs
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Volcanoes in human history: the far-reaching effects of major eruptions
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3173:"What is a Volcano? How planetary volcanism has changed our definition"
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1082:. They are made up of lava plateaus capping extensive pillow lavas and
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National Geographic. By Maya Wei-Haas. 2015. Downloaded June 24, 2022.
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eruptions from dry explosive eruption, of, as it turned out, a basalt
2940:(1571â1630) believed volcanoes were ducts for Earth's tears. In 1650,
2717:
is the most volcanically active object in the Solar System because of
2600:
volcano erupts a plume 330 km (205 mi) above the surface of
925:
Supervolcano eruptions, while the most dangerous type, are very rare;
527:
426:), and failed rifts are characterized by volcanoes that erupt unusual
126:, 3,000 kilometers (1,900 mi) deep within Earth. This results in
7599:
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5478:"Scientists' views about lay perceptions of volcanic hazard and risk"
5076:
4655:
MartĂ Molist, Joan (September 6, 2017). "Assessing Volcanic Hazard".
3073:
Rampino, M R; Self, S; Stothers, R B (May 1988). "Volcanic Winters".
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in northern Europe, may also owe its origins to a volcanic eruption.
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5813:"Exceptionally bright eruption on Io rivals largest in solar system"
3864:"Origin of mystery humming noises heard around the world, uncovered"
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1731:. They are driven by the resulting rapid buildup of pressure in the
292:
of the rock, causing volcanism and creating new oceanic crust. Most
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7092:
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Living under the shadow: The cultural impacts of volcanic eruptions
5147:"Impacts of Volcanic Gases on Climate, the Environment, and People"
4742:
Wired. August 15, 2015. By Erik Klimetti. Downloaded July 24, 2022.
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3048: â System for uniquely identifying volcanic features on Earth
2721:
interaction with Jupiter. It is covered with volcanoes that erupt
2423:
1901:
volcano has a repose/recharge period of around 700,000 years, and
19:
This article is about the geological feature. For other uses, see
7574:
7559:
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6994:
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5139:
This article incorporates text from this source, which is in the
4614:
Venzke, E. (compiler) (December 19, 2022). Venzke, Edward (ed.).
4573:
Venzke, E. (compiler) (December 19, 2022). Venzke, Edward (ed.).
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is thought to have taken place around 70,000 years ago after the
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1977:
1918:
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Lava can be broadly classified into four different compositions:
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Pinatubo: Why the Biggest Volcanic Eruption Wasn't the Deadliest
5097:
4776:"How is a volcano defined as being active, dormant, or extinct?"
3328:
2592:
2525:
Tourism associated with volcanoes is also a worldwide industry.
598:
Volcanic fissure vents are flat, linear fractures through which
102:, has volcanoes caused by divergent tectonic plates whereas the
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Large volume volcanic eruptions in the Basin and Range Province
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5787:"Glacial, volcanic and fluvial activity on Mars: latest images"
5556:
2006). "The constitution and structure of the lunar interior".
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2908:
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proposed eruptions were caused by a great wind. By 65 CE,
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339:
145:. Historically, large volcanic eruptions have been followed by
119:
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About to blow: Are we ready for the next volcanic catastrophe?
4344:
4294:
4231:
3304:
2907:
proposed combustion as the cause, an idea also adopted by the
1601:
1576:
flows as they move away from the vent, but never the reverse.
1258:, the name of magma when it emerges and flows over the surface
284:. The decrease of pressure in the rising mantle rock leads to
75:
below the surface. The process that forms volcanoes is called
7153:
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7133:
7004:
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which allowed in one event differentiation of the concurrent
2718:
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2199:
2193:
2005:
1500:
Mafic lavas occur in a wide range of settings. These include
1483:
1364:
1229:
882:
699:
Cinder cones result from eruptions of mostly small pieces of
391:
are thought to have been formed in such a manner, as has the
331:
161:, as defined for that body, and/or magmatic gas is erupted.'
158:
56:
7339:
5357:
Rapa NuiâEaster Island: Cultural and Historical Perspectives
5011:
4690:"Difference Between an Active, Dormant, and Extinct Volcano"
4457:
4421:
4356:
3390:
3118:"A Morphological and Spatial Analysis of Volcanoes on Venus"
2888:. The earliest known such example is a neolithic goddess at
2813:
also found evidence of a methane-spewing cryovolcano on the
2016:
in Scotland is located atop an extinct volcano, which forms
1453:
If the erupted magma contains 52â63% silica, the lava is of
1106:
in northern British Columbia. Tuya Butte was the first such
403:. However, the mantle plume hypothesis has been questioned.
7649:
7422:
7173:
7087:
6793:
6766:
6746:
6650:
6210:
6011:
5926:
4970:
10.1130/0091-7613(1991)019<0200:EHOESL>2.3.CO;2
4445:
4433:
3916:"Tuyas, flat-topped volcanoes in northern British Columbia"
3870:
3673:
3654:
3497:
2881:
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2473:
created global climate anomalies that became known as the "
2385:(HCl) and hydrogen fluoride (HF) can fall to the ground as
2365:
Volcanic gases can reach the stratosphere, where they form
1879:
In an article justifying the re-classification of Alaska's
1623:
1606:
1431:
1255:
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915:
712:
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being part of the North American plate currently above the
60:
6571:
5235:. Jelle Zeilinga de Boer, Donald Theodore Sanders (2002).
4720:
usgs.gov. Updated July 24, 2022. Downloaded July 24, 2022.
3471:
Wood, C.A. (1979). "Cindercones on Earth, Moon and Mars".
3170:
1883:
volcano from "dormant" to "active", volcanologists at the
7138:
6908:
6324:
5406:
5144:
4754:"Volcanic Hazards & Prediction of Volcanic Eruptions"
4167:
2936:"fermentation" as a heat source within Earth, Astronomer
2747:
2428:
2427:
Comparison of major United States prehistoric eruptions (
2318:(steam-generated eruptions), explosive eruptions of high-
1287:
is typically the most abundant volcanic gas, followed by
514:. Vents that issue volcanic material (including lava and
5886:"Cassini Finds an Atmosphere on Saturn's Moon Enceladus"
5712:
5284:
4469:
4368:
4332:
3734:
3287:"Do monogenetic volcanoes threaten the southwestern US?"
2447:
on Sumatra island in Indonesia. This may have created a
2389:. Excessive fluoride salts from eruptions have poisoned
2074:
The Decade Volcanoes are 16 volcanoes identified by the
753:
165:
6554:
U.S. Federal Emergency Management Agency Volcano advice
5979:""Super Earth" May Really Be New Planet Type: Super-Io"
4733:
How We Tell if a Volcano Is Active, Dormant, or Extinct
2976:
built upon his other knowledge with his studies on the
1989:
1098:, which is one of the several tuyas in the area of the
5844:"Chapter 44 - Cryovolcanism in the Outer Solar System"
2565:
1727:
are characterized by interaction of rising magma with
1004:
Satellite images of the January 15, 2022, eruption of
39:(Alaska) during its eruptive phase on January 24, 2006
6277:
Williams, Micheal (November 2007). "Hearts of fire".
5311:
5057:
Quarterly Journal of the Royal Meteorological Society
5047:
4940:
4613:
4572:
2791:
fountains of frozen particles erupting from Enceladus
654:, but can also form independently, as in the case of
6124:
5338:
5100:"Volcanic Eruption Of 1600 Caused Global Disruption"
5048:
Miles, M.G.; Grainger, R.G.; Highwood, E.J. (2004).
3893:(Fourth ed.). Oxford: Oxford University Press.
2995:
2876:
Many ancient accounts ascribe volcanic eruptions to
1651:
Schematic of volcano injection of aerosols and gases
1537:
Some erupted magmas contain â€45% silica and produce
1283:
can vary considerably from one volcano to the next.
342:
content, so it often does not reach the surface but
230:
According to the theory of plate tectonics, Earth's
5781:
5779:
5098:University of California â Davis (April 25, 2008).
3072:
2849:
2518:flow from Earth's interior. These can be tapped as
2080:
International Decade for Natural Disaster Reduction
1867:, India, is classified as a dormant volcano by the
1086:. These volcanoes are also called table mountains,
164:This article mainly covers volcanoes on Earth. See
6411:
6206:
6204:
6202:
6200:
6198:
6196:
5475:
4728:
4726:
4210:
3692:Francis, Peter (1983). "Giant Volcanic Calderas".
3657:Yellowstone Volcano Observatory. August 21, 2015.
3054: â Institution that monitors volcano activity
2346:. These can pose a hazard to humans. Earthquakes,
2082:(the 1990s). The 16 current Decade Volcanoes are:
623:, a shield volcano whose name means "broad shield"
545:(or ice volcanoes), particularly on some moons of
16:Rupture in a planet's crust where material escapes
6127:Geografiska Annaler: Series A, Physical Geography
5305:
5268:
4012:Kioka, Arata; Ashi, Juichiro (October 28, 2015).
3861:
1389:and are erupted as domes or short, stubby flows.
873:that produce great quantities of ash, as well as
594:, has a chain of volcanic cones along its length.
7786:
5776:
5402:
5400:
5398:
5396:
4768:
2750:on the frigid surface. This process is known as
2326:), effusive eruptions of low-silica lava (e.g.,
485:The most common perception of a volcano is of a
6409:
6302:. Wellington, New Zealand: Government Printer.
6193:
5850:, Amsterdam: Academic Press, pp. 763â776,
5278:
4723:
4522:Newhall, Christopher G.; Self, Stephen (1982).
4487:
4275:
4117:
4115:
3789:
3610:Lockwood, John P.; Hazlett, Richard W. (2010).
3609:
3374:Principles of igneous and metamorphic petrology
3208:Mind over Magma: The Story of Igneous Petrology
3116:Hahn, Rebecca M.; Byrne, Paul K. (April 2023).
82:On Earth, volcanoes are most often found where
6612:
6331:Journal of Volcanology and Geothermal Research
6092:Journal of Volcanology and Geothermal Research
5848:The Encyclopedia of Volcanoes (Second Edition)
5369:
5367:
5365:
4833:
1636:
506:rather than a summit crater while others have
311:
7355:
7221:
6598:
6179:. Walnut Creek: Left Coast. pp. 203â24.
6167:
5747:
5393:
4885:
4883:
4881:
4829:
4827:
4451:
4439:
4427:
4362:
4350:
4314:"Exploring the Valley of Ten Thousand Smokes"
4300:
4280:. Berlin: Springer-Verlag. pp. 210â211.
4276:Fisher, Richard V.; Schmincke, H.-U. (1984).
4237:
3966:
3889:Allaby, Michael, ed. (July 4, 2013). "Tuya".
3876:
3679:
3408:
3371:
3075:Annual Review of Earth and Planetary Sciences
3037: â Research to predict volcanic activity
1020:and by the discoloration of water because of
261:
6161:
5677:
5260:. Princeton University Press. Archived from
5207:
5116:
4991:"Volcanic Alert Levels of Various Countries"
4654:
4389:"The off-crust origin of granite batholiths"
4112:
4108:(11th ed.). Cambridge University Press.
