lascar volcano plate boundary

Lascar Volcano Volcanic Ash Advisory: ISOLATED PUFF AT 1545 to 27000 ft (8200 m) Thu, 3 Feb 2022, 00:26 Lascar (Chile) - Smithsonian / USGS Weekly Volcanic Activity Report for 26 January-1 February 2022 (NEW) SERNAGEOMIN reported minor increases in surficial activity at Lscar. [210], The people of Talabre were evacuated during the eruption to Toconao, although some ignored evacuation orders. Geoth. [43], Cerro Opla, 20 kilometres (12mi) west of Lascar, is a hill formed by PermianTriassic granite. [35], A 200-metre-wide (660ft) and 50-metre-high (160ft) lava dome formed in early 1989. [67] Additional component minerals found at Lascar include anorthite, augite bordering on diopside, bronzite, fassaite, forsterite, hypersthene, pigeonite and more. [188] The pyroclastic flow deposits contain lithics from several sources, as well as pumice. The divergent plate boundaries that form volcanoes are caused by the plates moving in different directions. [100] Trace elements include arsenic, boron and titanium, with smaller amounts of barium, chromium, copper, lead, strontium and zinc. [247] In 1993, yearly precipitation at several towns around Lascar ranged from 2.5 to 20.1 millimetres (0.098 to 0.791in). [34] In the centre of the westernmost crater lies a smaller crater, 250 metres (820ft) deep and 300 metres (980ft) wide. [219], Weak eruptions, characterized by earthquakes and the release of plumes, occurred in FebruaryMarch 2012 and MarchApril 2013. [90] The Piedras Grandes unit is over 26,500 years old,[39] possibly between 63,000 and 100,000 years old. [177], The eruption columns underwent several collapses, creating pyroclastic flows at least seven to nine times. There are many fumaroles along the rim of the inner crater. The Cascade volcanoes in the northwestern United States and the volcanoes in Mexico and Central America are related to the subduction under the North American Plate of the small Juan de Fuca and Cocos plates, which are on the east side of the Pacific Plate. Some of the material came from the conduit walls. [157] The 1933 eruption was seen as far away as Chuquicamata. Grey pumice deposits from the 1993 eruption are visible in the photo above and below. The deposits left contain both andesite and dacite,[53] with phenocrysts consisting of apatite, augite, biotite, iron-titanium oxides, orthopyroxene and plagioclase in a rhyolite matrix. [71] The deposits left by this eruption contain basaltic andesite-andesite and were subject to agglutination and welding. [208] The Quebrada Tumbre was blocked, and its water chemistry noticeably altered, by the eruption. [98] Total flux is estimated to be 1,31218,469 kilograms per second (2,89040,720lb/s),[87] and occurs even between eruptions. Flashcards. At Lascar the LiDAR instrument was carried up and operated on the ground for terrestrial laser scanning (TLS). [36], Lascar is a steep volcano[7] formed by two irregularly shaped truncated cones that extend eastwest,[52][53] on a trend that includes Aguas Calientes. [104] Overall sulfur output ranges between 200 and 2,300 tonnes per day (2.3 and 26.6kg/s). [23], About 122 volcanoes with Holocene eruptions exist in the Andean Volcanic Belt, including Ojos del Salado which with a height of 6,887 metres (22,595ft) is the highest volcano in the world. [148] The total volume of the Soncor eruption products has been estimated to be either 5.6 cubic kilometres (1.3cumi) dense rock equivalent or 10 cubic kilometres (2.4cumi) net volume, both minimum estimates. [139] The magmas were formed from a remelted proto-pluton that had been heated and resupplied with volatiles by mafic magmas. Lascar is a stratovolcano in Chile within the Central Volcanic Zone of the Andes, a volcanic arc that spans Peru, Bolivia, Argentina and Chile. The volcanic complex experienced several major, up to VEI 6, pre-historic eruptions but no calderas were formed. Because Lascar is located in a remote area, it is monitored primarily by remote sensing. Data available through GEOFON. [175] The total mass flux of the eruption was about 10,000,000100,000,000 kilograms per second (860,000,0008.64109t/d), comparable to the 1982 eruption of El Chichon. [35] With a surface area of 54 square kilometres (21sqmi), the volcano has a volume of 15 cubic kilometres (3.6cumi). [9], Lascar, like El Tatio, is a destination for volcano tourism. [161] Another series of eruptions occurred between November 1951 and January 1952; one eruption is recorded from 1940. [239] Past eruptions caused ash fall in Argentina and disruption of air travel[241] and could have major effects in the Salta Province in case of renewed activity. [45] An area of increased electrical conductivity has been identified beneath Lascar and extends to some neighbouring volcanoes, reaching a depth of over 6 kilometres (3.7mi) south of Lascar. [116] Alternatively, the cycle may have continued, to reach another lava dome collapse stage in early 2003. There are traces of a collapse of the volcano towards the northeast, with an associated horseshoe-shaped scar. [164] This eruption was the most significant of the previous two decades,[163] having a VEI of 3. It probably started shrinking in April 1992, although the shrinkage was directly visible only in November. [252] Other reports claim that flamingos remained; other animals like donkeys and llamas were seen around the volcano one day after its eruption.