Evolution of Irruputuncu volcano, Central Andes, northern Chile

The most active voJcano in Central Volcanic Zone (CVZ) is Lascar Volcano (230:22'S-67°44'W) (Francis & Rothery, 1987), a composite voJcano formed by andesitic and dacitic lava and pyroclastic flows, and occasional basaltic andesites lava flows (Gardeweg et al., 1998). Its historie activity have been explosive principally (vulcanian and subplinian eruptions) and is related to viscous lava dome growth and collapse cycles (Matthews et al., 1997). The largest historical eruption took place in April 1993 (subplinian eruption), which produced eruptive column that extended up to 20 km and pyroclastic flows that extended up to 7.5 km of the summit (Gardeweg & Medina, 1994). The more active voJcanoes in Southern VoJcanic Zone (SVZ) are Villarrica and L1aima voJcanoes (Moreno & Fuentealba, 1994). ViUarrica Volcano (390:25'S-71 °57'W) is a stratocone built over two calderas, with more than 30 adventitious eruptive centers (Moreno, 1998), formed by basaltic and andesitic lava and pyroclastic flows (Gonzalez-Ferran, 1995). In its summit crater there is a small and continuously active lava lake (Ortiz et al., 2003; Calder et al, 2004). Since 1558,59 important eruptions have been reported (Petit-Breuilh, 1994), with hawaiian, phreatomagmatic, vuJcanian and strombolian eruptions (Moreno, 1998). ViUarrica VoJcano eruptions have emitted lava flows as long as 18 km (Ortiz et al., 2003) and important lahars (» 20 km) have been formed by glaciers melting (Gonzalez-Ferran. 1995). One of most important historical eruptions occurred in 1971 (Gonzalez-Ferran, 1995). L1aima Volcano (38°42'S-71 °44'W) is a complex composite-shield volcano, with a buried caldera and 40 parasitic scoria cones, formed by basaltic and andesitic lava flows, andesitic pyroclastic flows and, dacitic surge and pumice fall deposits (Naranjo & Moreno, J991). Since 1640, about 47 eruptions have been reported, with phreatornagmatic, strombolian and subplinian eruptions (N aranjo & Moreno, 1991; Gonzalez-Ferran, 1995). At least, 10 eruptions have emitted voluminous lava flows and pyroclasts, also lahars have been formed by glaciers melting (Moreno & Fuentealba, 1994), being the 1957 eruption the biggest historie eruption (Naranjo & Moreno, 1991). In this work, are characterized the contrasting styles of voJcanic activity of these three volcanoes, correlated the voJcanic activity with satellite responses and determined the causes of thermal anornaly for each one, using radiance data from Landsat TM and ETM+ images, between December 1984 and December 2001.

Phreatomagmatic eruption

Stratovolcano

Strombolian eruption

Lava dome

Lahar

Effusive eruption

Phreatic eruption

Volcanic hazards

Peléan eruption

Basaltic andesite

Lapilli

Lava field

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Assessing the potential for future explosive activity from Teide–Pico Viejo stratovolcanoes (Tenerife, Canary Islands)

Journal of Volcanology and Geothermal Research (2008)

Joan Martı́Adelina Geyer Joan Andújar F. Teixidó Fidel Costa

Stratovolcano

Strombolian eruption

Caldera

Phreatomagmatic eruption

10.1016/j.jvolgeores.2008.07.011

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Citations (56)

Pyroclastic flows, lahars, and mixed avalanches generated during the 2006 eruption of Augustine Volcano: Chapter 10 in <i>The 2006 eruption of Augustine Volcano, Alaska</i>

USGS professional paper (2010)

