VOLCANO: SI/USGS Weekly Volcanic Activity Report 30 December 2009-5 January 2010

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SI/USGS Weekly Volcanic Activity Report 30 December 2009-5 January 2010
From: "Sally Kuhn Sennert" <KUHNS@xxxxxx>
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SI/USGS Weekly Volcanic Activity Report
30 December 2009-5 January 2010

Sally Kuhn Sennert - Weekly Report Editor
kuhns@xxxxxx
URL: http://www.volcano.si.edu/reports/usgs/


New Activity/Unrest: | Galeras, Colombia | Mayon, Luzon | Nyamuragira,
Democratic Republic of Congo | Piton de la Fournaise, Reunion Island |
Rinjani, Lombok Island (Indonesia) | Tungurahua, Ecuador | Turrialba,
Costa Rica

Ongoing Activity: | Barren Island, Andaman Is | Chaitén, Southern
Chile | Karymsky, Eastern Kamchatka | Kilauea, Hawaii (USA) |
Kliuchevskoi, Central Kamchatka (Russia) | Nevado del Huila, Colombia
| Rabaul, New Britain | Sakura-jima, Kyushu | Sangay, Ecuador | Santa
María, Guatemala | Shiveluch, Central Kamchatka (Russia) | Soufrière
Hills, Montserrat | Suwanose-jima, Ryukyu Islands (Japan)

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


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

An explosive eruption from Galeras detected by the seismic network on
2 January prompted INGEOMINAS to raise the Alert Level to I (Red;
"imminent eruption or in progress"). An ash plume rose to an altitude
of 12 km (39,400 ft) a.s.l. and drifted W and NW. Ashfall was reported
in areas downwind, as far away as 110 km W. Ejected incandescent
blocks fell onto the flanks 3.2-3.5 km away from the summit and
ignited fires. An overflight on 3 January revealed diffuse gas plumes
from the main crater. Fires started the previous day continued to burn
on the N flank. The Alert Level was lowered to II (Orange; "probable
eruption in term of days or weeks").

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//


MAYON Luzon 13.257°N, 123.685°E; summit elev. 2462 m

PHIVOLCS reported declining activity at Mayon from 28 December to 2
January. Steam plumes were emitted from the crater, but ash plumes
were last seen on 29 December. In addition, the majority of the
seismic signals originated from rockfalls and detached lava fragments
rolling down the flanks from advancing lava flows. Sulfur dioxide
emissions also decreased from close to 9,000 tonnes per day to about
2,600 tonnes per day. PHIVOLCS lowered the Alert Level from 4 to 3,
and reminded the public that no human activity should occur within the
6-km radius Permanent Danger Zone (PDZ) around the volcano and the
7-km Extended Danger Zone (EDZ) on the SE flank. During 2-5 January,
seismic activity indicated rockfall events related to the detachment
of lava fragments at the upper slopes. Cloud cover at the summit
prevented observations of steam plumes. Incandescence from the crater
at night was noted.

Geologic Summary. Beautifully symmetrical Mayon volcano, which rises
to 2,462 m above the Albay Gulf, is the Philippines' most active
volcano. The structurally simple volcano has steep upper slopes that
average 35-40° and is capped by a small summit crater. The historical
eruptions of this basaltic-andesitic volcano date back to 1616 and
range from Strombolian to basaltic Plinian. Eruptions occur
predominately from the central conduit and have also produced lava
flows that travel far down the flanks. Pyroclastic flows and mudflows
have commonly swept down many of the approximately 40 ravines that
radiate from the summit and have often devastated populated lowland
areas. Mayon's most violent eruption, in 1814, killed more than 1,200
people and devastated several towns. Eruptions that began in February
2000 led PHIVOLCS to recommend on 23 February 2000 the evacuation of
people within a radius of 7 km from the summit in the SE and within a
6 km radius for the rest of the volcano.

Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
http://www.phivolcs.dost.gov.ph/


NYAMURAGIRA Democratic Republic of Congo 1.408°S, 29.20°E; summit elev. 3058 m

According to news articles, Nyamuragira erupted on 2 January from a
fissure on the SE flank. Park rangers reported hearing a loud
explosion in the early morning before seeing flowing lava. By 3
January, the lava flow had traveled 4.6 km, was 15 m wide, and had
burned about 10 hectares of forest in a non-populated area of the
Virunga National Park.

Geologic Summary. Africa's most active volcano, Nyamuragira (Also
spelled Nyamulagira) is a massive basaltic shield volcano N of Lake
Kivu and NW of Nyiragongo volcano. Lava flows from Nyamuragira cover
1,500 sq km of the East African Rift. The 3058-m-high summit is
truncated by a small 2 x 2.3 km summit caldera that has walls up to
about 100 m high. About 40 historical eruptions have occurred since
the mid-19th century within the summit caldera and from numerous
fissures and cinder cones on the volcano's flanks. A lava lake in the
summit crater, active since at least 1921, drained in 1938.
Twentieth-century flank lava flows extend more than 30 km from the
summit, reaching as far as Lake Kivu.

Sources: CNN http://www.cnn.com/2010/WORLD/africa/01/02/congo.volcano/index.html?eref=ib_topstories,
Agence France-Presse
http://www.google.com/hostednews/afp/article/ALeqM5gttS1HfXOoqOMHLFL5jN2ek4Q9cA,
UN News Centre http://www.un.org/apps/news/story.asp?NewsID=33396&Cr=&Cr1=,
United Nations Organization Mission in the Democratic Republic of the
Congo (MONUC) http://monuc.unmissions.org/Default.aspx?tabid=932&ctl=Details&mid=2070&ItemID=7098


PITON DE LA FOURNAISE Reunion Island 21.231°S, 55.713°E; summit elev. 2632 m

OVPDLF reported that a seismic crisis at Piton de la Fournaise on 29
December was characterized by numerous earthquakes in the area W and
NW of Dolomieu crater (max M 3), at depths of 1.1-2.2 km below the
summit. Deformation was also detected. On 31 December, OVPDLF reported
decreased seismicity and fewer landslides within Dolomieu crater on 30
and 31 December. On 2 January, an eruption from a fissure near the top
of the W crater rim, preceded by a seismic crisis, produced lava
fountains a few tens of meters high and lava flows in Dolomieu crater.
Large landslides in Bory crater (W) along with the fissure eruption
generated ash and gas plumes that rose above Piton de la Fournaise.
During 2-3 January, seismicity and the number of landslides decreased.
As of 4 January, the lava flows covered about 80 percent of the crater
floor. Lava fountaining was still visible.

Geologic Summary. Massive Piton de la Fournaise shield volcano on the
island of Réunion is one of the world's most active volcanoes. Most
historical eruptions have originated from the summit and flanks of a
400-m-high lava shield, Dolomieu, that has grown within the youngest
of three large calderas. This depression is 8 km wide and is breached
to below sea level on the eastern side. More than 150 eruptions, most
of which have produced fluid basaltic lava flows within the caldera,
have been documented since the 17th century. The volcano is monitored
by the Piton de la Fournaise Volcano Observatory, one of several
operated by the Institut de Physique du Globe de Paris.

Source: Observatoire Volcanologique du Piton de la Fournaise (OVPDLF)
http://www.ipgp.fr/pages/03030810.php


RINJANI Lombok Island (Indonesia) 8.42°S, 116.47°E; summit elev. 3726 m

Based on a pilot report, the Darwin VAAC reported that on 2 January an
ash plume from Rinjani rose to an unspecified altitude. The plume was
not identified in satellite imagery; however a meteorological cloud
was present in the area.