3449:David S.G. Thomas and Andrew Goudie (eds.),
3372:Philpotts, Anthony R.; Ague, Jay J. (2009).
723:on larger volcanoes, or occur on their own.
350:. Typical examples are the volcanoes in the
6414:Volcanoes in the Sea: The Geology of Hawaii
6058:"The volcano in Athabascan oral narratives"
5362:
4934:
4896:Contribribtions to Mineralogy and Petrology
4657:Oxford Handbook Topics in Physical Sciences
4521:
4498:
4496:
3419:
3417:
3349:Plates vs. Plumes: A Geological Controversy
3285:Hsu-Buffalo, Charlotte (November 4, 2021).
3284:
1487:(because it contains higher percentages of
522:and may give rise to smaller cones such as
383:are volcanic areas thought to be formed by
7362:
7348:
7228:
7214:
6605:
6591:
6470:
6432:
6410:Macdonald, Gordon; Abbott, Agatin (1970).
5634:. Oregon State University. January 4, 2012
5608:. Oregon State University. January 4, 2012
5476:Donovan, A; Eiser, JR; Sparks, RS (2014).
4878:
4824:
4745:
4607:
4208:
3891:A dictionary of geology and earth sciences
3532:
3443:
1855:
1848:whenever subterranean indicators, such as
927:four are known from the last million years
166:§ Volcanoes on other celestial bodies
6433:Marti, Joan & Ernst, Gerald. (2005).
6360:
6350:
6253:
5948:"Hydrocarbon volcano discovered on Titan"
5501:
5329:
4925:
4915:
4782:. Oregon State University. Archived from
4502:
4475:
4463:
4412:
4374:
4338:
4318:Katmai National Park and Preserve, Alaska
4193:
4077:
4075:
4037:
4011:
3996:
3764:
3594:
3396:
3334:
3322:
3310:
3257:
3115:
1295:. Other principal volcanic gases include
592:major world climate alteration of 1783â84
482:, typically a volcanic cone or mountain.
6538:) is being considered for deletion. See
6456:. Australian National University Press.
6299:Report on the Tarawera volcanic district
6276:
5841:
5654:"A Lunar Mystery: The Gruithuisen Domes"
4493:
4255:Lassen Volcanic National Park California
4094:
3575:Journal of Geophysical Research: Planets
3414:
3122:Journal of Geophysical Research: Planets
3020:List of volcanic eruptions by death toll
2914:(1602â1680), who witnessed eruptions of
2654:
2591:
2528:
2491:Volcanogenic massive sulfide ore deposit
2422:
2276:
2268:
2041:
1956:
1859:
1753:
1646:
1600:
1367:contains a high percentage (>63%) of
1336:
1200:
1188:
1181:. The picture shows overflows of a main
1172:
1148:
1078:Subglacial volcanoes develop underneath
999:
757:
687:
615:
578:
451:
434:. Examples include the volcanoes of the
221:
149:which have caused catastrophic famines.
31:
6089:
5983:National Geographic web site daily news
5976:
5255:
4687:
4121:
3913:
3822:
3691:
3526:
3346:
3340:
2797:. The ejecta may be composed of water,
2674:There are several extinct volcanoes on
2620:(the darker patches seen on the Moon),
2264:
2028:
1067:
192:of Italy whose name in turn comes from
7787:
6451:
6295:
5977:Jaggard, Victoria (February 5, 2010).
5559:Reviews in Mineralogy and Geochemistry
5373:
4752:Nelson, Stephen A. (October 4, 2016).
4751:
4620:Volcanoes of the World (Version 5.0.1)
4616:"How many active volcanoes are there?"
4579:Volcanoes of the World (Version 5.0.1)
4566:
4386:
4072:
3888:
3862:Ashley Strickland (January 10, 2020).
3838:Volcanoes of the World (version 4.9.1)
3831:"How many active volcanoes are there?"
3828:
3805:Volcanoes of the World (version 4.9.1)
3795:
3030:Maritime impacts of volcanic eruptions
2926:and published his view of an Earth in
1792:database of volcanic eruptions in the
1566:
1556:
1543:lava. Ultramafic flows, also known as
1197:) eruption 2023. View from an airplane
983:
933:and ash released into the atmosphere.
406:
7343:
7209:
6586:
6235:
6175:. In Grattan, J; Torrence, R (eds.).
5916:
4688:Pariona, Amber (September 19, 2019).
4665:10.1093/oxfordhb/9780190699420.013.32
3561:
3201:
2504:people used tuff to make most of the
1626:or smaller) are called volcanic ash.
1048:In May and June 2018, a multitude of
1033:are common near these volcanoes, and
798:Layers of lava emitted by the volcano
754:Stratovolcanoes (composite volcanoes)
7743:
6306:from the original on August 29, 2023
6055:
5256:Ă GrĂĄda, Cormac (February 6, 2009).
3914:Mathews, W. H. (September 1, 1947).
3470:
3451:The Dictionary of Physical Geography
3264:. Berlin: Springer. pp. 13â20.
2292:, during an eruption in October 2005
1888:USGS still widely employs the term.
1749:
1221:can be classified into three types:
1094:. The origin of the term comes from
975:
885:. Large pieces of tephra are called
792:Layers of ash emitted by the volcano
441:
112:Wells Gray-Clearwater volcanic field
7767:
5819:. November 13, 2002. Archived from
5374:Kiprop, Joseph (January 18, 2019).
4711:Kilauea eruption confined to crater
4209:Casq, R.A.F.; Wright, J.V. (1987).
3095:10.1146/annurev.ea.16.050188.000445
2566:Volcanoes on other celestial bodies
2362:often accompany volcanic activity.
2247:Multi-Component Gas Analyzer System
2239:Deep Earth Carbon Degassing Project
2037:
1583:flows typically consist largely of
1434:. Volcanic gases may remain in the
1217:The material that is expelled in a
1144:
605:
334:. This magma tends to be extremely
200:. The study of volcanoes is called
13:
7235:
6471:SigurĂ°sson, Haraldur, ed. (2015).
6402:
6215:. Academic Press. pp. 15â37.
5856:10.1016/b978-0-12-385938-9.00044-4
5842:Geissler, Paul (January 1, 2015),
5208:O'Hanlon, Larry (March 14, 2005).
3015:List of extraterrestrial volcanoes
2572:List of extraterrestrial volcanoes
2401:and thus provide a deep source of
2393:in Iceland on multiple occasions.
2150:, Democratic Republic of the Congo
905:List of largest volcanic eruptions
211:
14:
7841:
6542:to help reach a consensus. âș
6492:
5846:, in Sigurdsson, Haraldur (ed.),
5149:. United States Geological Survey
3714:10.1038/scientificamerican0683-60
3661:from the original on July 3, 2017
1962:Capulin Volcano National Monument
1268:
892:
735:are examples of cinder cones. In
668:1980 eruption of Mount St. Helens
141:obscure the Sun and cool Earth's
7766:
7754:
7742:
7731:
7730:
7501:
6377:
6352:10.1016/j.jvolgeores.2022.107552
6318:
6289:
6270:
6229:
6168:Chester, DK; Duncan, AM (2007).
6118:
6112:10.1016/j.jvolgeores.2008.01.033
6083:
6048:
6005:
5970:
5940:
5917:Smith, Yvette (March 15, 2012).
5910:
5894:. March 16, 2005. Archived from
5878:
5835:
5331:10.1111/j.1475-4754.2005.00215.x
5134:
4387:Castro, Antonio (January 2014).
4217:. Unwin Hyman Inc. p. 528.
4082:
3647:"Questions About Supervolcanoes"
3453:(Oxford: Blackwell, 2000), 301.
2998:
2850:History of volcano understanding
1719:eruption of Mount Vesuvius in 79
1279:The concentrations of different
1252:S, depending on the temperature)
1236:, and a sulfur compound (either
1129:
1035:some support peculiar ecosystems
568:
7256:Prediction of volcanic activity
5805:
5741:
5715:Journal of Geophysical Research
5706:
5671:
5646:
5620:
5594:
5548:
5529:
5510:
5469:
5450:
5376:"Why Is Volcanic Soil Fertile?"
5249:
5224:
5201:
5179:
5161:
5128:
5110:
5091:
5041:
5005:
4983:
4798:
4704:
4681:
4648:
4532:Journal of Geophysical Research
4515:
4380:
4306:
4269:
4243:
4202:
4161:
4046:
4005:
3989:10.1016/j.earscirev.2017.03.001
3960:
3907:
3882:
3855:
3728:
3685:
3639:
3630:
3603:
3491:
3464:
3365:
3258:Schmincke, Hans-Ulrich (2003).
3035:Prediction of volcanic activity
2958:1886 eruption of Mount Tarawera
2880:causes, such as the actions of
2259:prediction of volcanic activity
1970:HawaiianâEmperor seamount chain
1913:, which destroyed the towns of
1209:stratovolcano off the coast of
767:(vertical scale is exaggerated)
673:
541:Other types of volcano include
6475:(2 ed.). Academic Press.
6437:. Cambridge University Press.
6418:. University of Hawaii Press.
6065:Alaska Journal of Anthropology
5954:. June 8, 2005. Archived from
5482:Journal of Applied Volcanology
5187:"When humans faced extinction"
4509:University of California Press
3613:Volcanoes: Global Perspectives
3278:
3251:
3226:
3195:
3164:
3109:
3066:
3041:Timeline of volcanism on Earth
1784:As of December 2022, the
1112:Tuya Mountains Provincial Park
956:(both western United States);
661:
1:
7369:
7324:Quaternary volcanic eruptions
6527:
6473:The Encyclopedia of Volcanoes
6435:Volcanoes and the Environment
4635:10.5479/si.GVP.VOTW5-2022.5.0
4594:10.5479/si.GVP.VOTW5-2022.5.0
4503:Heiken, G. & Wohletz, K.
3059:
2922:, then visited the crater of
1717:, who chronicled the Plinian
1412:Valley of Ten Thousand Smokes
1326:
639:
344:cools and solidifies at depth
6518:Resources in other libraries
5770:10.1016/j.icarus.2016.05.022
5210:"Yellowstone's Super Sister"
4018:Geophysical Research Letters
3555:10.1016/j.icarus.2011.11.030
3520:10.1016/j.icarus.2007.10.023
3411:, pp. 390â394, 396â397.
3347:Foulger, Gillian R. (2010).
