VOLCANO: Smithsonian/USGS Weekly Volcanic Activity Report 4-10 July 2012

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Smithsonian/USGS Weekly Volcanic Activity Report 4-10 July 2012
From: "Kuhn, Sally" <KUHNS@xxxxxx>
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Smithsonian/USGS Weekly Volcanic Activity Report

4-10 July 2012

 

Sally Kuhn Sennert - Weekly Report Editor

kuhns@xxxxxx

URL: http://www.volcano.si.edu/reports/usgs/

 

 

New Activity/Unrest: | Hierro, Canary Islands (Spain) | Pago, New Britain

 

Ongoing Activity: | Bagana, Bougainville | Batu Tara, Komba Island (Indonesia) | Cleveland, Chuginadak Island | Fuego, Guatemala | Galeras, Colombia | Karymsky, Eastern Kamchatka (Russia) | Kilauea, Hawaii (USA) | Nevado del Ruiz, Colombia | Popocatépetl, México | Sakura-jima, Kyushu | Sangay, Ecuador | Santa María, Guatemala | Shiveluch, Central Kamchatka (Russia) | Tungurahua, Ecuador

  

 

The Weekly Volcanic Activity Report is a cooperative project between the Smithsonian's Global Volcanism Program and the US Geological Survey's Volcano Hazards Program. Updated by 2300 UTC every Wednesday, notices of volcanic activity posted on these pages are preliminary and subject to change as events are studied in more detail. This is not a comprehensive list of all of Earth's volcanoes erupting during the week, but rather a summary of activity at volcanoes that meet criteria discussed in detail in the "Criteria and Disclaimers" section. Carefully reviewed, detailed reports on various volcanoes are published monthly in the Bulletin of the Global Volcanism Network.

 

Note: Many news agencies do not archive the articles they post on the Internet, and therefore the links to some sources may not be active. To obtain information about the cited articles that are no longer available on the Internet contact the source.

 

 

New Activity/Unrest

 

 

HIERRO Canary Islands (Spain) 27.73°N, 18.03°W; summit elev. 1500 m

 

On 11 July Instituto Geográfico Nacional (IGN) reported that seismic activity and deformation at Hierro had decreased since the previous week. During 4-10 July there were 650 seismic events located, most of them offshore SW of El Hierro Island at 20 km depth. The maximum magnitude recorded was 3.8, which occurred on 10 July at 0504, and 77 earthquakes were M 2.7 or higher. The total number of located events had reached more than 2,200 since the anomalous activity began on 24 June. The deformation during this period had maximum values of about 1.5 cm in the horizontal component and 1.5 cm of vertical displacement.

 

Geologic Summary. The triangular island of Hierro is the SW-most and least studied of the Canary Islands. The massive Hierro shield volcano is truncated by a large NW-facing escarpment formed as a result of gravitational collapse of El Golfo volcano about 130,000 years ago. The steep-sided 1500-m-high scarp towers above a low lava platform bordering 12-km-wide El Golfo Bay, and three other large submarine landslide deposits occur to the SW and SE. Three prominent rifts oriented NW, NE, and south at 120 degree angles form prominent topographic ridges. The subaerial portion of the volcano consists of flat-lying Quaternary basaltic and trachybasaltic lava flows and tuffs capped by numerous young cinder cones and lava flows. Holocene cones and flows are found both on the outer flanks and in the El Golfo depression. Hierro contains the greatest concentration of young vents in the Canary Islands. Uncertainty surrounds the report of an historical eruption in 1793.

 

Source: Instituto Geográfico Nacional (IGN) http://www.ign.es/ign/main/index.do

 

 

PAGO New Britain 5.58°S, 150.52°E; summit elev. 742 m

 

Based on analyses of satellite imagery, the Darwin VAAC reported that on 11 July an ash plume from Pago rose to an altitude of 4.3 km (14,000 ft) a.s.l. and drifted over 275 km SW.