Geologic Summary. Rinjani volcano on the island of Lombok rises to
3,726 m, second in height among Indonesian volcanoes only to Sumatra's
Kerinci volcano. Rinjani has a steep-sided conical profile when viewed
from the E, but the W side of the compound volcano is truncated by the
6 x 8.5 km, oval-shaped Segara Anak caldera. The western half of the
caldera contains a 230-m-deep lake whose crescentic form results from
growth of the post-caldera cone Barujari at the E end of the caldera.
Historical eruptions at Rinjani dating back to 1847 have been
restricted to Barujari cone and consist of moderate explosive activity
and occasional lava flows that have entered Segara Anak lake.

Source: Darwin Volcanic Ash Advisory Centre (VAAC)
http://www.ssd.noaa.gov/VAAC/OTH/AU/messages.html


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

The IG reported steam emissions from Tungurahua during 30 December-3
January. On 1 January, an ash plume rose to an altitude of 5.9 km
(19,500 ft) a.s.l. and drifted NW. Slight ashfall was reported the
next day in Manzano, 8 km SW. Roaring noises and incandescence from
the crater were also reported. On 3 and 4 January, incandescent blocks
were ejected from the crater. Based on information from the Guayaquil
MWO and SIGMET notices, the Washington VAAC reported that ash plumes
rose to altitudes of 6.7-9.1 km (22,000-30,000 ft) a.s.l. and drifted
W. Thermal anomalies were detected in satellite imagery. On 4 January,
ashfall was reported in areas to the W and SW.

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.

Sources: Instituto Geofísico-Escuela Politécnica Nacional (IG)
http://www.igepn.edu.ec/,
Volcanic Ash Advisory Center (VAAC) http://www.ssd.noaa.gov/VAAC/messages.html


TURRIALBA Costa Rica 10.025°N, 83.767°W; summit elev. 3340 m

On 5 January, OVSICORI-UNA reported that an eruption from Turrialba
produced ashfall in local areas, particularly in areas to the SW,
including near Irazú volcano (11 km SW). According to news articles,
about 20 people evacuated the area.

Geologic Summary. Turrialba, the easternmost of Costa Rica's Holocene
volcanoes, is a large vegetated basaltic-to-dacitic stratovolcano
located across a broad saddle NE of Irazú volcano overlooking the city
of Cartago. The massive 3340-m-high Turrialba is exceeded in height
only by Irazú, covers an area of 500 sq km, and is one of Costa Rica's
most voluminous volcanoes. Three well-defined craters occur at the
upper SW end of a broad 800 x 2200 m wide summit depression that is
breached to the NE. Most activity at Turrialba originated from the
summit vent complex, but two pyroclastic cones are located on the SW
flank. Five major explosive eruptions have occurred at Turrialba
during the past 3500 years. Turrialba has been quiescent since a
series of explosive eruptions during the 19th century that were
sometimes accompanied by pyroclastic flows. Fumarolic activity
continues at the central and SW summit craters.

Sources: Observatorio Vulcanológico y Sismológico de Costa
Rica-Universidad Nacional (OVSICORI-UNA)
http://www.ovsicori.una.ac.cr/,
Reuters http://www.reuters.com/article/idUSTRE6050FS20100106


Ongoing Activity


BARREN ISLAND Andaman Is 12.278°N, 93.858°E; summit elev. 354 m

Based on a pilot report, the Darwin VAAC reported that on 3 January a
plume from Barren Island rose to an altitude of 1.5 km (5,000 ft)
a.s.l. The plume was not identified in satellite imagery; however a
meteorological cloud was present in the area.

Geologic Summary. Barren Island, a possession of India in the Andaman
Sea about 135 km NE of Port Blair in the Andaman Islands, is the only
historically active volcano along the N-S-trending volcanic arc
extending between Sumatra and Burma (Myanmar). The 354-m-high island
is the emergent summit of volcano that rises from a depth of about
2,250 m. The small, uninhabited 3-km-wide island contains a roughly
2-km-wide caldera with walls 250-350 m high. The caldera, which is
open to the sea on the W, was created during a major explosive
eruption in the late Pleistocene that produced pyroclastic-flow and
-surge deposits. The morphology of a fresh pyroclastic cone that was
constructed in the center of the caldera has varied during the course
of historical eruptions. Lava flows fill much of the caldera floor and
have reached the sea along the western coast during historical
eruptions.