2978:1902 eruption of Mount Pelée
2742:, the smallest of Jupiter's
2395:Explosive volcanic eruptions
1620:when it flows to the surface
1414:, formed by the eruption of
914:-forming eruption. Ash flow
362:, or the eastern islands of
184:is derived from the name of
175:
7:
6034:10.2138/gselements.19.2.104
5987:National Geographic Society
4488:Fisher & Schmincke 1984
3921:American Journal of Science
3473:Lunar and Planetary Science
2991:
2484:
2397:release the greenhouse gas
2375:Russian famine of 1601â1603
2312:types of volcanic eruptions
1825:
1687:. Their primary product is
1643:Types of volcanic eruptions
1637:Types of volcanic eruptions
1371:, the lava is described as
1228:, a mixture made mostly of
1122:near the boundary with the
881:are material for dangerous
719:. Cinder cones may form as
709:monogenetic volcanic fields
369:
312:Convergent plate boundaries
188:, a volcanic island in the
10:
7846:
7314:Largest volcanic eruptions
7299:Extraterrestrial volcanoes
7261:Volcanic explosivity index
7191:
6572:"Global Volcanism Program"
5919:"Enceladus, Saturn's Moon"
5351:November 14, 2022, at the
5237:Princeton University Press
5122:Hekla, A Notorious Volcano
4917:10.1007/s00410-023-02075-z
4810:Alaska Volcano Observatory
3177:AGU Fall Meeting Abstracts
3025:List of volcanic landforms
2856:Volcanology § History
2853:
2635:has a surface that is 90%
2569:
2488:
2303:
2299:
2063:
1952:
1885:Alaska Volcano Observatory
1869:Geological Survey of India
1837:
1657:Volcanic Explosivity Index
1640:
1605:Light-microscope image of
1594:
1446:fractional crystallization
1330:
1272:
1133:
1071:
993:
987:
902:
896:
823:
677:
643:
609:
572:
445:
410:
373:
315:
294:divergent plate boundaries
265:
262:Divergent plate boundaries
238:in the underlying ductile
215:
18:
7726:
7668:
7510:
7499:
7377:
7289:
7243:
7187:
7106:
7068:
6987:
6892:
6844:
6722:
6691:
6633:
6624:
6513:Resources in your library
6242:Annals of Medical History
6213:Encyclopedia of volcanoes
5503:10.1186/s13617-014-0015-5
5258:"Famine: A Short History"
4452:Philpotts & Ague 2009
4440:Philpotts & Ague 2009
4428:Philpotts & Ague 2009
4414:10.1016/j.gsf.2013.06.006
4363:Philpotts & Ague 2009
4351:Philpotts & Ague 2009
4301:Philpotts & Ague 2009
4238:Philpotts & Ague 2009
4060:. Smithsonian Institution
3877:Philpotts & Ague 2009
3680:Philpotts & Ague 2009
3409:Philpotts & Ague 2009
2538:, and the application of
2314:and associated activity:
2310:There are many different
2249:instruments to measure CO
1933:volcano on the island of
1905:of around 380,000 years.
1833:
1725:Phreatomagmatic eruptions
1590:
1319:, organic compounds, and
1052:signals were detected by
1006:Hunga Tonga-Hunga Haʻapai
946:Yellowstone National Park
940:. Known examples include
834:in alternate layers, the
747:of over 60 cinder cones.
510:features such as massive
25:Volcanic (disambiguation)
7405:Cryptovolcanic structure
7329:Volcanic eruption deaths
7309:Large volcanic eruptions
6559:August 27, 2021, at the
6540:templates for discussion
5923:Image of the Day Gallery
5541:August 17, 2022, at the
4627:Global Volcanism Program
4586:Global Volcanism Program
4058:Global Volcanism Program
3836:Global Volcanism Program
3829:Venzke, E., ed. (2013).
3803:Global Volcanism Program
3796:Venzke, E., ed. (2013).
3651:Volcanic Hazards Program
3202:Young, Davis A. (2003).
2892:. The Ancient Greek god
2842:in 2009, suggested that
2838:, which was detected by
2051:Petropavlovsk-Kamchatsky
2004:, and many volcanoes in
1790:Global Volcanism Program
1456:intermediate composition
846:in the Philippines, and
763:Cross-section through a
21:Volcano (disambiguation)
7686:Eruptions by death toll
6576:Smithsonian Institution
5344:Richards, Colin. 2016.
4624:Smithsonian Institution
4583:Smithsonian Institution
4553:10.1029/JC087iC02p01231
4320:. National Park Service
4257:. National Park Service
4105:EncyclopĂŠdia Britannica
4054:"El Salvador Volcanoes"
3842:Smithsonian Institution
3809:Smithsonian Institution
3798:"Holocene Volcano List"
3337:, pp. 18, 106â107.
3325:, pp. 18, 113â126.
2733:rock, and as a result,
2284:concentration over the
2243:Deep Carbon Observatory
2241:, an initiative of the
2202:, Canary Islands, Spain
2174:Santa Maria/Santiaguito
1856:Dormant and reactivated
1786:Smithsonian Institution
1691:. They are named after
1568:[paËËho.eËho.e]
1491:(Mg) and iron (Fe)) or
864:of stratovolcanoes has
7266:Volcanic Seven Summits
6452:Ollier, Cliff (1969).
5522:July 19, 2022, at the
5462:July 25, 2022, at the
5118:Thorarinsson, Sigurdur
4738:July 25, 2022, at the
4716:July 17, 2022, at the
4195:10.5194/se-5-1209-2014
3616:. Wiley. p. 552.
3425:"Anatomy of a Volcano"
3313:, pp. 17â18, 276.
2948:in his writings about
2671:
2609:
2500:for construction. The
2432:
2344:volcanic gas emissions
2293:
2274:
2061:
2049:volcano towering over
1965:
1872:
1781:
1779:House of the Centenary
1745:; no magma is erupted.
1652:
1614:
1352:
1214:
1198:
1186:
1177:PÄhoehoe lava flow on
1170:
1008:
821:
715:explosion craters and
696:
624:
595:
470:
227:
172:for more information.
40:
6296:Hutton, F.W. (1887).
5958:on September 19, 2007
5817:W.M. Keck Observatory
5791:European Space Agency
5680:Reviews of Geophysics
5580:10.2138/rmg.2006.60.3
4562:on December 13, 2013.
3969:Earth-Science Reviews
3948:on September 29, 2011
3942:10.2475/ajs.245.9.560
3429:National Park Service
2658:
2595:
2576:Volcanism on the Moon
2529:Safety considerations
2475:Year Without a Summer
2469:The 1815 eruption of
2449:population bottleneck
2426:
2407:biogeochemical cycles
2280:
2272:
2045:
1960:
1863:
1757:
1650:
1604:
1528:; and as continental
1467:convergent boundaries
1344:eruption in 1994, in
1340:
1204:
1192:
1176:
1160:
1003:
761:
691:
619:
582:
464:
446:Further information:
225:
196:, the god of fire in
53:planetary-mass object
35:
7194:Geographical feature
7030:Volcanic crater lake
6281:. No. 11â2007.
6238:"Athanasius Kircher"
5264:on January 12, 2016.
5175:. November 24, 2009.
4393:Geoscience Frontiers
4213:Volcanic Successions
4122:Schmidt, R. (1981).
4039:10.1002/2015GL065713
3214:on November 12, 2015
3142:10.1029/2023je007753
2831:A 2010 study of the
2767:spacecraft observed
2381:, and acids such as
2373:may have caused the
2286:Sierra Negra Volcano
2265:Volcanoes and humans
2168:Kagoshima Prefecture
2094:(grouped together),
2029:Volcanic-alert level
1163:San Miguel (volcano)
1068:Subglacial volcanoes
590:, the source of the
360:Japanese Archipelago
352:Pacific Ring of Fire
338:because of its high
204:, sometimes spelled
124:coreâmantle boundary
104:Pacific Ring of Fire
47:is a rupture in the
7820:Volcanoes by status
7281:Volcano observatory
6343:2022JVGR..42707552B
6139:2015GeAnA..97..137T
6104:2008JVGR..176..427S
6026:2023Eleme..19..104Z
5993:on February 9, 2010
5793:. February 25, 2005
5762:2016Icar..277..433M
5727:1995JGR...10011755R
5692:1995RvGeo..33S.459B
5572:2006RvMG...60..221W
5494:2014JApV....3...15D
5457:Volcano Safety Tips
5428:2021GeolT..37..141T
5189:. BBC. June 9, 2003
5069:2004QJRMS.130.2361M
5027:2007Geo....35.1115A
4962:1991Geo....19..200C
4927:20.500.11850/646219
4908:2023CoMP..178...96C
4856:10.1038/nature08458
4848:2009Natur.461..780C
4786:on January 12, 2013
4756:. Tulane University
4545:1982JGR....87.1231N
4466:, pp. 131â132.
4405:2014GeoFr...5...63C
4186:2014SolE....5.1209P
4030:2015GeoRL..42.8406K
3981:2017ESRv..168...81M
3934:1947AmJS..245..560M
3757:10.1038/nature10706
3749:2012Natur.482...77D
3706:1983SciAm.248f..60F
3694:Scientific American
3587:2013JGRE..118..615L
3547:2012Icar..218...88B
3512:2008Icar..194..487M
3485:1979LPI....10.1370W
3399:, pp. 108â110.
3351:. Wiley-Blackwell.
3189:2009AGUFM.V21H..08L
3134:2023JGRE..12807753H
3087:1988AREPS..16...73R
3052:Volcano observatory
2954:Lazzaro Spallanzani
2929:Mundus Subterraneus
2789:probe photographed
2771:(ice volcanoes) on
2342:(debris flows) and
2220:Nagasaki Prefecture
2055:Kamchatka Peninsula
1996:in New Mexico, US,
1947:Fourpeaked Mountain
1804:eruption recurrence
1666:explosive eruptions
1165:degassing in 2022.
984:Submarine volcanoes
942:Yellowstone Caldera
871:explosive eruptions
774:Large magma chamber
407:Continental rifting
401:Yellowstone hotspot
397:Yellowstone Caldera
318:Convergent boundary
7815:Volcanic landforms
7800:Geological hazards
7681:Lists of volcanoes
7468:Subglacial volcano
7443:Pyroclastic shield
6236:Major, RH (1939).
6147:10.1111/geoa.12099
5658:Moon: NASA Science
5220:on March 14, 2005.
5063:(602): 2361â2376.
4140:10.1007/BF01822152
3596:10.1002/jgre.20060
2950:igneous intrusions
2912:Athanasius Kircher
2905:Seneca the Younger
2823:Kuiper Belt Object
2783:, and in 2005 the
2672:
2610:
2588:Volcanism on Venus
2433:
2316:phreatic eruptions
2294:
2275:
2212:, Papua New Guinea
2066:Lists of volcanoes
2062:
1966:
1873:
1782:
1739:Phreatic eruptions
1677:Hawaiian volcanoes
1653:
1615:
1424:Earth's atmosphere
1353:
1215:
1199:
1187:
1171:
1074:Subglacial volcano
1031:Hydrothermal vents
1009:
996:Subaqueous volcano
875:pyroclastic surges
862:explosive eruption
822:
697:
630:effusive eruptions
625:
596:
489:mountain, spewing
471:
448:Types of volcanoes
288:expansion and the
268:Divergent boundary
228:
100:Mid-Atlantic Ridge
59:, that allows hot
41:
7782:
7781:
7535:Basaltic andesite
7473:Submarine volcano
7337:
7336:
7203:
7202:
7114:Artificial island
7020:Submarine volcano
6929:Continental shelf
6896:coastal landforms
6692:Continental plain
6627:List of landforms
6499:Library resources
6482:978-0-12-385938-9
6463:978-0-7081-0532-0
6444:978-0-521-59254-3
6425:978-0-870-22495-9
6056:Fast, PA (2008).