 

Geologic Summary. Pago is a young post-caldera cone that was constructed within the 5.5 x 7.5 km Witori caldera. Extensive pyroclastic-flow deposits are associated with formation of the caldera about 3,300 years ago. The gently sloping outer flanks of Witori volcano consist primarily of dacitic pyroclastic-flow and airfall deposits produced during a series of five major explosive eruptions from about 5,600 to 1,200 years ago. The Buru caldera, which may have formed around the same time, cuts the SW flank of Witori volcano. The post-caldera cone of Witori, Mount Pago, may have formed less than 350 years ago and has grown to a height above that of the Witori caldera rim. A series of nine dacitic lava flows from Pago covers much of the caldera floor. The youngest of these was erupted during the 20th century and banks against the eastern caldera wall.

 

Source: Darwin Volcanic Ash Advisory Center (VAAC) ftp://ftp.bom.gov.au/anon/gen/vaac

 

 

Ongoing Activity

 

BAGANA Bougainville 6.140°S, 155.195°E; summit elev. 1750 m

 

Based on analyses of satellite imagery, the Darwin VAAC reported that on 4 July ash plumes from Bagana rose to altitudes of 2.4-3 km (8,000-10,000 ft) a.s.l. and drifted 55 km W.

 

Geologic Summary. Bagana volcano, occupying a remote portion of central Bougainville Island, is one of Melanesia's youngest and most active volcanoes. Bagana is a massive symmetrical lava cone largely constructed by an accumulation of viscous andesitic lava flows. The entire lava cone could have been constructed in about 300 years at its present rate of lava production. Eruptive activity at Bagana is characterized by non-explosive effusion of viscous lava that maintains a small lava dome in the summit crater, although explosive activity occasionally producing pyroclastic flows also occurs. Lava flows form dramatic, freshly preserved tongue-shaped lobes up to 50-m-thick with prominent levees that descend the volcano's flanks on all sides.

 

Source: Darwin Volcanic Ash Advisory Centre (VAAC) ftp://ftp.bom.gov.au/anon/gen/vaac

 

 

BATU TARA Komba Island (Indonesia) 7.792°S, 123.579°E; summit elev. 748 m

 

Based on analyses of satellite imagery, the Darwin Volcanic Ash Advisory Centre (VAAC) reported that on 8 July an ash plume from Batu Tara rose to an altitude of 1.5 km (5,000 ft) a.s.l. and drifted almost 95 km SW.

 

Geologic Summary. The small isolated island of Batu Tara in the Flores Sea about 50 km north of Lembata (formerly Lomblen) Island contains a scarp on the eastern side similar to the Sciara del Fuoco of Italy's Stromboli volcano. Vegetation covers the flanks of Batu Tara to within 50 m of the 748-m-high summit. Batu Tara lies north of the main volcanic arc and is noted for its potassic leucite-bearing basanitic and tephritic rocks. The first historical eruption from Batu Tara, during 1847-52, produced explosions and a lava flow.

 

Source: Darwin Volcanic Ash Advisory Centre (VAAC) ftp://ftp.bom.gov.au/anon/gen/vaac

 

 

CLEVELAND Chuginadak Island 52.825°N, 169.944°W; summit elev. 1730 m

 

AVO reported that cloudy conditions at Cleveland often prevented observations during 4-9 July. Clear views of the volcano by the web camera on the morning of 6 July revealed a distinct plume, likely containing water vapor and volcanic gas, drifting several tens of miles downwind from the summit. Elevated surface temperatures were detected in satellite images on 10 July. The Volcano Alert Level remained at Watch and the Aviation Color Code remained at Orange.

 

Geologic Summary. Symmetrical Mount Cleveland stratovolcano is situated at the western end of the uninhabited dumbbell-shaped Chuginadak Island in the east-central Aleutians. The 1,730-m-high stratovolcano is the highest of the Islands of Four Mountains group and is one of the most active in the Aleutians. Numerous large lava flows descend its flanks. It is possible that some 18th to 19th century eruptions attributed to Carlisle (a volcano located across the Carlisle Pass Strait to the NW) should be ascribed to Cleveland. In 1944 Cleveland produced the only known fatality from an Aleutian eruption. Recent eruptions from Mt. Cleveland have been characterized by short-lived explosive ash emissions, at times accompanied by lava fountaining and lava flows down the flanks.