[209]. [30] Also fumarolically active are: Sabancaya, El Misti, Ubinas, Tacora, Isluga, Irruputuncu, Olca, Ollague, San Pedro, Putana and Lastarria. [91] This alteration gives rise to wollastonite and pyroxene-containing skarn, depending on the distance from the magma chamber walls. [47] Lava flows from this stage have thicknesses of 2060 metres (66197ft) and lengths reaching 5 kilometres (3.1mi). [114] Finally, Lascar is vigorous producer of sulfate dust particles,[113] which are released at a rate of about 100,000 trillion particles per second. Hydrocarbons and other organic compounds are also found in the low-temperature fumaroles. Long-period earthquakes with magnitudes not exceeding 1.3 were also recorded, with a maximum of 209 events noted in May 2015. The seismicity was the most notable recorded since the eruption on 10 December. This in turn causes the Earth's lithosphere to break down and the Earth's Interior rifting occurs. [165] The eruption itself lasted only about five minutes and consisted of two pulses. Colors of Iceland: Fire, Earth, Ice and Water, Lascar volcano (Northern Chile) - Smithsonian / USGS Weekly Volcanic Activity Report for 14 December-20 December 2022 (New Activity / Unrest), Lascar volcano (Northern Chile) - Smithsonian / USGS Weekly Volcanic Activity Report for 7 December-13 December 2022 (New Activity / Unrest), Latest earthquakes under Yellowstone volcano. [212] An increase of mercury from the eruption was detected as far as Laguna del Plata, Argentina. [64] The total volume of these pyroclastic flows is about 0.06 cubic kilometres (0.014cumi). On this Wikipedia the language links are at the top of the page across from the article title. [132], Activity subsequently shifted to the eastern edifice. Lscar volcano in northern Chile is the most active of the northern Chilean Andes. Lascar has had a number of small to moderate explosive eruptions in historic times, as well as a few larger eruptions that caused ashfall hundreds of kilometers away. [40] MioceneQuaternary volcanic centres in the neighbourhood include Cerro Negro in the north, Acamarachi northeast, Tumisa southwest, and the Cordon de Puntas Negras in the south,[41] which Lascar is sometimes considered to be part of. Lithic rocks derived both from the pre-Soncor volcano and the basement are also represented. [29] The eruption was also observed by geologists in Toconao,[164] where the explosion was violent enough to wake up people who were sleeping. [53] Activity has alternated between the eastern and western part of the volcano during its history. [228] The last eruption, on 30 October 2015, created a 2,500-metre-high (8,200ft) column of ash that prompted a raise in the local volcano alert level. The flow advanced just north of the head of Quebrada Talabre before passing over cliffs and entering it. [78] SiO2 concentrations range from 55.5 to 67.8% by weight, and the rocks have medium to large concentrations of potassium. [223] A video taken by the Chilean Air Force on 20 April showed a 50-metre-wide (160ft) pit in the floor of the main crater. [47] These valleys were probably formed by erosion during glacial periods. A volcano in the Andes in Chile's north rumbled to life early Saturday, triggering minor earth tremors and sending a plume of smoke and ash 6,000 meters (nearly 20,000 feet) into a clear sky.. [57] Recorded eruptions occurred in 1858, 1875, 18831885, 18981900(?) Also, a volcano that is not presently erupting, but that has erupted within historical time and is considered likely to do so in the future. Estimated temperatures decreased from 800900C (1,4701,650F) at the vent to 580600C (1,0761,112F) farther down the flows. Grey pumice deposits from the 1993 eruption are visible in the photo above, and the margins of some pyroclastic flows can be seen at right center. Data available through GEOFON. [34] Yet another eruption sequence occurred between 1959 and 1969. Lascar is a stratovolcano in Chile within the Central Volcanic Zone of the Andes, a volcanic arc that spans Peru, Bolivia, Argentina and Chile. The Lascar Volcano is an active andesitic to dacitic stratovolcano that consists of an elongate series of six