Source: Darwin Volcanic Ash Advisory Centre (VAAC)
http://www.ssd.noaa.gov/VAAC/OTH/AU/messages.html


CHAITEN Southern Chile 42.833°S, 72.646°W; summit elev. 1122 m

Based on web camera views, the Buenos Aires VAAC reported that a plume
from Chaitén's lava-dome complex drifted SE on 30 December at an
altitude of 2.1 km (7,000 ft) a.s.l.

Geologic Summary. Chaitén is a small, glacier-free caldera with a
Holocene lava dome located 10 km NE of the town of Chaitén on the Gulf
of Corcovado. A pyroclastic-surge and pumice deposit considered to
originate from the eruption that formed the elliptical 2.5 x 4 km wide
summit caldera was dated at about 9400 years ago. A rhyolitic,
962-m-high obsidian lava dome occupies much of the caldera floor.
Obsidian cobbles from this dome found in the Blanco River are the
source of prehistorical artifacts from archaeological sites along the
Pacific coast as far as 400 km away from the volcano to the north and
south. The caldera is breached on the SW side by a river that drains
to the bay of Chaitén, and the high point on its southern rim reaches
1122 m.

Source: Buenos Aires Volcanic Ash Advisory Center (VAAC)
http://www.ssd.noaa.gov/VAAC/OTH/AG/messages.html


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

KVERT reported that a thermal anomaly over Karymsky was detected in
satellite imagery during 24-26 and 29-30 December. Gas-and-steam
bursts were seen by volcanologists on 28 December. The Level of
Concern 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 30 December-3 January, HVO reported that lava flowed SE from
beneath Kilauea's Thanksgiving Eve Breakout (TEB) and rootless shield
complex through a lava tube system, reaching the ocean at Waikupanaha.
Lava was not seen entering the ocean on 4 and 5 January. Thermal
anomalies detected by satellite and occasional visual observations
revealed active lava flows on the pali. Incandescence was seen almost
daily coming from Pu'u 'O'o crater. During an overflight of Pu'u 'O'o
crater on 29 December, geologists saw that a part of the high point of
the W rim had collapsed, and a new gas vent had opened up at base of
the N wall.

The vent in Halema'uma'u crater continued to produce a plume that
drifted NE and NW, dropping small amounts of ash, and occasionally
fresh spatter, downwind. Incandescence originated from an active and
sometimes sloshing lava surface within an opening on the deep floor of
the vent cavity.

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/


KLIUCHEVSKOI Central Kamchatka (Russia) 56.057°N, 160.638°E; summit elev. 4835 m

KVERT reported that during 24-31 December seismic activity from
Kliuchevskoi was above background levels and lava continued to flow
down the ESE flank. Strombolian activity ejected material 500 m above
the crater. Satellite imagery revealed a large daily thermal anomaly
at the volcano. The Level of Concern Color Code remained at Orange.

Geologic Summary. Kliuchevskoi is Kamchatka's highest and most active
volcano. Since its origin about 7,000 years ago, the beautifully
symmetrical, 4,835-m-high basaltic stratovolcano has produced frequent
moderate-volume explosive and effusive eruptions without major periods
of inactivity. More than 100 flank eruptions, mostly on the NE and SE
flanks of the conical volcano between 500 m and 3,600 m elevation,
have occurred during the past 3,000 years. The morphology of its
700-m-wide summit crater has been frequently modified by historical
eruptions, which have been recorded since the late-17th century.
Historical eruptions have originated primarily from the summit crater,
but have also included major explosive and effusive events from flank
craters.

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


NEVADO DEL HUILA Colombia 2.93°N, 76.03°W; summit elev. 5364 m

Based on web camera views, INGEOMINAS reported that during 23-29
December a continuous white plume from Nevado del Huila rose 1 km. The
output of sulfur dioxide was less than during the previous months of
October and November. Seismicity and the rate of lava extrusion had
also decreased during the previous weeks. On 5 January, INGEOMINAS
lowered the Alert Level to III (Yellow; "changes in the behavior of
volcanic activity").