 

Source: Alaska Volcano Observatory (AVO) http://www.avo.alaska.edu/

 

 

FUEGO Guatemala 14.473°N, 90.880°W; summit elev. 3763 m

 

INSIVUMEH reported that during 4-6 July explosions from Fuego produced ash plumes that rose 400-800 m above the crater and drifted W. Rumbling sounds were reported and tephra avalanches descended the S flank. During 7-8 July rumbling and degassing sounds were reported. Although cloud cover mostly prevented observations, a weak plume was noted rising 200-300 m above the crater and drifting NE. Ash fell in Yepocapa (8 km WNW), and on the La Conchita and Monteclaro ranches. Small tephra avalanchas descended the Taniluyá (SW) and Ceniza (SSW) drainages. During 8-9 July a series of seven explosions produced ash plumes that rose 300-900 m above the crater and drifted 10 km W, again causing ashfall in Yepocapa,  La Conchita, Monte llano, and Sangre de Cristo (8 km WSW). Explosions on 10 July produced ash plumes that rose 300-600 m above the crater and drifted W. Incandescence rose above the crater during 8-10 July.

 

Geologic Summary. Volcán Fuego, one of Central America's most active volcanoes, is one of three large stratovolcanoes overlooking Guatemala's former capital, Antigua. The scarp of an older edifice, Meseta, lies between 3,763-m-high Fuego and its twin volcano to the N, Acatenango. Construction of Meseta volcano continued until the late Pleistocene or early Holocene, after which growth of the modern Fuego volcano continued the southward migration of volcanism that began at Acatenango. Frequent vigorous historical eruptions have been recorded at Fuego since the onset of the Spanish era in 1524, and have produced major ashfalls, along with occasional pyroclastic flows and lava flows. The last major explosive eruption from Fuego took place in 1974, producing spectacular pyroclastic flows visible from Antigua.

 

Source: Instituto Nacional de Sismologia, Vulcanologia, Meteorologia, e Hidrologia (INSIVUMEH) http://www.insivumeh.gob.gt/

 

 

GALERAS Colombia 1.22°N, 77.37°W; summit elev. 4276 m

 

INGEOMINAS reported that during 4-10 July seismicity at Galeras indicated continuing gas emissions; sulfur dioxide levels were moderate. The emissions, observed by a network of video cameras, contained some ash during 4-5 July. The Alert Level remained at III (Yellow; "changes in the behavior of volcanic activity").

 

Geologic Summary. Galeras, a stratovolcano with a large breached caldera located immediately W of the city of Pasto, is one of Colombia's most frequently active volcanoes. The dominantly andesitic Galeras volcanic complex has been active for more than 1 million years, and two major caldera collapse eruptions took place during the late Pleistocene. Longterm extensive hydrothermal alteration has affected the volcano. This has contributed to large-scale edifice collapse that has occurred on at least three occasions, producing debris avalanches that swept to the W and left a large horseshoe-shaped caldera inside which the modern cone has been constructed. Major explosive eruptions since the mid Holocene have produced widespread tephra deposits and pyroclastic flows that swept all but the southern flanks. A central cone slightly lower than the caldera rim has been the site of numerous small-to-moderate historical eruptions since the time of the Spanish conquistadors.

 

Source: Instituto Colombiano de Geología y Minería (INGEOMINAS) http://www.ingeominas.gov.co/

 

 

KARYMSKY Eastern Kamchatka (Russia) 54.05°N, 159.45°E; summit elev. 1536 m

 

KVERT reported that moderate seismic activity from Karymsky continued to be detected during 29 June-10 July, and indicated that possible ash plumes rose to altitudes of 2.1-3.3 km (6,900-10,800 ft) a.s.l. during 29 June-7 July. Satellite imagery showed a weak thermal anomaly on the volcano on 29 June and 1 July. The Aviation Color Code remained at Orange.

 

Geologic Summary. Karymsky, the most active volcano of Kamchatka's eastern volcanic zone, is a symmetrical stratovolcano constructed within a 5-km-wide caldera that formed about 7,600-7,700 radiocarbon years ago. Construction of the Karymsky stratovolcano began about 2,000 years later. The latest eruptive period began about 500 years ago, following a 2,300-year quiescence. Much of the cone is mantled by lava flows less than 200 years old. Historical eruptions have been Vulcanian or Vulcanian-Strombolian with moderate explosive activity and occasional lava flows from the summit crater. Most seismicity preceding Karymsky eruptions has originated beneath Akademia Nauk caldera, which is located immediately S of Karymsky volcano and erupted simultaneously with Karymsky in 1996.

