VOLCANO: SI/USGS Weekly Volcanic Activity Report 9-15 December 2009

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SI/USGS Weekly Volcanic Activity Report 9-15 December 2009
From: "Kuhn, Sally" <KUHNS@xxxxxx>
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SI/USGS Weekly Volcanic Activity Report
9-15 December 2009

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


New Activity/Unrest: | Concepción, Nicaragua | Galeras, Colombia |
Mayon, Luzon | Piton de la Fournaise, Reunion Island | Soufrière
Hills, Montserrat

Ongoing Activity: | Chaitén, Southern Chile | Dukono, Halmahera |
Fuego, Guatemala | Karymsky, Eastern Kamchatka | Kilauea, Hawaii (USA)
| Kliuchevskoi, Central Kamchatka (Russia) | Manam, Northeast of New
Guinea (SW Pacific) | Nevado del Huila, Colombia | Pacaya, Guatemala |
Rabaul, New Britain | Sakura-jima, Kyushu | Santa María, Guatemala |
Shiveluch, Central Kamchatka (Russia) | 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


CONCEPCION Nicaragua 11.538°N, 85.622°W; summit elev. 1700? m

According to a news article, INETER reported that an explosion of ash
and gas from Concepción on 11 December produced a plume that rose 150
m above the crater. Ashfall was reported in three nearby communities.

Geologic Summary. Volcán Concepción is one of Nicaragua's highest
volcanoes and is also one of its most active. The symmetrical volcano
forms the NW half of the dumbbell-shaped island of Ometepe in Lake
Nicaragua. Concepción is connected to neighboring Madera volcano by a
narrow isthmus. N-S-trending fractures cutting across the volcano are
associated with spatter cones, cinder cones, and maars located on the
middle N flank and on the lower S flank down to Lake Nicaragua.
Concepción has had frequent moderate explosive eruptions in the past
century, most of which have originated from a small summit crater.

Source: Reuters http://www.abc.net.au/news/stories/2009/12/12/2769772.htm


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

INGEOMINAS reported that observations of Galeras during an overflight
on 3 December revealed thermal anomalies in the main crater measuring
155 degrees Celsius. During 8-11 December, seismic activity decreased,
although some seismic signals resembled patterns seen prior to
previous eruptions. Sulfur dioxide emissions were low. Seismicity
increased on 12 December; earthquakes M 2.2 and less were detected
within 2 km of the summit and at depths up to 3 km below the summit
during 12-15 December. The Alert Level was raised 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

According to news articles, PHIVOLCS reported that on 11 December an
explosion from Mayon was detected by the seismic network. On 14
December, incandescence emanated from the lava dome in the summit
crater and incandescent material traveled as far as 3 km down the S
and SE flanks. At least five minor explosions were detected by the
seismic network. Some local ashfall was reported. The Alert Level was
raised to 3, prompting the order to evacuate about 50,000 people
living within an 8-km radius from the base of the volcano.

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.

Sources: Philippine Daily Inquirer
http://newsinfo.inquirer.net/breakingnews/regions/view/20091214-242001/Philvolcs-to-raise-Alert-Level-3-on-Mayon,
Inquirer Southern Luzon
http://newsinfo.inquirer.net/breakingnews/regions/view/20091215-242075/Albay-to-evacuate-47000-around-Mayon,
The Manila Times
http://www.manilatimes.net/index.php/component/content/article/42-rokstories/7926-as-mayon-acts-up-locals-evacuate


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

OVPDLF reported that on 14 December an eruption from Piton de la
Fournaise was preceded by a seismic crisis and summit deformation.
Sub-parallel fissures along the rim of Dolomieu crater fed lava flows
on the S slope. A third fissure that also produced lava flows opened
on the E flank. The lava stopped flowing during the night, after a
gradual decrease. On 15 December, gas was emitted from the S and SE
fractures and low-intensity tremor was detected.