5898:on March 10, 2007
5865:978-0-12-385938-9
5823:on August 6, 2017
5735:10.1029/95JE00147
5700:10.1029/95RG00281
5436:10.1111/gto.12362
5214:Discovery Channel
5035:10.1130/G24149A.1
5021:(12): 1115â1118.
4993:. Volcanolive.com
4842:(7265): 780â783.
4674:978-0-19-069942-0
4575:"Database Search"
4539:(C2): 1231â1238.
4353:, pp. 15â16.
4278:Pyroclastic rocks
4224:978-0-04-552022-0
4024:(20): 8406â8414.
3623:978-1-4051-6250-0
3358:978-1-4051-6148-0
2648:, in the form of
2580:Volcanism on Mars
2383:hydrogen chloride
2336:pyroclastic flows
2290:Galapagos Islands
1964:in New Mexico, US
1929:the long-dormant
1911:eruption of 79 CE
1850:earthquake swarms
1750:Volcanic activity
1715:Pliny the Younger
1629:Tephra and other
1526:continental crust
1400:Pyroclastic flows
1323:metal chlorides.
1305:hydrogen fluoride
1301:hydrogen chloride
1219:volcanic eruption
1158:
1118:and south of the
990:Submarine volcano
976:Caldera volcanoes
970:Ngorongoro Crater
968:, Indonesia; and
462:
442:Volcanic features
436:East African Rift
393:Snake River Plain
376:Hotspot (geology)
356:Cascade Volcanoes
128:hotspot volcanism
108:East African Rift
71:to escape from a
37:Augustine Volcano
7837:
7770:
7769:
7758:
7746:
7745:
7734:
7733:
7691:Decade Volcanoes
7669:Lists and groups
7660:Pyroclastic flow
7655:Pyroclastic fall
7505:
7438:Pyroclastic cone
7364:
7357:
7350:
7341:
7340:
7251:Decade Volcanoes
7230:
7223:
7216:
7207:
7206:
7149:Land reclamation
7045:Volcanic plateau
6607:
6600:
6593:
6584:
6583:
6579:
6486:
6467:
6448:
6429:
6417:
6396:
6395:
6393:
6391:
6381:
6375:
6374:
6364:
6354:
6322:
6316:
6315:
6313:
6311:
6293:
6287:
6286:
6283:Korean Air Lines
6274:
6268:
6267:
6257:
6233:
6227:
6226:
6208:
6191:
6190:
6174:
6165:
6159:
6158:
6122:
6116:
6115:
6087:
6081:
6080:
6078:
6076:
6062:
6052:
6046:
6045:
6009:
6003:
6002:
6000:
5998:
5989:. Archived from
5974:
5968:
5967:
5965:
5963:
5944:
5938:
5937:
5935:
5933:
5914:
5908:
5907:
5905:
5903:
5882:
5876:
5875:
5874:
5872:
5839:
5833:
5832:
5830:
5828:
5809:
5803:
5802:
5800:
5798:
5783:
5774:
5773:
5745:
5739:
5738:
5710:
5704:
5703:
5675:
5669:
5668:
5666:
5664:
5650:
5644:
5643:
5641:
5639:
5628:"Sinuous Rilles"
5624:
5618:
5617:
5615:
5613:
5598:
5592:
5591:
5552:
5546:
5533:
5527:
5514:
5508:
5507:
5505:
5473:
5467:
5454:
5448:
5447:
5413:
5404:
5391:
5390:
5388:
5386:
5371:
5360:
5342:
5336:
5335:
5333:
5309:
5303:
5302:
5300:
5298:
5282:
5276:
5272:
5266:
5265:
5253:
5247:
5228:
5222:
5221:
5216:. Archived from
5205:
5199:
5198:
5196:
5194:
5183:
5177:
5176:
5165:
5159:
5158:
5156:
5154:
5138:
5137:
5132:
5126:
5125:
5114:
5108:
5107:
5095:
5089:
5088:
5077:10.1256/qj.03.60
5054:
5045:
5039:
5038:
5009:
5003:
5002:
5000:
4998:
4987:
4981:
4980:
4978:
4976:
4947:
4938:
4932:
4931:
4929:
4919:
4887:
4876:
4875:
4831:
4822:
4821:
4819:
4817:
4802:
4796:
4795:
4793:
4791:
4772:
4766:
4765:
4763:
4761:
4749:
4743:
4730:
4721:
4708:
4702:
4701:
4699:
4697:
4692:. WorldAtlas.com
4685:
4679:
4678:
4652:
4646:
4645:
4643:
4641:
4611:
4605:
4604:
4602:
4600:
4570:
4564:
4563:
4561:
4555:. Archived from
4528:
4519:
4513:
4512:
4500:
4491:
4485:
4479:
4473:
4467:
4461:
4455:
4449:
4443:
4437:
4431:
4425:
4419:
4418:
4416:
4384:
4378:
4372:
4366:
4360:
4354:
4348:
4342:
4336:
4330:
4329:
4327:
4325:
4310:
4304:
4303:, p. 73-77.
4298:
4292:
4291:
4273:
4267:
4266:
4264:
4262:
4247:
4241:
4240:, p. 70-72.
4235:
4229:
4228:
4216:
4206:
4200:
4199:
4197:
4180:(2): 1209â1221.
4165:
4159:
4158:
4156:
4154:
4119:
4110:
4109:
4088:
4086:
4085:
4079:
4070:
4069:
4067:
4065:
4050:
4044:
4043:
4041:
4009:
4003:
4002:
4000:
3964:
3958:
3957:
3955:
3953:
3944:. Archived from
3911:
3905:
3904:
3886:
3880:
3874:
3868:
3867:
3859:
3853:
3852:
3850:
3848:
3826:
3820:
3819:
3817:
3815:
3793:
3787:
3786:
3768:
3732:
3726:
3725:
3689:
3683:
3677:
3671:
3670:
3668:
3666:
3643:
3637:
3634:
3628:
3627:
3607:
3601:
3600:
3598:
3565:
3559:
3558:
3530:
3524:
3523:
3495:
3489:
3488:
3468:
3462:
3447:
3441:
3440:
3438:
3436:
3421:
3412:
3406:
3400:
3394:
3388:
3387:
3369:
3363:
3362:
3344:
3338:
3332:
3326:
3320:
3314:
3308:
3302:
3301:
3299:
3297:
3282:
3276:
3275:
3255:
3249:
3248:
3246:
3244:
3230:
3224:
3223:
3221:
3219:
3210:. Archived from
3199:
3193:
3192:
3168:
3162:
3161:
3113:
3107:
3106:
3070:
3008:
3006:Volcanoes portal
3003:
3002:
2520:geothermal power
2495:Geothermal power
2464:mass extinctions
2457:Permian-Triassic
2332:sector collapses
2148:Mount Nyiragongo
2102:Nevado de Colima
2070:Decade Volcanoes
2038:Decade volcanoes
2014:Edinburgh Castle
1865:Narcondam Island
1570:
1560:
1510:Hawaiian Islands
1506:Shield volcanoes
1502:mid-ocean ridges
1377:. Felsic lavas (
1297:hydrogen sulfide
1246:hydrogen sulfide
1159:
1145:Erupted material
1092:British Columbia
960:in New Zealand;
938:geologic mapping
860:produced by the
652:Mount St. Helens
606:Shield volcanoes
586:fissure vent in
532:Volcanic craters
480:
479:
478:volcanic edifice
469:), Iceland, 2023
463:
389:Hawaiian Islands
274:mid-ocean ridges
147:volcanic winters
132:Hawaiian hotspot
7845:
7844:
7840:
7839:
7838:
7836:
7835:
7834:
7810:Plate tectonics
7785:
7784:
7783:
7778:
7722:
7664:
7630:Tephriphonolite
7506:
7497:
7493:Harmonic tremor
7395:Complex volcano
7373:
7368:
7338:
7333:
7285:
7271:Volcanic winter
7239:
7234:
7204:
7199:
7196:
7183:
7119:Artificial reef
7102:
7064:
7040:Volcanic island
7025:Volcanic crater
6983:
6979:Volcanic island
6959:Mid-ocean ridge
6895:
6888:
6840:
6718:
6687:
6629:
6620:
6611:
6570:
6561:Wayback Machine
6543:
6524:
6523:
6522:
6507:
6506:
6502:
6495:
6490:
6483:
6464:
6445:
6426:
6405:
6403:Further reading
6400:
6399:
6389:
6387:
6383:
6382:
6378:
6323:
6319:
6309:
6307:
6294:
6290:
6275:
6271:
6234:
6230:
6223:
6209:
6194:
6187:
6172:
6166:
6162:
6123:
6119:
6088:
6084:
6074:
6072:
6060:
6053:
6049:
6010:
6006:
5996:
5994:
5975:
5971:
5961:
5959:
5946:
5945:
5941:
5931:
5929:
5915:
5911:
5901:
5899:
5884:
5883:
5879:
5870:
5868:
5866:
5840:
5836:
5826:
5824:
5811:
5810:
5806:
5796:
5794:
5785:
5784:
5777:
5746:
5742:
5711:
5707:
5686:(S1): 459â467.
5676:
5672:
5662:
5660:
5652:
5651:
5647:
5637:
5635:
5626:
5625:
5621:
5611:
5609:
5600:
5599:
5595:
5553:
5549:
5543:Wayback Machine
5534:
5530:
5524:Wayback Machine
5515:
5511:
5474:
5470:
5464:Wayback Machine
5455:
5451:
5411:
5405:
5394:
5384:
5382:
5372:
5363:
5353:Wayback Machine
5343:
5339:
5310:
5306:
5296:
5294:
5283:
5279:
5273:
5269:
5254:
5250:
5229:
5225:
5206:
5202:
5192:
5190:
5185:
5184:
5180:
5167:
5166:
5162:
5152:
5150:
5135:
5133:
5129:
5115:
5111:
5096:
5092:
5052:
5046:
5042:
5010:
5006:
4996:
4994:
4989:
4988:
4984:
4974:
4972:
4945:
4939:
4935:
4888:
4879:
4832:
4825:
4815:
4813:
4804:
4803:
4799:
4789:
4787:
4774:
4773:
4769:
4759:
4757:
4750:
4746:
4740:Wayback Machine
4731:
4724:
4718:Wayback Machine
4709:
4705:
4695:
4693:
4686:
4682:
4675:
4659:. Vol. 1.
4653:
4649:
4639:
4637:
4612:
4608:
4598:
4596:
4571:
4567:
4559:
4526:
4520:
4516:
4501:
4494:
4486:
4482:
4478:, pp. 132.