James W. Vallance K. F. Bull Michelle L. Coombs

Each of the three phases of the 2006 eruption at Augustine Volcano had a distinctive eruptive style and flowage deposits. From January 11 to 28, the explosive phase comprised short vulcanian eruptions that punctuated dome growth and produced volcanowide pyroclastic flows and more energetic hot currents whose mobility was influenced by efficient mixing with and vaporization of snow. Initially, hot flows moved across winter snowpack, eroding it to generate snow, water, and pyroclastic slurries that formed mixed avalanches and lahars, first eastward, then northward, and finally southward, but subsequent flows produced no lahars or mixed avalanches. During a large explosive event on January 27, disruption of a lava dome terminated the explosive phase and emplaced the largest pyroclastic flow of the 2006 eruption northward toward Rocky Point. From January 28 to February 10, activity during the continuous phase comprised rapid dome growth and frequent dome-collapse pyroclastic flows and a lava flow restricted to the north sector of the volcano. Then, after three weeks of inactivity, during the effusive phase of March 3 to 16, the volcano continued to extrude the lava flow, whose steep sides collapsed infrequently to produce block-and-ash flows. The three eruptive phases were each unique not only in terms of eruptive style, but also in terms of the types and morphologies of deposits that were produced, and, in particular, of their lithologic components. Thus, during the explosive phase, low-silica andesite scoria predominated, and intermediate- and high-silica andesite were subordinate. During the continuous phase, the eruption shifted predominantly to high-silica andesite and, during the effusive phase, shifted again to dense low-silica andesite. Each rock type is present in the deposits of each eruptive phase and each flow type, and lithologic proportions are unique and consistent within the deposits that correspond to each eruptive phase. The chief factors that influenced pyroclastic currents and the characteristics of their deposits were genesis, grain size, and flow surface. Column collapse from short-lived vulcanian blasts, dome collapses, and collapses of viscous lavas on steep slopes caused the pyroclastic currents documented in this study. Column-collapse flows during the explosive phase spread widely and probably were affected by vaporization of ingested snow where they overran snowpack. Such pyroclastic currents can erode substrates formed of snow or ice through a combination of mechanical and thermal processes at the bed, thus enhancing the spread of these flows across snowpack and generating mixed avalanches and lahars. Grain-size characteristics of these initial pyroclastic currents and overburden pressures at their bases favored thermal scour of snow and coeval fluidization. These flows scoured substrate snow and generated secondary slurry flows, whereas subsequent flows did not. Some secondary flows were wetter and more laharic than others. Where secondary flows were quite watery, recognizable mixed-avalanche deposits were small or insignificant, and lahars were predominant. Where such flows contained substantial amounts of snow, mixed-avalanche deposits blanketed medial reaches of valleys and formed extensive marginal terraces and axial islands in distal reaches. Flows that contained significant amounts of snow formed cogenetic mixed avalanches that slid across surfaces protected by snowpack, whereas water-rich axial lahars scoured channels. Correlations of planimetric area (A) versus volume (V) for pyroclastic deposits with similar origins and characteristics exhibit linear trends, such that A=cV2/3, where c is a constant for similar groups of flows. This relationship was tested and calibrated for dome-collapse, column-collapse, and surgelike flows using area-volume data from this study and examples from Montserrat, Merapi, and Mount St. Helens. The ratio A/V2/3=c gives a dimensionless measure of mobility calibrated for each of these three types of flow. Surgelike flows are highly mobile, with c≈520; column-collapse flows have c≈150; and dome-collapse flows have c≈35, about that of simple rock avalanches. Such calibrated mobility factors have a potential use in volcano-hazard assessments.

Lava dome

Stratovolcano

Peléan eruption

Lahar

Effusive eruption

Pyroclastic fall

Phreatic eruption

Phreatomagmatic eruption

Scoria

Dome (geology)

Strombolian eruption

10.3133/pp176910

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Analogy of Volcanic Edifices between Modern Volcanoes and Ancient Remnant Volcanoes in Songliao Basin

XU Zhong-jie

Modern volcanoes can be classified as three main forms in shape (Shield-shape,cone-shape and dome-shape) and seven different types.In surrounding sections and northern faulted depression in the Songliao Basin,there are mainly four types of volcanoes such as shield volcano,composite volcano,pyroclastic cone and lava dome.Shield volcanoes are built almost entirely of fluid lava flows,with little explosive pyroclastics.Composite volcanoes are built of flow layers alternating with pyroclas-tics,thus the alternate sequence of effusive and explosive facies is well developed.Pyroclastic cones,the simplest type of volcano,consist of particles and blobs of congealed lava from a single vent,mainly of explosive facies.Lava domes are formed by relatively small,bulbous masses of the lava which is too viscous to flow long distance,therefore,the lava piles over and around its vent by extrusion.Eruption patterns here mainly include effusive,extrusive and volcanic vent facies.In the Songliao Basin the buried volcanic edifices is characterized by slope angle ranging from minimum 3° to maximal 25°,bottom diameter from 2 to 14 kilometers and volcanic rock thickness from 100 to 600 meters.The buried volcanic edifices may cover an area of 4 to 50 sq.kilometers for each.As a whole,buried volcanoes of the northern Songliao Basin appear numerous,individually small and are controlled by regional faults.They are normally featured with crack and multi-central type eruptions,volcanic products of different vents commonly pile up each other.Volcanic lithology and lithofacies are the main factors that control the types and forms of the volcanic apparatus in the Songliao Basin.

Shield volcano

Lava dome

Volcanic cone

Volcanic plateau

Stratovolcano

Diatreme

Lava field

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Citations (4)

Volcano-Tectonic Earthquakes at Basaltic Volcanoes

Elsevier eBooks (2011)

Vyacheslav M. Zobin