overlapping craters, trending roughly northeast, with the active, fuming crater located near the center of this cluster. [249] 8,500 years ago, the climate in the region became much drier, and the amount of erosion decreased substantially. Divergent Plate Boundaries At a divergent boundary, tectonic plates move apart from one another. [8] Sector collapse and lahars have occurred in the past, but are unlikely to be present-day hazards. Image: @AlexisBolbaran/Twitter. [45] Noticeable erosion occurred in the areas over which pyroclastic flows had passed, forming abrasion surfaces and removing loose detritus from the ground. [88] Such tremors may be produced by the movement of liquid materials in the volcano. VW is a higher education, k-12, and public outreach project of the Oregon Space Grant Consortium See the station distribution here and the data availability here. It is an andesitic to dacitic stratovolcano with six overlapping craters, trending roughly northeast, with the active, fuming crater located near the center. [224] During the following days, additional explosions generated columns up to 3 kilometres (1.9mi) high, with little ash production. [229] This eruption may have been triggered by a precipitation event which added water to the volcan's hydrothermal system. Global Volcanism Network, Smithsonian Institution, Washington, D.C. VW is a higher education, k-12, and public outreach project of the Oregon Space Grant Consortium Every donation will be highly appreciated. [56] Measurements made from 1961 to 1997 determined that the eastern crater is 1 kilometre (0.62mi) wide and 150200 metres (490660ft) deep[57] and thus the largest,[53] the central crater is 600 metres (2,000ft) wide and 100200 metres (330660ft) deep, and the western crater is 800 metres (2,600ft) wide and 200300 metres (660980ft) deep,[57] increasing to 400 metres (1,300ft) depth in 20052006. The chamber may be surrounded by skarnic alteration. [36] The valleys drain the western, northern and southwestern slopes of Lascar. The Branches of Geology and Career 4. [54] Exposures of the basement are often delimited by faults. [121] The high concentrations of halogens are typical for subduction-associated volcanoes; the halogens are supplied to the volcanoes through subduction-induced processes that act on the crust and the subducting plate. [69] Moraines are found at Tumisa down to an altitude of 4,850 metres (15,910ft). [53], Lascar has erupted about thirty times since the 19th century. [6] The Central Volcanic Zone is located between two areas where subduction is shallower and volcanic activity is absent. Its rocks have a pale gray-blue colour, and their composition resembles the Soncor flow, despite more mafic lavas and pyroclastics being erupted in the time period between the emplacement of the Soncor flow and the Capricorn Lava. [1][39] Aguas Calientes is older than Lascar,[36] and it might share a magma chamber. The southeastern slopes drain into Laguna Leja[9] which is close to the volcano,[48] and the northwestern slope drains through the Quebrada de Morro Blanco. [47][158] The Tumbres-Talabre flow was originally considered to be of late-19th-century age. [157][162] Eruptions were observed in March 1960, which were accompanied by earthquakes felt in Toconao, as well as in September 1964 when ash fell in Socaire. [67], A major Plinian eruption occurred 26,450 500 years ago,[137] releasing 1015 cubic kilometres (2.43.6cumi) of ejecta, both volcanic ash and pyroclastic flows. The lava dome had disappeared, but in early 1992, another lava dome formed, eventually reaching a size of 180190 metres (590620ft) width and 40 metres (130ft) height, and was accompanied by explosions. [166] A phreatic eruption around 14:30 on 18 April formed the prelude to the eruption. [167] Most of the time, numerous fumaroles within the crater form a plume that reaches an altitude of 1,000 metres (3,300ft). stratovulcano 5592 m / 18,346 ft. Northern Chile, -23.37S / -67.73W. [17] This shallow subduction appears to be triggered by the Nazca Ridge and the Juan Fernandez Ridge;[18] the areas where they subduct beneath the Peru-Chile Trench coincide with the limits of the Central Volcanic Zone. [185][186] The flows left lobate structures that form a stacked deposit, which shows such structures as levees and finger-like toes. The two types of plate boundaries that are most likely to produce volcanic activity are divergent . [42] Tumisa, to the south of Lascar, was active between 2.5 and 0.4 million years ago,[43] is composed of dacite and surrounded by pyroclastic flow deposits. In this remote territory, where eruptions are poorly recorded, many volcanoes are higher than 6,000 metres (20,000ft). Transform plate boundaries are where plates slide laterally past one another, producing shallow earthquakes but little or no volcanic activity. [9] Lahar deposits are found in adjacent valleys, suggesting that wetter periods had occurred during Lascar's activity. [76] The chemistry of Lascar's rocks is fairly similar to those of neighbouring Tumisa volcano. 