4474:
4470:
4462:
4458:
4450:
4446:
4438:
4434:
4426:
4422:
4385:
4381:
4373:
4369:
4361:
4357:
4349:
4345:
4337:
4333:
4323:
4321:
4312:
4311:
4307:
4299:
4295:
4288:
4274:
4270:
4260:
4258:
4249:
4248:
4244:
4236:
4232:
4225:
4207:
4203:
4166:
4162:
4152:
4150:
4120:
4113:
4098:, ed. (1911). "
4083:
4081:
4080:
4073:
4063:
4061:
4052:
4051:
4047:
4010:
4006:
3965:
3961:
3951:
3949:
3912:
3908:
3901:
3887:
3883:
3875:
3871:
3860:
3856:
3846:
3844:
3827:
3823:
3813:
3811:
3794:
3790:
3743:(7383): 77â80.
3733:
3729:
3690:
3686:
3678:
3674:
3664:
3662:
3645:
3644:
3640:
3635:
3631:
3624:
3608:
3604:
3566:
3562:
3531:
3527:
3496:
3492:
3469:
3465:
3448:
3444:
3434:
3432:
3423:
3422:
3415:
3407:
3403:
3395:
3391:
3384:
3370:
3366:
3359:
3345:
3341:
3333:
3329:
3321:
3317:
3309:
3305:
3295:
3293:
3283:
3279:
3272:
3256:
3252:
3242:
3240:
3232:
3231:
3227:
3217:
3215:
3200:
3196:
3169:
3165:
3114:
3110:
3071:
3067:
3062:
3057:
3004:
2997:
2994:
2962:phreatomagmatic
2938:Johannes Kepler
2858:
2852:
2811:CassiniâHuygens
2799:liquid nitrogen
2786:CassiniâHuygens
2590:
2584:Volcanism on Io
2568:
2540:risk management
2531:
2497:
2487:
2437:volcanic winter
2308:
2306:Volcanic hazard
2302:
2267:
2256:
2252:
2235:
2118:, Sicily, Italy
2072:
2064:Main articles:
2040:
2031:
1998:Zuidwal volcano
1955:
1931:SoufriĂšre Hills
1894:Chaitén volcano
1881:Mount Edgecumbe
1858:
1842:
1836:
1828:
1752:
1645:
1639:
1631:volcaniclastics
1599:
1593:
1558:[ËÊaÊa]
1471:tectonic plates
1428:eruption column
1363:If the erupted
1335:
1329:
1313:carbon monoxide
1277:
1271:
1251:
1243:
1149:
1147:
1138:
1132:
1124:Yukon Territory
1076:
1070:
998:
992:
986:
978:
907:
901:
895:
828:
820:
819:
756:
686:
678:Main articles:
676:
664:
648:
642:
614:
608:
577:
571:
477:
476:
452:
450:
444:
415:
409:
378:
372:
320:
314:
290:partial melting
278:tectonic plates
270:
264:
220:
218:Plate tectonics
214:
212:Plate tectonics
198:Roman mythology
190:Aeolian Islands
178:
130:, of which the
116:Rio Grande rift
96:mid-ocean ridge
84:tectonic plates
28:
17:
12:
11:
5:
7843:
7833:
7832:
7827:
7825:Volcanic rocks
7822:
7817:
7812:
7807:
7802:
7797:
7780:
7779:
7777:
7776:
7764:
7752:
7740:
7727:
7724:
7723:
7721:
7720:
7719:
7718:
7713:
7706:Volcanic field
7703:
7698:
7693:
7688:
7683:
7678:
7672:
7670:
7666:
7665:
7663:
7662:
7657:
7652:
7647:
7642:
7637:
7635:Trachyandesite
7632:
7627:
7622:
7617:
7612:
7607:
7602:
7597:
7592:
7587:
7582:
7577:
7572:
7567:
7562:
7557:
7552:
7547:
7542:
7537:
7532:
7527:
7522:
7516:
7514:
7512:Volcanic rocks
7508:
7507:
7500:
7498:
7496:
7495:
7490:
7485:
7480:
7475:
7470:
7465:
7460:
7455:
7453:Shield volcano
7450:
7445:
7440:
7435:
7433:Parasitic cone
7430:
7425:
7420:
7415:
7412:
7407:
7402:
7397:
7392:
7387:
7381:
7379:
7375:
7374:
7367:
7366:
7359:
7352:
7344:
7335:
7334:
7332:
7331:
7326:
7321:
7319:Earth timeline
7316:
7311:
7306:
7301:
7295:
7293:
7287:
7286:
7284:
7283:
7278:
7276:Volcano Number
7273:
7268:
7263:
7258:
7253:
7247:
7245:
7241:
7240:
7237:Volcano topics
7233:
7232:
7225:
7218:
7210:
7201:
7200:
7198:
7197:
7188:
7185:
7184:
7182:
7181:
7176:
7171:
7166:
7161:
7156:
7151:
7146:
7141:
7136:
7131:
7126:
7121:
7116:
7110:
7108:
7104:
7103:
7101:
7100:
7095:
7090:
7085:
7080:
7074:
7072:
7066:
7065:
7063:
7062:
7057:
7052:
7047:
7042:
7037:
7032:
7027:
7022:
7017:
7012:
7007:
7002:
6997:
6991:
6989:
6985:
6984:
6982:
6981:
6976:
6971:
6966:
6964:Oceanic trench
6961:
6956:
6951:
6946:
6941:
6936:
6931:
6926:
6921:
6916:
6911:
6906:
6900:
6898:
6890:
6889:
6887:
6886:
6881:
6876:
6871:
6866:
6861:
6856:
6850:
6848:
6842:
6841:
6839:
6838:
6833:
6828:
6823:
6818:
6817:
6816:
6811:
6801:
6796:
6791:
6786:
6781:
6776:
6775:
6774:
6764:
6759:
6754:
6749:
6744:
6739:
6734:
6728:
6726:
6720:
6719:
6717:
6716:
6711:
6706:
6701:
6695:
6693:
6689:
6688:
6686:
6685:
6680:
6675:
6670:
6665:
6664:
6663:
6653:
6648:
6643:
6637:
6635:
6631:
6630:
6625:
6622:
6621:
6610:
6609:
6602:
6595:
6587:
6581:
6580:
6568:
6563:
6551:
6521:
6520:
6515:
6509:
6508:
6497:
6496:
6494:
6493:External links
6491:
6489:
6488:
6481:
6468:
6462:
6449:
6443:
6430:
6424:
6406:
6404:
6401:
6398:
6397:
6376:
6317:
6288:
6269:
6248:(2): 105â120.
6228:
6221:
6192:
6185:
6160:
6117:
6082:
6047:
6004:
5969:
5939:
5909:
5877:
5864:
5834:
5804:
5775:
5740:
5705:
5670:
5645:
5619:
5593:
5566:(1): 221â364.
5547:
5528:
5509:
5468:
5449:
5392:
5380:WorldAtlas.com
5361:
5337:
5324:(3): 485â510.
5304:
5293:. 19â21132: 96
5277:
5267:
5248:
5223:
5200:
5178:
5160:
5127:
5109:
5090:
5040:
5004:
4982:
4956:(3): 200â203.
4933:
4877:
4823:
4797:
4767:
4744:
4722:
4703:
4680:
4673:
4647:
4606:
4565:
4514:
4511:. p. 246.
4492:
4480:
4476:Schmincke 2003
4468:
4464:Schmincke 2003
4456:
4444:
4432:
4430:, p. 377.
4420:
4379:
4377:, p. 143.
4375:Schmincke 2003
4367:
4365:, p. 378.
4355:
4343:
4341:, p. 229.
4339:Schmincke 2003
4331:
4305:
4293:
4286:
4268:
4242:
4230:
4223:
4201:
4160:
4111:
4096:Chisholm, Hugh
4071:
4045:
4004:
3959:
3928:(9): 560â570.
3906:
3899:
3881:
3869:
3854:
3821:
3788:
3727:
3684:
3672:
3638:
3629:
3622:
3602:
3560:
3525:
3490:
3463:
3442:
3431:. July 5, 2023
3413:
3401:
3397:Schmincke 2003
3389:
3382:
3364:
3357:
3339:
3335:Schmincke 2003
3327:
3323:Schmincke 2003
3315:
3311:Schmincke 2003
3303:
3277:
3270:
3250:
3238:Dictionary.com
3225:
3194:
3163:
3108:
3064:
3063:
3061:
3058:
3056:
3055:
3049:
3046:Volcano Number
3043:
3038:
3032:
3027:
3022:
3017:
3011:
3010:
3009:
2993:
2990:
2980:, and by 1928
2974:Alfred Lacroix
2942:René Descartes
2854:Main article:
2851:
2848:
2744:Galilean moons
2727:sulfur dioxide
2688:Hecates Tholus
2567:
2564:
2552:Mount Pinatubo
2530:
2527:
2486:
2483:
2453:End-Ordovician
2399:carbon dioxide
2304:Main article:
2301:
2298:
2282:Sulfur dioxide
2266:
2263:
2254:
2250:
2234:
2233:
2223:
2213:
2203:
2197:
2187:
2177:
2171:
2161:
2151:
2145:
2135:
2129:
2119:
2113:
2099:
2084:
2057:, Far Eastern
2039:
2036:
2030:
2027:
1954:
1951:
1857:
1854:
1840:Active volcano
1838:Main article:
1835:
1832:
1827:
1824:
1763:Mount Vesuvius
1751:
1748:
1747:
1746:
1736:
1722:
1711:
1704:
1696:
1680:
1673:lava fountains
1669:
1641:Main article:
1638:
1635:
1595:Main article:
1592:
1589:
1553:
1552:
1534:
1533:
1497:
1496:
1479:
1450:
1449:
1440:
1439:
1395:
1394:
1331:Main article:
1328:
1325:
1293:sulfur dioxide
1289:carbon dioxide
1281:volcanic gases
1273:Main article:
1270:
1269:Volcanic gases
1267:
1266:
1265:
1259:
1253:
1249:
1241:
1238:sulfur dioxide
1234:carbon dioxide
1226:Volcanic gases
1195:Fagradalsfjall
1193:Litli-HrĂștur (
1146:
1143:
1134:Main article:
1131:
1128:
1120:Jennings River
1072:Main article:
1069:
1066:
1022:volcanic gases
988:Main article:
985:
982:
977:
974:
950:Valles Caldera
897:Main article:
894:
893:Supervolcanoes
891:
887:volcanic bombs
848:Mount Vesuvius
824:Main article:
818:
817:
814:
811:
808:
805:
804:Parasitic cone
802:
799:
796:
793:
790:
787:
784:
781:
780:Conduit (pipe)
778:
775:
771:
770:
755:
752:
745:volcanic field
727:in Mexico and
693:Izalco volcano
675:
672:
663:
660:
644:Main article:
641:
638:
612:Shield volcano
610:Main article:
607:
604:
573:Main article:
570:
567:
526:on a flank of
493:and poisonous
467:Fagradalsfjall
443:
440:
411:Main article:
408:
405:
374:Main article:
371:
368:
354:, such as the