 

Source: Kamchatkan Volcanic Eruption Response Team (KVERT) http://www.kscnet.ru/ivs/kvert/index_eng.php

 

 

KILAUEA Hawaii (USA) 19.421°N, 155.287°W; summit elev. 1222 m

 

During 4-10 July HVO reported that the circulating lava lake periodically rose and fell in the deep pit within Kilauea's Halema'uma'u Crater. Measurements indicated that the gas plume from the vent continued to deposit variable amounts of spatter and Pele's hair onto nearby areas. The lava pond in a small pit on the E edge of the Pu'u 'O'o crater floor and two vents along the S edge of the floor were visible with the web cameras. On most days lava flows were active on the pali, at the base of the pali and onto the coastal plain, and farther out on the coastal plain near the Royal Gardens/Hawai'i Volcanoes National Park boundary.

 

Geologic Summary. Kilauea, one of five coalescing volcanoes that comprise the island of Hawaii, is one of the world's most active volcanoes. Eruptions at Kilauea originate primarily from the summit caldera or along one of the lengthy E and SW rift zones that extend from the caldera to the sea. About 90% of the surface of Kilauea is formed of lava flows less than about 1,100 years old; 70% of the volcano's surface is younger than 600 years. A long-term eruption from the East rift zone that began in 1983 has produced lava flows covering more than 100 sq km, destroying nearly 200 houses and adding new coastline to the island.

 

Source: US Geological Survey Hawaiian Volcano Observatory (HVO) http://hvo.wr.usgs.gov/

 

 

NEVADO DEL RUIZ Colombia 4.895°N, 75.322°W; summit elev. 5321 m

 

According to INGEOMINAS, the Observatorio Vulcanológico and Sismológico de Manizales reported that during 5-9 July seismic signals at Nevado del Ruiz indicated continuing gas and ash emissions. On 6 July a gas-and-ash plume rose 400 m above the crater and drifted SW. On 8 July gas-and-ash plumes rose 400-500 m above the crater and drifted NW and W. The Washington Volcanic Ash Advisory Center (VAAC) reported that a gas-and-ash plume was observed in satellite imagery drifting 65 km. On 9 July INGEOMINAS  noted that a gas-and-ash plume, observed with a web camera, rose around 400 m above the crater. On 10 July satellite imagery and ground-based observations showed sulfur dioxide emissions. The Alert Level remained at II (Orange; "eruption likely within days or weeks").

 

Geologic Summary. Nevado del Ruiz is a broad, glacier-covered volcano in central Colombia that covers >200 sq km. Three major edifices, composed of andesitic and dacitic lavas and andesitic pyroclastics, have been constructed since the beginning of the Pleistocene. The modern cone consists of a broad cluster of lava domes built within the summit caldera of an older Ruiz volcano. The 1-km-wide, 240-m-deep Arenas crater occupies the summit. Steep headwalls of massive landslides cut the flanks of Nevado del Ruiz. Melting of its summit icecap during historical eruptions, which date back to the 16th century, has resulted in devastating lahars, including one in 1985 that was South America's deadliest eruption.

 

Sources: Instituto Colombiano de Geología y Minería (INGEOMINAS) http://www.ingeominas.gov.co/,

Washington Volcanic Ash Advisory Center (VAAC) http://www.ssd.noaa.gov/VAAC/messages.html

 

 

POPOCATEPETL México 19.023°N, 98.622°W; summit elev. 5426 m

 

CENAPRED reported that during 4-10 July seismicity at Popocatépetl indicated continuing gas-and-ash emissions. Incandescence from the crater was often observed at night. On 4 July a gas-and-steam plume drifted W. The next day a steam-and-gas plume that likely contained ash rose 2 km above the crater and drifted WSW. Some emissions were accompanied by increased incandescence from the crater. During 6-10 July steam-and-gas plumes rose from the crater. The Alert Level remained at Yellow, Phase Three.