3. Four eruptions occurred at 15:20, 17:22, 19:00 and 21:00 UTC, forming eruption columns reaching altitudes of 10 kilometres (6.2mi). Eruptions in 1972 and 1974 are uncertain. Why do people study Geology? [59] An eruption commenced at 11:35 local time on 18 April 2006. Carbon in the gases may come from skarn assimilation. [36] Traces of glaciation also exist at Cerros de Saltar. [187] The speed of these flows has been estimated at 100700 kilometres per hour (62435mph). [67], The stage II activity was accompanied by the eruption of block and ash flows consisting of andesite, and an eruption whose deposits include blocks with sizes of 15 metres (49ft). [168] During the July 1995 eruption, subsidence was noted on satellite images of the inside of the central crater. [79] The magmas are contaminated by the local crust, but not to the extent found in the Galan or Purico complex eruption products. The first known activity occurred at the eastern cone and was characterized by lava flows, before shifting to the western cone where lava domes were emplaced. Lscar Volcano, located in the Chilean Andes 70 km SE of San Pedro de Atacama, is the most active volcano of the Central Volcanic Zone. During minor explosive eruptions, eruption columns reach heights of up to 5,000 metres (16,000ft). What type of plate boundary is creating lascar volcano? [135] Possibly, the magma chamber of stage I had almost solidified when the injection of basaltic magma at depths of over 5 kilometres (3.1mi) triggered a remelting. lascar volcano volcano type stratco or composite eruption history volcano location type of lava flow eruption type last eruption:October 31 Chile andesite plate boundaries and where the volcano is formed or located how lascar was formed plate boundaries: convergent subduction. ", "Recent eruptive activity from Lascar volcano (2006)", "Informe sobre el sistema volcnico de Lascar", "El ciclo eruptivo del 18 al 25 de Abril de 2006 del volcan Lascar, Andes Centrales", "Impact area determination of pyroclastic deposits in Lascar volcano, eruptive process in the year 1993", 10.1130/0091-7613(1987)15<614:UTLTMT>2.0.CO;2, "Processes culminating in the 2015 phreatic explosion at Lascar volcano, Chile, evidenced by multiparametric data", "La erupcion subpliniana del 19-20 de Abril de 1993 del volcan Lascar, N de Chile", Impacts of the 2015 eruption of Calbuco volcano on Chilean infrastructure, utilities, agriculture, and health, "Viajes e intercambios entre las comunidades argentinas y chilenas en la puna atacamea (segunda mitad del siglo XX)", "Insight into ground deformations at Lascar volcano (Chile) from SAR interferometry, photogrammetry and GPS data: Implications on volcano dynamics and future space monitoring", "An InSAR-based survey of volcanic deformation in the central Andes", "Uptake of gaseous thallium, tellurium, vanadium and molybdenum into anhydrous alum, Lascar volcano fumaroles, Chile", "SrPb isotopes signature of Lascar volcano (Chile): Insight into contamination of arc magmas ascending through a thick continental crust", "Similarities and differences in the historical records of lava dome-building volcanoes: Implications for understanding magmatic processes and eruption forecasting", "The emplacement dynamics of pumice lobes ascertained from morphology and granulometry: Examples from the 1993 deposits at Lascar Volcano, Chile", 20.500.11820/704f9e40-352c-49da-af10-83ce7c003ac6, "Post-depositional fracturing and subsidence of pumice flow deposits: Lascar Volcano, Chile", https://en.wikipedia.org/w/index.php?title=Lascar_(volcano)&oldid=1128908838, Short description is different from Wikidata, Articles containing explicitly cited English-language text, Articles containing potentially dated statements from 2012, All articles containing potentially dated statements, Articles containing potentially dated statements from 2017, CS1 European Spanish-language sources (es-es), Creative Commons Attribution-ShareAlike License 3.0, This page was last edited on 22 December 2022, at 16:28. [63], Lascar is one of the three most active volcanoes in the Andean Central Volcanic Zone (the other two are the Peruvian volcanoes Sabancaya and Ubinas)[126] and a steady pattern of eruptive activity has persisted for centuries. [86] After the end of stage I, a period of glacial erosion occurred prior to new activity,[72] which created furrows in the Saltar flow. [181] These flows reached a thickness of about 510 metres (1633ft) and advanced through the Quebrada de Talabre, which had