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


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

MVO reported that during 4-11 December activity from the Soufrière
Hills lava dome continued at a high level and pyroclastic flow
activity was concentrated on the N side. Pyroclastic flows traveled as
far as 2 km NW into Tyers Ghaut and NE in abundance down Tuitt's
Ghaut, and sometimes Whites Bottom Ghaut, continuing onto Farrell's
plain. A few small pyroclastic flows also descended the Tar River
valley to the E. On 10 December, a large seismic signal was associated
with a relatively large pyroclastic flow in Tyers Ghaut that traveled
3.5 km, stopping just beyond the W end of Lee's village. The event
prompted the National Disaster Preparedness and Response Advisory
Committee (NDPRAC) to raise the Hazard Level to 4, restricting the
hours residents can enter certain pre-designated hazard areas.

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/


Ongoing Activity


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
steam-and-gas plume from Chaitén's lava-dome complex drifted SE on 12
December at altitudes of 1.5-2.1 km (5,000-7,000 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


DUKONO Halmahera 1.68°N, 127.88°E; summit elev. 1335 m

The Darwin VAAC reported that during 9-11 December ash plumes from
Dukono rose to an altitude of 3 km (10,000 ft) a.s.l. and drifted
90-130 km E and SE.

Geologic Summary. Reports from this remote volcano in northernmost
Halmahera are rare, but Dukono has been one of Indonesia's most active
volcanoes. More-or-less continuous explosive eruptions, sometimes
accompanied by lava flows, occurred from 1933 until at least the
mid-1990s, when routine observations were curtailed. During a major
eruption in 1550, a lava flow filled in the strait between Halmahera
and the N-flank cone of Gunung Mamuya. Dukono is a complex volcano
presenting a broad, low profile with multiple summit peaks and
overlapping craters. Malupang Wariang, 1 km SW of Dukono's summit
crater complex, contains a 700 x 570 m crater that has also been
active during historical time.

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


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

On 11, 14, and 15 December, INSIVUMEH reported that explosions from
Fuego produced ash plumes that rose to altitudes of 4.1-4.7 km
(13,500-15,400 ft) a.s.l. and drifted 8-12 km W and SW. Incandescence
from the main crater and rumbling noises were noted. Avalanches
descended the S and W flanks. Based on analyses of satellite imagery,
the Washington VAAC reported that on 12 December a gas-and-ash plume
drifted 20 km W. On 15 December, ashfall was reported in areas SW.

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.

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


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

KVERT reported that analyses of satellite imagery revealed a thermal
anomaly from Karymsky during 3 and 6-7 December; ash deposits extended
45 km SE on 6 December. A new lava flow was seen on the S flank on 8
December. Seismic data were seldom available due to technical
problems. 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 9-15 December, 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 multiple locations
between Waikupanaha and areas farther to the W. Towards the beginning
of the reporting period, thermal anomalies detected by satellite and
visual observations revealed occasional active lava flows.
Incandescence was seen almost daily from Pu'u 'O'o crater. The vent in
Halema'uma'u crater continued to produce an off-white plume that
drifted predominantly to the SW, dropping small amounts of ash
downwind. Incandescence originated from a few holes in the deep floor
of the vent cavity. On 13 December, lava ponded on the floor, crusted
over, and blocked the holes. Incandescence was again visible the next
night.

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 4-11 December seismic activity from
Kliuchevskoi was above background levels and lava continued to flow
down the ESE flank. Strombolian activity ejected tephra 200-300 m
above the crater. Gas-and-steam plumes containing small amounts of ash
rose to an altitude of 6.3 km (20,700 ft) a.s.l. and drifted E during
5-9 December. 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


MANAM Northeast of New Guinea (SW Pacific) 4.080°S, 145.037°E; summit
elev. 1807 m

Based on analyses of satellite imagery, the Darwin VAAC reported that
on 12 December an eruption from Manam produced a plume that rose to an
altitude of 3 km (10,000 ft) a.s.l. and drifted 75 km N.

Geologic Summary. The 10-km-wide island of Manam, lying 13 km off the
northern coast of mainland Papua New Guinea, is one of the country's
most active volcanoes. Four large radial valleys extend from the
unvegetated summit of the conical 1807-m-high basaltic-andesitic
stratovolcano to its lower flanks. These "avalanche valleys,"
regularly spaced 90 degrees apart, channel lava flows and pyroclastic
avalanches that have sometimes reached the coast. Two summit craters
are present; both are active, although most historical eruptions have
originated from the southern crater, concentrating eruptive products
during much of the past century into the SE avalanche valley. Frequent
historical eruptions, typically of mild-to-moderate scale, have been
recorded at Manam since 1616. Occasional larger eruptions have
produced pyroclastic flows and lava flows that reached flat-lying
coastal areas and entered the sea, sometimes impacting populated
areas.