 

Geologic Summary. Popocatépetl, whose name is the Aztec word for smoking mountain, towers to 5,426 m 70 km SE of Mexico City and is North America's second-highest volcano. Frequent historical eruptions have been recorded since the beginning of the Spanish colonial era. A small eruption on 21 December 1994 ended five decades of quiescence. Since 1996 small lava domes have incrementally been constructed within the summit crater and destroyed by explosive eruptions. Intermittent small-to-moderate gas-and-ash eruptions have continued, occasionally producing ashfall in neighboring towns and villages.

 

Source: Centro Nacional de Prevencion de Desastres (CENAPRED) http://www.cenapred.unam.mx/es/

 

SAKURA-JIMA Kyushu 31.585°N, 130.657°E; summit elev. 1117 m

 

JMA reported that during 2-6 July explosions from Sakura-jima's Showa Crater ejected tephra as far as 1,300 m from the crater. Based on information from JMA, the Tokyo VAAC reported multiple explosions during 4-10 July; plumes rose to altitudes of 1.8-3.7 km (6,000-12,000 ft) a.s.l. and drifted E, SE, and N. A pilot observed an ash plume on 4 July that rose to an altitude of 2.4 (8,000 ft) a.s.l.

 

Geologic Summary. Sakura-jima, one of Japan's most active volcanoes, is a post-caldera cone of the Aira caldera at the northern half of Kagoshima Bay. Eruption of the voluminous Ito pyroclastic flow was associated with the formation of the 17 x 23-km-wide Aira caldera about 22,000 years ago. The construction of Sakura-jima began about 13,000 years ago and built an island that was finally joined to the Osumi Peninsula during the major explosive and effusive eruption of 1914. Activity at the Kita-dake summit cone ended about 4,850 years ago, after which eruptions took place at Minami-dake. Frequent historical eruptions, recorded since the 8th century, have deposited ash on Kagoshima, one of Kyushu's largest cities, located across Kagoshima Bay only 8 km from the summit. The largest historical eruption took place during 1471-76.

 

Sources: Japan Meteorological Agency (JMA) http://www.jma.go.jp/jma/,

Tokyo Volcanic Ash Advisory Center (VAAC) http://ds.data.jma.go.jp/svd/vaac/data/vaac_list.html

 

 

SANGAY Ecuador 2.002°S, 78.341°W; summit elev. 5230 m

 

According to the Washington VAAC, a thermal anomaly on Sangay was detected in satellite imagery during 4-6 July.

 

Geologic Summary. The isolated Sangay volcano, located E of the Andean crest, is the southernmost of Ecuador's volcanoes, and its most active. It has been in frequent eruption for the past several centuries. The steep-sided, 5,230-m-high glacier-covered volcano grew within horseshoe-shaped calderas of two previous edifices, which were destroyed by collapse to the E, producing large debris avalanches that reached the Amazonian lowlands. The modern edifice dates back to at least 14,000 years ago. Sangay towers above the tropical jungle on the E side; on the other sides flat plains of ash from the volcano have been sculpted by heavy rains into steep-walled canyons up to 600 m deep. The earliest report of an historical eruption was in 1628. More or less continuous eruptions were reported from 1728 until 1916, and again from 1934 to the present. The more or less constant eruptive activity has caused frequent changes to the morphology of the summit crater complex.

 

Source: Washington Volcanic Ash Advisory Center (VAAC) http://www.ssd.noaa.gov/VAAC/messages.html

 

 

SANTA MARIA Guatemala 14.756°N, 91.552°W; summit elev. 3772 m

 

INSIVUMEH reported that during 4-6 and 9-10 July an explosion from Santa María's Santiaguito lava-dome complex produced an ash plume that rose 300-800 m above Caliente dome and drifted SW. Ashfall was reported in La Florida (5 km S), Monte Claro (S), and Palajunoj (SW). Tephra avalanches from the lava dome traveled down the SE and SW flanks. During 7-8 July fumarolic plumes rose 200 m above the crater and drifted SW. One explosion generated an ash plume that rose 300 m and drifted SW. During 8-9 July gas plumes rose from the crater and avalanches descended the SE and SW flanks. Active lava flows were observed at night during 9-10 July; incandescent material traveled down the SE and SW flanks.