Geologic Summary. Nevado del Huila, the highest active volcano in
Colombia, is an elongated N-S-trending volcanic chain mantled by a
glacier icecap. The andesitic-dacitic volcano was constructed within a
10-km-wide caldera. Volcanism at Nevado del Huila has produced six
volcanic cones whose ages in general migrated from south to north. Two
glacier-free lava domes lie at the southern end of the Huila volcanic
complex. The first historical eruption from this little known volcano
took place in the 16th century. Two persistent steam columns rise from
the central peak, and hot springs are also present.

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


RABAUL New Britain 4.271°S, 152.203°E; summit elev. 688 m

RVO reported that activity from Rabaul caldera's Tavurvur cone was at
a low level during 21-31 December; no emission from the crater was
observed on most days. White steam plumes accompanied by blue plumes
were occasionally emitted. On 23 December, ash emissions rose less
than 200 m above the cone. Based on analyses of satellite imagery, the
Darwin VAAC reported that on 31 December an ash plume rose to an
altitude of 2.4 km (8,000 ft) a.s.l. and drifted less than 30 km SE.

Geologic Summary. The low-lying Rabaul caldera on the tip of the
Gazelle Peninsula at the NE end of New Britain forms a broad sheltered
harbor. The outer flanks of the 688-m-high asymmetrical pyroclastic
shield volcano are formed by thick pyroclastic-flow deposits. The 8 x
14 km caldera is widely breached on the E, where its floor is flooded
by Blanche Bay. Two major Holocene caldera-forming eruptions at Rabaul
took place as recently as 3,500 and 1,400 years ago. Three small
stratovolcanoes lie outside the northern and NE caldera rims.
Post-caldera eruptions built basaltic-to-dacitic pyroclastic cones on
the caldera floor near the NE and western caldera walls. Several of
these, including Vulcan cone, which was formed during a large eruption
in 1878, have produced major explosive activity during historical
time. A powerful explosive eruption in 1994 occurred simultaneously
from Vulcan and Tavurvur volcanoes and forced the temporary
abandonment of Rabaul city.

Sources: Rabaul Volcano Observatory (RVO),
Darwin Volcanic Ash Advisory Centre (VAAC)
http://www.ssd.noaa.gov/VAAC/OTH/AU/messages.html


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

Based on information from JMA, the Tokyo VAAC reported that during 30
December-5 January multiple explosions from Sakura-jima often produced
plumes that rose to altitudes of 1.2-2.7 km (4,000-9,000 ft) a.s.l.
and drifted NE, E, SE, and S. During 31 December-4 January pilots
reported that ash plumes rose to altitudes of 2.4-5.5 km (8,000-18,000
ft) a.s.l. and drifted SE and E.

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.

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


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

The Washington VAAC reported that during 2-4 January thermal anomalies
from Sangay were seen in satellite imagery. On 2 January, a pilot saw
an ash plume drifting NW at an altitude of 7 km (23,000 ft) a.s.l. An
ash plume was also reported by a pilot the next day.

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

On 30 December and 5 January, INSIVUMEH reported that explosions from
Santa María's Santiaguito lava dome complex produced ash plumes that
rose to altitudes of 3-3.4 km (10,000-11,200 ft) a.s.l. and drifted W
and SW. The Washington VAAC reported that ash plumes seen on satellite
imagery drifted more than 30 km WSW. Avalanches occasionally descended
the SW flank of the dome.

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.