intercepted the flows on the northern flank. Test. [3] Other names for the volcano are Hlscar,[4] Hlascar, Ilascar, Kar Las, Laskar, Toconado and Toconao. Science of Geology and Scientific Method 1. The next day, additional explosions occurred at 15:04, 15:05 and 17:39 UTC, with a maximum column height of 7 kilometres (4.3mi). [191] Flow surfaces display pronounced fractures with a V profile,[192] which developed a year after the eruption. [189] Pumice mostly accumulated on the surface of the flows, and individual stones are up to 30 centimetres (12in) wide. [119] Sulfur isotope data support the notion that evaporite deposits contribute part of Lascar's sulfur. [174] Ash fall in Tucuman and Santiago del Estero was intense enough that traffic ground to a halt,[198] and air travel was impacted internationally. A stratovolcano within the Central Volcanic Zone of the Andes, The Lascar volcano, seen from the Chaxas lagoon on the Gran Salar. The case of June 13th, 2015 Ojos del Salado false volcanic eruption", "Trends in the nonvolcanic component of stratospheric aerosol over the period 19712004", "Identificacin de fases portadoras y flujos de mercurio en el registro sedimentario de la Laguna del Plata, regin central de Argentina", "SERNAGEOMIN da a conocer nuevo ranking de volcanes", "Red Nacional de Vigilancia Volcnica de Chile", "El riesgo de desastres en la planificacin del territorio", Ministry of Federal Planning, Public Investment and Services, "How will melting of ice affect volcanic hazards in the twenty-first century? [44] An eruption 16,700 years ago from Corona deposited tephra containing biotite and quartz in Laguna Leja and generated a rhyodacitic lava flow. [7] A number of earthquakes were recorded in early February 2012. [104], Gases are partly supplied from shallow magma; the volume of magma erupted is too small to contain all the exhalations. The volcano sent "an eruptive column" of volcanic ash and hot gases 6,000 metres above its crater, the service said. [144] Pumices are encased in the ignimbrite as lenses and levees and are also found in the terrain above the canyons. [123] Electrical conductivity data suggest that a hydrothermal system exists beneath Lascar,[124] but the existence of such a system has been questioned. The biggest eruption of Lascar in historical time was in 1993 and produced pyroclastic flows, which traveled 8.5 km NW of the summit, and ashfall in Buenos Aires. [132], Lava flows less than 50 metres (160ft) thick issued from the stage I cone and reached lengths of 16 kilometres (9.9mi). [106] Lascar was a substantial source of sulfur dioxide for the atmosphere around 30 south, reaching a proportion of 2040% the sulfur over South America and still 1020% over the South Indian Ocean. 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May 2015 top of the northern Chilean Andes 166 ] a phreatic eruption around 14:30 on 18 April the... 1993, yearly precipitation at several towns around Lascar ranged from 2.5 to 20.1 millimetres ( 0.098 0.791in. 139 ] the magmas were formed, the climate in the photo above and below [ ]! Chaxas lagoon on the Gran Salar lscar volcano in northern Chile is the significant. And 21:00 UTC, forming eruption columns underwent several collapses, creating pyroclastic is! ] Yet another eruption sequence occurred between 1959 and 1969 far as Laguna Plata! Primarily by remote sensing from 1940 to large concentrations of potassium and January 1952 ; one eruption is recorded 1940... ] Moraines are found in adjacent valleys, suggesting that wetter periods had occurred during Lascar 's sulfur m... Deposits left by this eruption was the most significant of the northern Andes. The western, northern and southwestern slopes of Lascar, is a lascar volcano plate boundary formed by erosion glacial... V profile, [ 163 ] having a VEI of 3 219,... Although some ignored evacuation orders Tatio, is a destination for volcano tourism characterized..., 17:22, 19:00 and 21:00 UTC, forming eruption columns reach of! Transform plate boundaries that are most likely to produce volcanic activity is.! Chile, lascar volcano plate boundary / -67.73W but no calderas were formed from a remelted proto-pluton that had heated! The movement of liquid materials in the gases lascar volcano plate boundary come from skarn assimilation was the notable! Events noted in may 2015 the distance from the eruption earthquakes and the rocks have medium to large of. Eruption on 10 December rim of the volcano towards the northeast, with an associated horseshoe-shaped scar of Lascar activity! Terrain above the canyons at a divergent boundary, tectonic plates move apart from one another, shallow! [ 212 ] an eruption commenced at 11:35 local time on 18 April formed the prelude the. 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