GVP/USGS Weekly Volcanic Activity Report 1-7 Feb. 2006

[Date Prev][Date Next][Thread Prev][Thread Next][Date Index][Thread Index]

 



*******************************************************
GVP/USGS Weekly Volcanic Activity Report 1-7 Feb. 2006
*******************************************************
From: Gari Mayberry <mayberry@xxxxxxxxxxxxxx>
 

GVP/USGS Weekly Volcanic Activity Report
1-7 February 2006
http://www.volcano.si.edu/reports/usgs/

New Activity/Unrest: | Cleveland, USA 

Ongoing Activity: | Augustine, USA | Colima, México | Fuego, Guatemala | 
Galeras, Colombia | Karymsky, Russia | Kilauea, USA | Popocatépetl, México | 
Sakura-jima, Japan | Santa Ana, El Salvador | Santa María, Guatemala | 
Soufrière Hills, Montserrat | St. Helens, USA | Suwanose-jima, Japan | 
Tungurahua, Ecuador


New Activity/Unrest  

CLEVELAND Aleutian Islands, USA 52.82°N, 169.95°W; summit elev. 1,730 m; All 
times are local (= UTC - 9 hours)

An ash cloud emitted from Cleveland was detected on satellite imagery 
beginning at 0757 on 6 February, leading AVO to increase the Concern Color 
Code to Red from an unassigned code (Cleveland does not normally have a 
Concern Color Code because it is not seismically monitored, therefore no 
definitive information about background activity is available) 
<http://www.avo.alaska.edu/color_codes.php>. An image at 0900 on the same day 
showed a small ash cloud ~130 km ESE of the volcano. Initial data suggested 
that the cloud was at a height of ~6.7 km (22,000 ft) a.s.l. The ash cloud 
detached from the volcano and there was no indication of continuous ash 
emission. Ash had largely dissipated on satellite imagery by 1341. AVO 
received no information about additional ash emissions, so they decreased the 
Concern Color Code to Orange around 1655 on 6 February.

Background. The 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.

Sources: Alaska Volcano Observatory 
http://www.avo.alaska.edu/activity/avoreport.php?view=update, 
Anchorage Volcanic Ash Advisory Center 
http://www.ssd.noaa.gov/VAAC/OTH/AK/messages.html, 
Washington Volcanic Ash Advisory Center 
http://www.ssd.noaa.gov/VAAC/messages.html 

Cleveland Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1101-24-


Ongoing Activity 


AUGUSTINE  SW Alaska, USA  59.363°N, 153.43°W; summit elev. 1,252 m

During 1-7 February, occasional pyroclastic flows continued to travel down 
Augustine's flanks and low-level ash plumes reached no higher than 4.6 km 
(15,000 ft) a.s.l. on satellite imagery. On 3 February, seismicity decreased 
significantly, but remained above background levels. Seismicity remained low 
throughout the remainder of the report period. Satellite imagery from the 
evening of 6 February showed a persistent thermal signal and occasional light 
ash emission. On 7 February, a steam plume was visible rising ~150 m (~500 ft) 
above the summit. AVO warned that further explosive activity producing ash 
clouds to heights over 7.6 km (25,000 ft) may still occur with little or no 
warning. Augustine remained at Concern Color Code Orange 
<http://www.avo.alaska.edu/color_codes.php>. 

Background. Augustine volcano, rising above Kamishak Bay in the southern Cook 
Inlet about 290 km SW of Anchorage, is the most active volcano of the eastern 
Aleutian arc. It consists of a complex of overlapping summit lava domes 
surrounded by an apron of volcaniclastic debris that descends to the sea on 
all sides. Few lava flows are exposed; the flanks consist mainly of debris-
avalanche and pyroclastic-flow deposits formed by repeated collapse and 
regrowth of the volcano's summit. The latest episode of edifice collapse 
occurred during Augustine's largest historical eruption in 1883; subsequent 
dome growth has restored the volcano to a height comparable to that prior to 
1883. The oldest dated volcanic rocks on Augustine are more than 40,000 years 
old. At least 11 large debris avalanches have reached the sea during the past 
1800-2000 years, and five major pumiceous tephras have been erupted during 
this interval.  Historical eruptions have typically consisted of explosive 
activity with emplacement of pumiceous pyroclastic-flow deposits followed by 
lava dome extrusion with associated block-and-ash flows.

Sources: Alaska Volcano Observatory 
http://www.avo.alaska.edu/activity/avoreport.php?view=update, 
Anchorage Volcanic Ash Advisory Center 
http://www.ssd.noaa.gov/VAAC/OTH/AK/messages.html

Augustine Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1103-01-


COLIMA Western México 19.514°N, 103.62°W; summit elev. ~3,850 m

During 4-7 February, small explosions occurred at Colima. The highest 
resultant ash plume reached ~8.5 km (28,000 ft) a.s.l. on 4 February. 

Background. The Colima volcanic complex is the most prominent volcanic center 
of the western Mexican Volcanic Belt. It consists of two southward-younging 
volcanoes, Nevado de Colima (the 4,320 m high point of the complex) on the N 
and the historically active Volcán de Colima on the S. Volcán de Colima (also 
known as Volcán Fuego) is a youthful stratovolcano constructed within a 5-km-
wide caldera, breached to the S, that has been the source of large debris 
avalanches. Major slope failures have occurred repeatedly from both the Nevado 
and Colima cones, and have produced a thick apron of debris-avalanche deposits 
on three sides of the complex. Frequent historical eruptions date back to the 
16th century.  Occasional major explosive eruptions (most recently in 1913) 
have destroyed the summit and left a deep, steep-sided crater that was slowly 
refilled and then overtopped by lava dome growth.