Sources: Instituto Nacional de Sismologia, Vulcanologia, Meteorologia,
e Hidrologia (INSIVUMEH) http://www.insivumeh.gob.gt/ ,
Washington Volcanic Ash Advisory Center (VAAC)
http://www.ssd.noaa.gov/VAAC/messages.html


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

KVERT reported that during 24-31 December seismic activity from
Shiveluch was above background levels, possibly indicating ash plumes
rising to an altitude of 4.9 km (16,000 ft) a.s.l. Fumarolic activity
was occasionally seen when the weather was clear. Analyses of
satellite imagery revealed a large daily thermal anomaly from the lava
dome and an ash plume that drifted 15 km W on 28 December. The Level
of Concern Color Code remained at Orange. Based on information from
KEMSD and KVERT, the Tokyo VAAC reported that during 30 December-3
January eruptions produced plumes that rose to altitudes of 4.3-7.6 km
(14,000-25,000 ft) a.s.l.

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.

Sources: Kamchatkan Volcanic Eruption Response Team (KVERT)
http://www.kscnet.ru/ivs/kvert/index_eng.php,
Tokyo Volcanic Ash Advisory Center (VAAC)
http://www.ssd.noaa.gov/VAAC/OTH/JP/messages.html


SOUFRIERE HILLS Montserrat 16.72°N, 62.18°W; summit elev. 915 m

MVO reported that during 24-31 December activity from the Soufrière
Hills lava dome continued at a high level. Cycles of increased
activity associated with vigorous ash venting and pyroclastic flows
occurred every six to eight hours. Audible rockfalls, roaring, and
occasional thunder were noted during the most intense events. Frequent
pyroclastic flows traveled N down Whites Ghaut, Farrells plain, and
Tyers Ghaut. Pyroclastic flows also traveled W down Gages Valley into
Spring Ghaut, and occasionally to the S in Gingoes Ghaut. On 29
December several pyroclastic flows traveled 2.5 km, reaching Dyers
village. A comparison of photographs from 30 December and 2 January
revealed that the lava dome morphology had changed rapidly, with a
significant addition of lava on the N side. The additional area of
growth was approximately 60 m high and 100 m wide. The Hazard Level
remained at 4.

Geologic Summary. The complex dominantly andesitic Soufrière Hills
volcano occupies the southern half of the island of Montserrat. The
summit area consists primarily of a series of lava domes emplaced
along an ESE-trending zone. English's Crater, a 1-km-wide crater
breached widely to the E, was formed during an eruption about 4,000
years ago in which the summit collapsed, producing a large submarine
debris avalanche. Block-and-ash flow and surge deposits associated
with dome growth predominate in flank deposits at Soufrière Hills.
Non-eruptive seismic swarms occurred at 30-year intervals in the 20th
century, but with the exception of a 17th-century eruption that
produced the Castle Peak lava dome, no historical eruptions were
recorded on Montserrat until 1995. Long-term small-to-moderate ash
eruptions beginning in that year were later accompanied by lava-dome
growth and pyroclastic flows that forced evacuation of the southern
half of the island and ultimately destroyed the capital city of
Plymouth, causing major social and economic disruption.

Source: Montserrat Volcano Observatory (MVO) http://www.mvo.ms/


SUWANOSE-JIMA Ryukyu Islands (Japan) 29.635°N, 129.716°E; summit elev. 799 m

Based on information from JMA, the Tokyo VAAC reported explosions from
Suwanose-jima during 30 December-2 January and 4-5 January. Plumes
rose to altitudes of 1.5-1.8 km (5,000-6,000 ft) a.s.l. on 2 and 4
January, and drifted NE and E on 4 January.

Geologic Summary. The 8-km-long, spindle-shaped island of
Suwanose-jima in the northern Ryukyu Islands consists of an andesitic
stratovolcano with two historically active summit craters. Only about
50 persons live on the sparsely populated island. The summit of the
volcano is truncated by a large breached crater extending to the sea
on the east flank that was formed by edifice collapse. Suwanose-jima,
one of Japan's most frequently active volcanoes, was in a state of
intermittent Strombolian activity from On-take, the NE summit crater,
that began in 1949 and lasted nearly a half century. The largest
historical eruption took place in 1813-14, when thick scoria deposits
blanketed residential areas, after which the island was uninhabited
for about 70 years. The SW crater produced lava flows that reached the
western coast in 1813, and lava flows reached the eastern coast of the
island in 1884.

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

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