 

Geologic Summary. Symmetrical, forest-covered Santa María volcano is one of a chain of large stratovolcanoes that rises dramatically above the Pacific coastal plain of Guatemala. The stratovolcano has a sharp-topped, conical profile that is cut on the SW flank by a large, 1-km-wide crater, which formed during a catastrophic eruption in 1902 and extends from just below the summit to the lower flank. The renowned Plinian eruption of 1902 followed a long repose period and devastated much of SW Guatemala. The large dacitic Santiaguito lava-dome complex has been growing at the base of the 1902 crater since 1922. Compound dome growth at Santiaguito has occurred episodically from four westward-younging vents, accompanied by almost continuous minor explosions and periodic lava extrusion, larger explosions, pyroclastic flows, and lahars.

 

Source: Instituto Nacional de Sismologia, Vulcanologia, Meteorologia, e Hidrologia (INSIVUMEH) http://www.insivumeh.gob.gt/

 

 

SHIVELUCH Central Kamchatka (Russia) 56.653°N, 161.360°E; summit elev. 3283 m

 

KVERT reported that during 29 June-6 July explosive activity at Shiveluch continued and seismic data indicated that possible ash plumes rose to an altitude of 4.7 km (15,400 ft) a.s.l. Observers noted ash plumes rising to an altitude of 3.5 km (11,500 ft) a.s.l. on 29 June; weather conditions prevented observations of the volcano on the other days. Satellite imagery showed a thermal anomaly on the lava dome during 28-30 June and 7-10 July. The Aviation Color Code remained at Orange.

 

Geologic Summary. The high, isolated massif of Shiveluch volcano (also spelled Sheveluch) rises above the lowlands NNE of the Kliuchevskaya volcano group and forms one of Kamchatka's largest and most active volcanoes. The currently active Molodoy Shiveluch lava-dome complex was constructed during the Holocene within a large breached caldera formed by collapse of the massive late-Pleistocene Strary Shiveluch volcano. At least 60 large eruptions of Shiveluch have occurred during the Holocene, making it the most vigorous andesitic volcano of the Kuril-Kamchatka arc. Frequent collapses of lava-dome complexes, most recently in 1964, have produced large debris avalanches whose deposits cover much of the floor of the breached caldera. Intermittent explosive eruptions began in the 1990s from a new lava dome that began growing in 1980. The largest historical eruptions from Shiveluch occurred in 1854 and 1964.

 

Source: Kamchatkan Volcanic Eruption Response Team (KVERT) http://www.kscnet.ru/ivs/kvert/index_eng.php

 

 

TUNGURAHUA Ecuador 1.467°S, 78.442°W; summit elev. 5023 m

 

IG reported that during 4-10 July visual observations of Tungurahua were limited due to cloud cover. An explosion on 5 July produced "cannon shot" sounds, along with sounds resembling blocks rolling down the flanks.  Ashfall was reported in Manzano (8 km SW) and Chacuaco. On 6 July a satellite image showed a steam-and gas plume drifting W. On 7 and 9 July steam plumes rose 100 m above the crater.

 

Geologic Summary. The steep-sided Tungurahua stratovolcano towers more than 3 km above its northern base. It sits ~140 km S of Quito, Ecuador's capital city, and is one of Ecuador's most active volcanoes. Historical eruptions have all originated from the summit crater. They have been accompanied by strong explosions and sometimes by pyroclastic flows and lava flows that reached populated areas at the volcano's base. The last major eruption took place from 1916 to 1918, although minor activity continued until 1925. The latest eruption began in October 1999 and prompted temporary evacuation of the town of Baños on the N side of the volcano.

 

Source: Instituto Geofísico-Escuela Politécnica Nacional (IG) http://www.igepn.edu.ec/

 

+++++++++++++++++++++++++++++++++++++

Sally Kuhn Sennert

SI/USGS Weekly Volcanic Activity Report Editor

Global Volcanism Program

http://www.volcano.si.edu/reports/usgs/

Smithsonian Institution, National Museum of Natural History

Department of Mineral Sciences, MRC-119

Washington, D.C., 20560

Phone: 202.633.1805
Fax: 202.357.2476

 
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