316:Main article:
313:
310:
266:Main article:
263:
260:
216:Main article:
213:
210:
177:
174:
98:, such as the
15:
9:
6:
4:
3:
2:
7842:
7831:
7828:
7826:
7823:
7821:
7818:
7816:
7813:
7811:
7808:
7806:
7803:
7801:
7798:
7796:
7793:
7792:
7790:
7775:
7774:
7765:
7763:
7762:
7757:
7753:
7751:
7750:
7741:
7739:
7738:
7729:
7728:
7725:
7717:
7714:
7712:
7709:
7708:
7707:
7704:
7702:
7701:Volcanic belt
7699:
7697:
7694:
7692:
7689:
7687:
7684:
7682:
7679:
7677:
7674:
7673:
7671:
7667:
7661:
7658:
7656:
7653:
7651:
7648:
7646:
7643:
7641:
7638:
7636:
7633:
7631:
7628:
7626:
7623:
7621:
7618:
7616:
7613:
7611:
7608:
7606:
7605:Phonotephrite
7603:
7601:
7598:
7596:
7593:
7591:
7588:
7586:
7583:
7581:
7578:
7576:
7573:
7571:
7568:
7566:
7563:
7561:
7558:
7556:
7553:
7551:
7548:
7546:
7543:
7541:
7538:
7536:
7533:
7531:
7528:
7526:
7523:
7521:
7518:
7517:
7515:
7513:
7509:
7504:
7494:
7491:
7489:
7488:Volcanic cone
7486:
7484:
7481:
7479:
7476:
7474:
7471:
7469:
7466:
7464:
7463:Stratovolcano
7461:
7459:
7458:Somma volcano
7456:
7454:
7451:
7449:
7448:Rootless cone
7446:
7444:
7441:
7439:
7436:
7434:
7431:
7429:
7426:
7424:
7421:
7419:
7416:
7413:
7411:
7408:
7406:
7403:
7401:
7398:
7396:
7393:
7391:
7388:
7386:
7383:
7382:
7380:
7376:
7372:
7365:
7360:
7358:
7353:
7351:
7346:
7345:
7342:
7330:
7327:
7325:
7322:
7320:
7317:
7315:
7312:
7310:
7307:
7305:
7302:
7300:
7297:
7296:
7294:
7292:
7288:
7282:
7279:
7277:
7274:
7272:
7269:
7267:
7264:
7262:
7259:
7257:
7254:
7252:
7249:
7248:
7246:
7242:
7238:
7231:
7226:
7224:
7219:
7217:
7212:
7211:
7208:
7195:
7190:
7189:
7186:
7180:
7177:
7175:
7172:
7170:
7167:
7165:
7162:
7160:
7157:
7155:
7152:
7150:
7147:
7145:
7142:
7140:
7137:
7135:
7132:
7130:
7127:
7125:
7122:
7120:
7117:
7115:
7112:
7111:
7109:
7105:
7099:
7096:
7094:
7091:
7089:
7086:
7084:
7081:
7079:
7076:
7075:
7073:
7071:
7067:
7061:
7058:
7056:
7053:
7051:
7050:Volcanic plug
7048:
7046:
7043:
7041:
7038:
7036:
7033:
7031:
7028:
7026:
7023:
7021:
7018:
7016:
7013:
7011:
7008:
7006:
7003:
7001:
6998:
6996:
6993:
6992:
6990:
6986:
6980:
6977:
6975:
6972:
6970:
6967:
6965:
6962:
6960:
6957:
6955:
6952:
6950:
6947:
6945:
6942:
6940:
6937:
6935:
6932:
6930:
6927:
6925:
6922:
6920:
6917:
6915:
6912:
6910:
6907:
6905:
6902:
6901:
6899:
6897:
6891:
6885:
6884:Tunnel valley
6882:
6880:
6877:
6875:
6872:
6870:
6867:
6865:
6862:
6860:
6857:
6855:
6852:
6851:
6849:
6847:
6843:
6837:
6834:
6832:
6829:
6827:
6824:
6822:
6819:
6815:
6812:
6810:
6807:
6806:
6805:
6802:
6800:
6797:
6795:
6792:
6790:
6787:
6785:
6782:
6780:
6777:
6773:
6770:
6769:
6768:
6765:
6763:
6760:
6758:
6755:
6753:
6750:
6748:
6745:
6743:
6740:
6738:
6735:
6733:
6730:
6729:
6727:
6725:
6721:
6715:
6712:
6710:
6707:
6705:
6702:
6700:
6697:
6696:
6694:
6690:
6684:
6681:
6679:
6676:
6674:
6671:
6669:
6666:
6662:
6659:
6658:
6657:
6654:
6652:
6649:
6647:
6644:
6642:
6639:
6638:
6636:
6632:
6628:
6623:
6619:
6615:
6608:
6603:
6601:
6596:
6594:
6589:
6588:
6585:
6577:
6573:
6569:
6567:
6566:Volcano World
6564:
6562:
6558:
6555:
6552:
6550:
6546:
6541:
6537:
6536:
6531:
6526:
6525:
6519:
6516:
6514:
6511:
6510:
6505:
6500:
6484:
6478:
6474:
6469:
6465:
6459:
6455:
6450:
6446:
6440:
6436:
6431:
6427:
6421:
6416:
6415:
6408:
6407:
6386:
6380:
6372:
6368:
6363:
6358:
6353:
6348:
6344:
6340:
6336:
6332:
6328:
6321:
6305:
6301:
6300:
6292:
6284:
6280:
6273:
6265:
6261:
6256:
6251:
6247:
6243:
6239:
6232:
6224:
6222:9780123859396
6218:
6214:
6207:
6205:
6203:
6201:
6199:
6197:
6188:
6186:9781315425177
6182:
6178:
6171:
6164:
6156:
6152:
6148:
6144:
6140:
6136:
6133:(1): 137â66.
6132:
6128:
6121:
6113:
6109:
6105:
6101:
6098:(3): 427â31.
6097:
6093:
6086:
6071:(1â2): 131â40
6070:
6066:
6059:
6051:
6043:
6039:
6035:
6031:
6027:
6023:
6020:(2): 104â10.
6019:
6015:
6008:
5992:
5988:
5984:
5980:
5973:
5957:
5953:
5952:New Scientist
5949:
5943:
5928:
5924:
5920:
5913:
5897:
5893:
5892:
5887:
5881:
5867:
5861:
5857:
5853:
5849:
5845:
5838:
5822:
5818:
5814:
5808:
5792:
5788:
5782:
5780:
5771:
5767:
5763:
5759:
5755:
5751:
5744:
5736:
5732:
5728:
5724:
5721:(E6): 11755.
5720:
5716:
5709:
5701:
5697:
5693:
5689:
5685:
5681:
5674:
5659:
5655:
5649:
5633:
5632:Volcano World
5629:
5623:
5607:
5606:Volcano World
5603:
5597:
5589:
5585:
5581:
5577:
5573:
5569:
5565:
5561:
5560:
5551:
5544:
5540:
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5532:
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5504:
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5491:
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5479:
5472:
5465:
5461:
5458:
5453:
5445:
5441:
5437:
5433:
5429:
5425:
5421:
5417:
5416:Geology Today
5410:
5403:
5401:
5399:
5397:
5381:
5377:
5370:
5368:
5366:
5358:
5354:
5350:
5347:
5341:
5332:
5327:
5323:
5319:
5315:
5308:
5297:September 29,
5292:
5288:
5281:
5271:
5263:
5259:
5252:
5246:
5245:0-691-05081-3
5242:
5238:
5234:
5233:
5227:
5219:
5215:
5211:
5204:
5188:
5182:
5174:
5170:
5164:
5148:
5142:
5141:public domain
5131:
5123:
5119:
5113:
5105:
5101:
5094:
5086:
5082:
5078:
5074:
5070:
5066:
5062:
5058:
5051:
5044:
5036:
5032:
5028:
5024:
5020:
5016:
5008:
4992:
4986:
4971:
4967:
4963:
4959:
4955:
4951:
4944:
4937:
4928:
4923:
4918:
4913:
4909:
4905:
4901:
4897:
4893:
4886:
4884:
4882:
4873:
4869:
4865:
4861:
4857:
4853:
4849:
4845:
4841:
4837:
4830:
4828:
4812:. May 9, 2022
4811:
4807:
4801:
4785:
4781:
4780:Volcano World
4777:
4771:
4755:
4748:
4741:
4737:
4734:
4729:
4727:
4719:
4715:
4712:
4707:
4691:
4684:
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4670:
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4658:
4651:
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4632:
4628:
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4595:
4591:
4587:
4584:
4580:
4576:
4569:
4558:
4554:
4550:
4546:
4542:
4538:
4534:
4533:
4525:
4518:
4510:
4506:
4499:
4497:
4490:, p. 89.
4489:
4484:
4477:
4472:
4465:
4460:
4454:, p. 24.
4453:
4448:
4442:, p. 16.
4441:
4436:
4429:
4424:
4415:
4410:
4406:
4402:
4398:
4394:
4390:
4383:
4376:
4371:
4364:
4359:
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4347:
4340:
4335:
4319:
4315:
4309:
4302:
4297:
4289:
4283:
4279:
4272:
4256:
4252:
4246:
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4234:
4226:
4220:
4215:
4214:
4205:
4196:
4191:
4187:
4183:
4179:
4175:
4171:
4164:
4153:September 27,
4149:
4145:
4141:
4137:
4133:
4129:
4125:
4118:
4116:
4107:
4106:
4101:
4097:
4092:
4091:public domain
4078:
4076:
4059:
4055:
4049:
4040:
4035:
4031:
4027:
4023:
4019:
4015:
4008:
3999:
3994:
3990:
3986:
3982:
3978:
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3970:
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3947:
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3927:
3923:
3922:
3917:
3910:
3902:
3900:9780199653065
3896:
3892:
3885:
3879:, p. 66.
3878:
3873:
3865:
3858:
3843:
3839:
3837:
3832:
3825:
3810:
3806:
3804:
3799:
3792:
3784:
3780:
3776:
3772:
3767:
3762:
3758:
3754:
3750:
3746:
3742:
3738:
3731:
3723:
3719:
3715:
3711:
3707:
3703:
3699:
3695:
3688:
3682:, p. 77.
3681:
3676:
3660:
3656:
3652:
3648:
3642:
3633:
3625:
3619:
3615:
3614:
3606:
3597:
3592:
3588:
3584:
3580:
3576:
3572:
3564:
3556:
3552:
3548:
3544:
3540:
3536:
3529:
3521:
3517:
3513:
3509:
3505:
3501:
3494:
3486:
3482:
3479:: 1370â1372.