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


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

Based on information from the Bogata MWO, the Washington VAAC reported
that on 10 December an ash plume rose to an altitude of 7 km (23,000
ft) a.s.l. and drifted S. Ash was not identified in satellite imagery
due to meteorological clouds in the area. INGEOMINAS reported that
during 9-15 December seismic signals indicated occasional gas-and-ash
emissions. White and bluish gas plumes seen on the web camera rose 2
km. Overflights revealed that the lava dome continued to grow and emit
gases.

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.

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


PACAYA Guatemala 14.381°N, 90.601°W; summit elev. 2552 m

On 11, 14, and 15 December, INSIVUMEH reported that white and blue
fumarolic plumes from Pacaya's MacKenney cone rose up 100 m and
drifted S. Multiple lava flows on the S flank traveled 25-350 m.
Incandescence from one of the inter-crater cones was noted.
Geologic Summary. Eruptions from Pacaya, one of Guatemala's most
active volcanoes, are frequently visible from Guatemala City, the
nation's capital. Pacaya is a complex volcano constructed on the
southern rim of the 14 x 16 km Pleistocene Amatitlan caldera. A
cluster of dacitic lava domes occupies the caldera floor. The Pacaya
massif includes the Cerro Grande lava dome and a younger volcano to
the SW. Collapse of Pacaya volcano about 1,100 years ago produced a
debris-avalanche deposit that extends 25 km onto the Pacific coastal
plain and left an arcuate somma rim inside which the modern Pacaya
volcano (MacKenney cone) grew. During the past several decades,
activity at Pacaya has consisted of frequent Strombolian eruptions
with intermittent lava flow extrusion on the flanks of MacKenney cone,
punctuated by occasional larger explosive eruptions.

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


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

RVO reported that activity from Rabaul caldera's Tavurvur cone
consisted of a few strong explosions towards the beginning of the 4-10
December reporting period, and emissions of gray ash afterwards.
Diffuse white vapor was emitted during quieter intervals. Ash plumes
rose 1 km above the summit and drifted SE towards Tokua and the Tokua
airport, causing suspension of some flights. Based on analyses of
satellite imagery, the Darwin VAAC reported that on 14 December an ash
plume rose to an altitude of 2.1 km (7,000 ft) a.s.l. and drifted 35
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 explosions
from Sakura-jima during 9-15 December produced plumes that rose to
altitudes of 1.8-2.4 km (6,000-8,000 ft) a.s.l. and drifted NE, E, SE,
and S. On 14 December, a pilot reported that an ash plume drifted S at
an altitude of 2.7 km (9,000 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.

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


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

On 11, 14, and 15 December, INSIVUMEH reported that explosions from
Santa María's Santiaguito lava dome complex produced ash plumes that
rose to altitudes of 2.8-3.5 km (9,200-11,500 ft) a.s.l. and drifted W
and SW. Avalanches occasionally descended the SE flank of the dome. On
15 December, explosions generated pyroclastic flows that descended the
E 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 4-11 December seismic activity from
Shiveluch was above background levels, possibly indicating ash plumes
rising to an altitude of 5.5 km (18,000 ft) a.s.l. Fumarolic activity
was seen with a video camera. Analyses of satellite imagery revealed a
large daily thermal anomaly from the lava dome and an ash plume
drifting 85 km SE on 6 December. The Level of Concern Color Code
remained at Orange. Based on information from KEMSD, the Tokyo VAAC
reported that on 13 December an eruption produced a plume that rose to
an altitude of 5.8 km (19,000 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


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

Based on information from JMA, the Tokyo VAAC reported eruptions from
Suwanose-jima on 14 and 15 December. Plumes rose to altitudes of
1.2-1.5 km (4,000-5,000 ft) a.s.l. and drifted E.

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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