3478:
3474:
3467:
3460:
3459:0-631-20473-3
3456:
3452:
3446:
3430:
3426:
3420:
3418:
3410:
3405:
3398:
3393:
3385:
3383:9780521880060
3379:
3375:
3368:
3360:
3354:
3350:
3343:
3336:
3331:
3324:
3319:
3312:
3307:
3292:
3288:
3281:
3273:
3271:9783540436508
3267:
3263:
3262:
3254:
3239:
3235:
3234:"Vulcanology"
3229:
3213:
3209:
3205:
3198:
3190:
3186:
3182:
3178:
3174:
3167:
3159:
3155:
3151:
3147:
3143:
3139:
3135:
3131:
3127:
3123:
3119:
3112:
3104:
3100:
3096:
3092:
3088:
3084:
3080:
3076:
3069:
3065:
3053:
3050:
3047:
3044:
3042:
3039:
3036:
3033:
3031:
3028:
3026:
3023:
3021:
3018:
3016:
3013:
3012:
3007:
3001:
2996:
2989:
2987:
2983:
2982:Arthur Holmes
2979:
2975:
2971:
2967:
2963:
2959:
2955:
2951:
2947:
2943:
2939:
2935:
2931:
2930:
2925:
2921:
2917:
2913:
2910:
2906:
2902:
2897:
2895:
2891:
2887:
2883:
2879:
2874:
2872:
2868:
2863:
2857:
2847:
2845:
2844:tidal heating
2841:
2837:
2834:
2829:
2827:
2824:
2820:
2816:
2812:
2808:
2804:
2800:
2796:
2792:
2788:
2787:
2782:
2778:
2774:
2770:
2769:cryovolcanoes
2766:
2765:
2761:In 1989, the
2759:
2757:
2753:
2752:cryovolcanism
2749:
2745:
2741:
2736:
2732:
2728:
2724:
2720:
2716:
2713:
2709:
2705:
2703:
2702:
2697:
2693:
2689:
2685:
2684:Ascraeus Mons
2681:
2677:
2669:
2665:
2661:
2657:
2653:
2651:
2647:
2642:
2638:
2634:
2629:
2627:
2623:
2619:
2615:
2607:
2603:
2599:
2594:
2589:
2585:
2581:
2577:
2573:
2563:
2559:
2557:
2553:
2547:
2543:
2541:
2537:
2526:
2523:
2521:
2515:
2513:
2512:Easter Island
2509:
2508:
2503:
2496:
2492:
2482:
2480:
2476:
2472:
2471:Mount Tambora
2467:
2465:
2462:
2461:Late Devonian
2458:
2454:
2450:
2446:
2442:
2441:supereruption
2438:
2430:
2425:
2421:
2419:
2415:
2410:
2408:
2404:
2400:
2396:
2392:
2388:
2384:
2380:
2376:
2372:
2368:
2367:sulfuric acid
2363:
2361:
2357:
2353:
2349:
2345:
2341:
2337:
2333:
2329:
2325:
2321:
2317:
2313:
2307:
2297:
2291:
2287:
2283:
2279:
2271:
2262:
2260:
2248:
2244:
2240:
2231:
2227:
2224:
2221:
2217:
2214:
2211:
2207:
2204:
2201:
2198:
2196:, Philippines
2195:
2191:
2188:
2185:
2181:
2178:
2175:
2172:
2169:
2165:
2162:
2159:
2155:
2154:Mount Rainier
2152:
2149:
2146:
2143:
2139:
2136:
2133:
2130:
2127:
2123:
2120:
2117:
2114:
2111:
2107:
2103:
2100:
2097:
2093:
2089:
2086:
2085:
2083:
2081:
2077:
2071:
2067:
2060:
2056:
2052:
2048:
2044:
2035:
2026:
2023:
2019:
2015:
2011:
2010:Monte Vulture
2007:
2003:
1999:
1995:
1991:
1987:
1983:
1979:
1975:
1971:
1963:
1959:
1950:
1948:
1944:
1940:
1936:
1932:
1927:
1922:
1920:
1916:
1912:
1908:
1904:
1900:
1895:
1889:
1886:
1882:
1877:
1870:
1866:
1862:
1853:
1851:
1847:
1841:
1831:
1823:
1821:
1817:
1813:
1809:
1805:
1800:
1798:
1795:
1791:
1787:
1780:
1776:
1773:, as seen in
1772:
1768:
1764:
1760:
1756:
1744:
1740:
1737:
1734:
1730:
1726:
1723:
1720:
1716:
1712:
1709:
1705:
1702:
1697:
1694:
1690:
1686:
1681:
1678:
1674:
1670:
1667:
1662:
1661:
1660:
1658:
1649:
1644:
1634:
1632:
1627:
1625:
1621:
1612:
1608:
1603:
1598:
1588:
1586:
1582:
1577:
1574:
1569:
1564:
1559:
1550:
1546:
1542:
1541:
1536:
1535:
1531:
1530:flood basalts
1527:
1523:
1519:
1515:
1511:
1507:
1503:
1499:
1498:
1494:
1490:
1486:
1485:
1480:
1476:
1472:
1468:
1464:
1463:
1458:
1457:
1452:
1451:
1447:
1442:
1441:
1437:
1433:
1429:
1425:
1421:
1417:
1413:
1409:
1405:
1401:
1397:
1396:
1392:
1388:
1385:) are highly
1384:
1380:
1376:
1375:
1370:
1366:
1362:
1361:
1360:
1357:
1351:
1347:
1343:
1342:Mount Rinjani
1339:
1334:
1324:
1322:
1318:
1314:
1310:
1306:
1302:
1298:
1294:
1290:
1286:
1282:
1276:
1263:
1260:
1257:
1254:
1247:
1239:
1235:
1231:
1227:
1224:
1223:
1222:
1220:
1212:
1208:
1203:
1196:
1191:
1184:
1180:
1175:
1168:
1164:
1161:Timelapse of
1142:
1137:
1130:Mud volcanoes
1127:
1125:
1121:
1117:
1113:
1109:
1105:
1101:
1097:
1093:
1089:
1085:
1081:
1075:
1065:
1063:
1059:
1058:oceanographic
1055:
1051:
1046:
1044:
1040:
1036:
1032:
1027:
1023:
1019:
1014:
1007:
1002:
997:
991:
981:
973:
972:in Tanzania.
971:
967:
963:
959:
955:
951:
947:
943:
939:
934:
932:
928:
923:
921:
920:flood basalts
917:
913:
910:catastrophic
906:
900:
890:
888:
884:
880:
876:
872:
867:
863:
859:
855:
853:
849:
845:
844:Mayon Volcano
841:
837:
833:
827:
826:Stratovolcano
815:
812:
809:
806:
803:
800:
797:
794:
791:
788:
785:
782:
779:
776:
773:
772:
768:
766:
765:stratovolcano
760:
751:
748:
746:
742:
738:
734:
730:
729:Sunset Crater
726:
722:
718:
714:
710:
706:
702:
694:
690:
685:
681:
680:volcanic cone
671:
669:
659:
657:
653:
647:
637:
635:
631:
622:
621:SkjaldbreiĂ°ur
618:
613:
603:
601:
593:
589:
585:
581:
576:
569:Fissure vents
566:
564:
560:
559:mud volcanoes
556:
552:
548:
544:
543:cryovolcanoes
539:
537:
533:
529:
525:
521:
517:
513:
509:
505:
500:
496:
492:
488:
483:
481:
468:
449:
439:
437:
433:
429:
425:
420:
419:flood basalts
414:
404:
402:
398:
394:
390:
386:
385:mantle plumes
382:
377:
367:
365:
361:
357:
353:
349:
348:volcanic arcs
345:
341:
337:
333:
329:
324:
319:
309:
307:
303:
302:Black smokers
299:
295:
291:
287:
283:
282:oceanic crust
279:
275:
269:
259:
257:
256:
251:
250:
243:
241:
237:
233:
224:
219:
209:
207:
203:
199:
195:
191:
187:
183:
173:
171:
167:
162:
160:
156:
155:cryovolcanism
150:
148:
144:
140:
139:sulfuric acid
135:
133:
129:
125:
121:
117:
113:
109:
105:
101:
97:
93:
89:
85:
80:
78:
74:
73:magma chamber
70:
66:
62:
58:
54:
50:
46:
38:
34:
30:
26:
22:
7771:
7759:
7747:
7735:
7696:Volcanic arc
7640:Trachybasalt
7478:Supervolcano
7410:Fissure vent
7370:
7236:
7054:
7035:Volcanic dam
6732:Alluvial fan
6533:
6503:
6472:
6453:
6434:
6413:
6390:November 12,
6388:. Retrieved
6379:
6334:
6330:
6320:
6308:. Retrieved
6298:
6291:
6285:. p. 6.
6279:Morning Calm
6278:
6272:
6245:
6241:
6231:
6212:
6176:
6163:
6130:
6126:
6120:
6095:
6091:
6085:
6075:November 11,
6073:. Retrieved
6068:
6064:
6050:
6017:
6013:
6007:
5995:. Retrieved
5991:the original
5982:
5972:
5960:. Retrieved
5956:the original
5951:
5942:
5930:. Retrieved
5922:
5912:
5900:. Retrieved
5896:the original
5889:
5880:
5869:, retrieved
5847:
5837:
5825:. Retrieved
5821:the original
5816:
5807:
5795:. Retrieved
5753:
5749:
5743:
5718:
5714:
5708:
5683:
5679:
5673:
5661:. Retrieved
5657:
5648:
5638:November 17,
5636:. Retrieved
5631:
5622:
5612:November 12,
5610:. Retrieved
5605:
5596:
5563:
5557:
5550:
5531:
5512:
5485:
5481:
5471:
5452:
5422:(4): 141â9.
5419:
5415:
5385:November 27,
5383:. Retrieved
5379:
5359:, pp.150-151
5356:
5340:
5321:
5318:Archaeometry
5317:
5307:
5295:. Retrieved
5290:
5280:
5270:
5262:the original
5251:
5230:
5226:
5218:the original
5213:
5203:
5191:. Retrieved
5181:
5173:ScienceDaily
5172:
5163:
5151:. Retrieved
5130:
5121:
5112:
5104:ScienceDaily
5103:
5093:
5060:
5056:
5043:
5018:
5014:
5007:
4995:. Retrieved
4985:
4973:. Retrieved
4953:
4949:
4936:
4899:
4895:
4839:
4835:
4814:. Retrieved
4809:
4800:
4790:September 5,
4788:. Retrieved
4784:the original
4779:
4770:
4760:September 5,
4758:. Retrieved
4747:
4706:
4696:November 27,
4694:. Retrieved
4683:
4656:
4650:
4638:. Retrieved
4619:
4609:
4597:. Retrieved
4578:
4568:
4557:the original
4536:
4530:
4517:
4505:Volcanic Ash
4504:
4483:
4471:
4459:
4447:
4435:
4423:
4399:(1): 63â75.
4396:
4392:
4382:
4370:
4358:
4346:
4334:
4324:November 27,
4322:. Retrieved
4317:
4308:
4296:
4277:
4271:
4261:November 27,
4259:. Retrieved
4254:
4245:
4233:
4212:
4204:
4177:
4173:
4163:
4151:. Retrieved
4131:
4127:
4103:
4062:. Retrieved
4057:
4048:
4021:
4017:
4007:
3972:
3968:
3962:
3952:November 27,
3950:. Retrieved
3946:the original
3925:
3919:
3909:
3890:
3884:
3872:
3857:
3847:November 18,
3845:. Retrieved
3834:
3824:
3814:November 18,
3812:. Retrieved
3801:
3791:
3740:
3736:
3730:
3700:(6): 60â73.
3697:
3693:
3687:
3675:
3663:. Retrieved
3650:
3641:
3632:
3612:
3605:
3578:
3574:
3563:
3538:
3534:
3528:
3503:
3499:
3493:
3476:
3472:
3466:
3450:
3445:
3433:. Retrieved
3404:
3392:
3373:
3367:
3348:
3342:
3330:
3318:
3306:
3294:. Retrieved
3290:
3280:
3260:
3253:
3243:November 27,
3241:. Retrieved
3237:
3228:
3216:. Retrieved
3212:the original
3207:
3197:
3180:
3176:
3166:
3125:
3121:
3111:
3081:(1): 73â99.
3078:
3074:
3068:
2966:hydrothermal
2946:James Hutton
2927:
2898:
2878:supernatural
2875:
2871:Mount Merapi
2859:
2830:
2810:
2793:, a moon of
2784:
2762:
2760:
2756:Solar System
2706:
2701:Mars Express
2699:
2696:Pavonis Mons
2692:Olympus Mons
2673:
2668:Solar System
2660:Olympus Mons
2630:
2611:
2560:
2548:
2544:
2532:
2524:
2516:
2505:
2498:
2468:
2434:
2414:jet aircraft
2411:
2371:Huaynaputina
2364:
2322:lava (e.g.,
2309:
2295:
2236:
2190:Taal Volcano
2142:Central Java
2138:Mount Merapi
2134:, Hawaii, US
2073:
2032:
1967:
1923:
1890:
1878:
1874:
1845:
1843:
1829:
1819:
1815:
1811:
1807:
1803:
1801:
1783:
1771:Agathodaemon
1743:country rock
1735:groundwater.
1654:
1628:
1616:
1611:thin section
1578:
1554:
1538:
1512:, including
1482:
1460:
1454:
1436:stratosphere
1372:
1358:
1354:
1278:
1275:Volcanic gas
1216:
1183:lava channel
1139:
1077:
1047:
1043:pumice rafts
1010:
979:
935:
924:
908:
899:Supervolcano
866:historically
856:
829:
762:
749:
741:Caja del Rio
705:pyroclastics
698:
674:Cinder cones
665:
649:
626:
597:
575:Fissure vent
540:
484:
475:
472:
432:carbonatites
416:
379:
328:flux melting
321:
271:
253:
247:
244:
229:
205:
181:
179:
163:
151:
136:
81:
65:volcanic ash
44:
42:
29:
7830:Volcanology
7773:WikiProject
7716:polygenetic
7711:monogenetic
7590:Nephelinite
7545:Blairmorite
7520:Agglomerate
7428:Mud volcano
7400:Cryovolcano
7390:Cinder cone
6894:Oceanic and
6634:Mountainous
6528:âč The
5962:October 24,
5756:: 433â441.
5488:(1): 1â14.
4975:January 20,
4640:January 12,
4599:January 12,
4251:"Volcanoes"
4174:Solid Earth
4064:November 8,
3998:10852/61234
3435:November 3,
3218:January 11,
2809:compounds.
2805:, dust, or
2631:The planet
2536:probability
2510:statues in
2429:VEI 7 and 8
2379:ozone layer
2348:hot springs
2216:Mount Unzen
2210:New Britain
2176:, Guatemala
2144:, Indonesia
2018:Castle Rock
2002:Netherlands
1915:Herculaneum
1899:Yellowstone
1733:superheated
1729:groundwater
1708:Mount Pelée
1609:as seen in
1549:Proterozoic
1520:), on both
1404:ignimbrites
1391:Lassen Peak
1317:halocarbons
1285:Water vapor
1167:El Salvador
1136:Mud volcano
1039:chemotrophs
1026:Pillow lava
1018:hydrophones
721:flank vents
684:Cinder cone
662:Cryptodomes
656:Lassen Peak
636:, as well.
530:in Hawaii.
428:alkali lava
395:, with the
255:monogenetic
249:polygenetic
232:lithosphere
206:vulcanology
202:volcanology
170:cryovolcano
143:troposphere
7789:Categories
7615:Rhyodacite
7565:Ignimbrite
7540:Benmoreite
7192:See also:
7107:Artificial
7015:Lava field
6934:Coral reef
6762:Floodplain
6362:2292/59681
6337:: 107552.
6310:August 30,
5871:January 6,
5663:January 6,
5239:. p. 155.
5193:January 5,
4997:August 22,
4287:3540127569
3975:: 81â112.
3766:10220/7536
3665:August 22,
3581:(4): 615.
3506:(2): 487.
3060:References
2952:of magma.
2916:Mount Etna
2901:Anaxagoras
2894:Hephaistos
2890:ĂatalhöyĂŒk
2680:Arsia Mons
2641:Lava flows
2570:See also:
2556:Mount Etna
2489:See also:
2164:Sakurajima
2158:Washington
2128:, Colombia
2116:Mount Etna
2088:Avachinsky
1986:New Mexico
1974:Hohentwiel
1943:ghost town
1935:Montserrat
1685:a gas slug
1624:sand-sized
1545:komatiites
1540:ultramafic
1508:(such the
1438:for years.
1327:Lava flows
1104:Tuya Range
1100:Tuya River
1096:Tuya Butte
1084:palagonite
1054:earthquake
994:See also:
958:Lake TaupĆ
954:New Mexico
903:See also:
854:in Italy.
842:in Japan,
840:Mount Fuji
737:New Mexico
717:tuff rings
640:Lava domes
536:Lake TaupĆ
504:lava domes
323:Subduction
236:convection
114:, and the
92:converging
55:, such as
7805:Volcanism
7795:Volcanoes
7600:Phonolite
7585:Leucitite
7570:Komatiite
7418:Lava dome
7414:Lava cone
7371:Volcanoes
7169:Reservoir
7060:Wall rock
7010:Lava dome
6969:Peninsula
6879:Ice field
6836:Waterfall
6699:Ice sheet
6678:Tableland
6618:landforms
6545:Volcanoes
6454:Volcanoes
6371:248111450
6155:129186824
6042:259423377
5997:March 11,
5588:130734866
5444:238802288
5153:August 9,
4148:128375559
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3261:Volcanism
3204:"Volcano"
3158:257745255
3150:2169-9097
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2920:Stromboli
2833:exoplanet
2815:Saturnian
2764:Voyager 2
2650:ash flows
2646:Maat Mons
2445:Lake Toba
2391:livestock
2387:acid rain
2352:fumaroles
2180:Santorini
2132:Mauna Loa
2096:Kamchatka
2092:Koryaksky
2047:Koryaksky
1693:Stromboli
1581:Rhyolitic
1514:Mauna Loa
1489:magnesium
1462:andesitic
1416:Novarupta
1383:rhyolites
1350:Indonesia
1333:Lava flow
1207:Stromboli
1116:Tuya Lake
1037:based on
962:Lake Toba
852:Stromboli
816:Ash cloud
807:Lava flow
725:ParĂcutin
646:Lava dome
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584:Lakagigar
524:PuÊ»u Ê»ĆÊ»Ć
508:landscape
424:aulacogen
364:Indonesia
286:adiabatic
180:The word
176:Etymology
122:from the
88:diverging
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7737:Category
7645:Trachyte
7620:Rhyolite
7595:Obsidian
7525:Andesite
7129:Building
7093:Sandhill
7083:Dry lake
6988:Volcanic
6974:Seamount
6656:Mountain
6557:Archived
6530:template
6304:Archived
6264:33943407
6014:Elements
5797:July 21,
5539:Archived
5520:Archived
5460:Archived
5349:Archived
5120:(1970).
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4864:19812671
4736:Archived
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3783:22297973
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3291:Futurity
2992:See also
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2886:demigods
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2836:COROT-7b
2731:silicate
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2604:'s moon
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2502:Rapa Nui
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2356:mud pots
2324:rhyolite
2226:Vesuvius
2186:, Greece
2184:Cyclades
2112:, Mexico
2098:, Russia
2022:calderas
2008:such as
1982:Shiprock
1939:Plymouth
1926:Pinatubo
1907:Vesuvius
1826:Erupting
1808:erupting
1794:Holocene
1585:obsidian
1573:Hawaiian
1571:), both
1563:pÄhoehoe
1493:basaltic
1469:between
1321:volatile
1309:hydrogen
1108:landform
1080:ice caps
1013:Holocene
520:landform
512:plateaus
381:Hotspots
370:Hotspots
298:seafloor
7749:Commons
7676:Hotspot
7575:Lapilli
7560:Felsite
7385:Caldera
7070:Aeolian
7055:Volcano
6995:Caldera
6949:Isthmus
6939:Estuary
6919:Channel
6874:Glacier
6846:Glacial
6784:Meander
6752:Channel
6724:Fluvial
6668:Plateau
6532:below (
6504:Volcano
6339:Bibcode
6255:7939598
6135:Bibcode
6100:Bibcode
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5932:July 4,
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5291:Lanl-Ur
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2840:transit
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2781:Neptune
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2602:Jupiter
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2222:, Japan
2170:, Japan
2122:Galeras
2106:Jalisco
2000:in the
1994:Capulin
1978:Germany
1953:Extinct
1941:into a
1919:Pompeii
1820:extinct
1816:dormant
1775:Pompeii
1767:Bacchus
1765:behind
1701:Vulcano
1522:oceanic
1518:Kilauea
1387:viscous
1379:dacites
1062:Mayotte
1050:seismic
966:Sumatra
912:caldera
777:Bedrock
733:Arizona
634:Iceland
588:Iceland
563:igneous
555:Neptune
547:Jupiter
528:KÄ«lauea
497:from a
487:conical
358:or the
336:viscous
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272:At the
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7610:Pumice
7580:Latite
7555:Dacite
7550:Cinder
7530:Basalt
7483:Tossol
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7179:Tunnel
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7098:Tundra
7078:Desert
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6954:Lagoon
6944:Island
6859:Cirque
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6772:island
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2637:basalt
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2479:famine
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2320:silica
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2110:Colima
2059:Russia
1945:) and
1846:active
1834:Active
1812:active
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801:Throat
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6641:Butte
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6367:S2CID
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6151:S2CID
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2719:tidal
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2633:Venus
2626:domes
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2006:Italy
1818:, or
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795:Flank
743:is a
495:gases
332:magma
159:magma
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7650:Tuff
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7174:Road
7088:Dune
6914:Cape
6794:Pond
6767:Lake
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6651:Hill
6646:Flat
6477:ISBN
6458:ISBN
6439:ISBN
6420:ISBN
6392:2023
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6260:PMID
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6181:ISBN
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5999:2010
5964:2010
5934:2014
5927:NASA
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5873:2024
5860:ISBN
5829:2018
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5665:2024
5640:2023
5614:2023
5387:2020
5299:2020
5241:ISBN
5195:2007
5155:2014
4999:2011
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4818:2022
4792:2018
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4698:2020
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4642:2023
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4326:2020
4282:ISBN
4263:2020
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3779:PMID
3771:ISSN
3667:2017
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3245:2020
3220:2016
3181:2009
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2970:dyke
2964:and
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2882:gods
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2777:moon
2775:, a
2729:and
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