Sources: Universidad de Colima http://www.ucol.mx/volcan/, 
Washington Volcanic Ash Advisory Center 
http://www.ssd.noaa.gov/VAAC/messages.html

Colima Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1401-04=


FUEGO Guatemala 14.47°N, 90.88°W; summit elev. 3,763 m

During 1-3 February, weak-to-moderate explosions occurred at Fuego. Shock 
waves from the explosions were sometimes felt in villages near the volcano. 
Small avalanches of volcanic material traveled down Fuego's S and W flanks. 

Background. 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, Meterologia, e 
Hidrologia http://www.insivumeh.gob.gt/principal/alertas.htm

Fuego Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1402-09=


GALERAS Colombia 1.22°N, 77.37°W; summit elev. 4,276 m

During 30 January to 6 February, seismicity continued at Galeras, with an 
average of 200 small earthquakes occurring per day. In addition, slight 
deformation was recorded at the volcano. A flux of about 300 metric tons of 
sulfur dioxide was measured per day. Strong degassing occurred in several 
sectors of the active cone and around the lava dome. Steam rose to ~900 m 
above the volcano (or ~17,000 ft a.s.l.). Galeras remained at Alert Level 3 
("changes in the behavior of volcanic activity have been noted"). 

Background. 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. Long-term 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 
http://www.ingeominas.gov.co/tmsingeominas/ModuloPublicacionPortal/PublicacionP
ortal.asp

Galeras Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1501-08= 


KARYMSKY Kamchatka Peninsula, Russia 54.05°N, 159.43°E; summit elev. 1,536 m

According to reports from pilots of local airlines, ash emissions from 
Karymsky rose to 4-5 km (13,100-16,400 ft) a.s.l. during 30-31 January. The 
ash plumes extended 13-29 km from the volcano to the SW and SE, respectively. 
A thermal anomaly was visible at the lava dome during 27 January to 3 
February, except when the volcano was obscured by clouds on the 28th.  KVERT 
warned that activity from the volcano could affect nearby low-flying aircraft. 
Karymsky remained at Concern Color Code Orange 
<http://www.avo.alaska.edu/avo4/updates/color_code.html>.  

Background. 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 
http://www.kcs.iks.ru/ivs/kvert/updates.shtml

Karymsky Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1000-13=  


KILAUEA Hawaii, USA 19.43°N, 155.29°W; summit elev. 1,222 m

During 2-7 February, lava from Kilauea continued to enter the sea at the East 
Lae`apuki area and surface lava flows were visible on the Pulama pali fault 
scarp. Background volcanic tremor was near normal levels at Kilauea's summit, 
with numerous shallow earthquakes continuing to occur at the summit and upper 
E rift zone. Volcanic tremor reached moderate levels at Pu`u `O`o. Small 
amounts of inflation and deflation occurred at the volcano during the report 
period. 

Background. 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 by lava flows less than about 1,100 years old; 
70% of the volcano's surface is younger than 600 years. The latest Kilauea 
eruption began in January 1983 along the E rift zone. This long-term ongoing 
eruption from Pu`u `O`o-Kupaianaha has produced lava flows that have traveled 
11-12 km from the vents to the sea, paving about 104 km2 of land on the S 
flank of Kilauea and building more than 200 hectares of new land. 

Source: US Geological Survey Hawaiian Volcano Observatory 
http://volcanoes.usgs.gov/update.html

Kilauea information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1302-01-


POPOCATÉPETL México 19.02°N, 98.62°W; summit elev. 5,426 m

During 1-7 February, several small-to-moderate emissions of steam, gas, and 
small amounts of ash occurred at Popocatépetl. On the 4th, an explosion 
produced a plume that rose to ~6.7 km (22,000 ft) a.s.l. 

Background. 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.

Sources: Centro Nacional de Prevencion de Desastres 
http://www.cenapred.unam.mx/, Washington Volcanic Ash Advisory Center 
http://www.ssd.noaa.gov/VAAC/messages.html 

Popocatépetl Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1401-09=


SAKURA-JIMA Kyushu, Japan 31.58°N, 130.67°E; summit elev. 1,117 m

Based on information from JMA, the Tokyo VAAC reported that an explosion at 
Sakura-jima on 5 February produced a plume that reached a height of ~1.8 km 
(6,000 ft) a.s.l. and drifted N. 

Background. 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 
http://www.ssd.noaa.gov/VAAC/OTH/JP/messages.html

Sakura-jima Information from the Global Volcanism Program 
http://www.volcano.si.edu/gvp/world/volcano.cfm?vnum=0802-08=


SANTA ANA El Salvador 13.853°N, 89.630°W; summit elev. 2,365 m

During 27 January- 3 February, volcanic activity was at moderate levels at 
Santa Ana. On the 2nd, there was an increase in seismicity at the volcano, 
possibly related to an earthquake on the coast of Guatemala. There was also an 
increase in the sulfur-dioxide flux, with an average of 2,000 metric tons 
measured daily. Steam plumes rose to low levels above the volcano. The Alert 
Level at Santa Ana remained at Red, the highest level, within a 5-km radius 
around the volcano's summit crater.

Background. Santa Ana, El Salvador's highest volcano, is a massive 
stratovolcano immediately W of Coatepeque caldera. Collapse of the volcano 
during the late Pleistocene or early Holocene produced a massive debris 
avalanche that swept into the Pacific, forming the Acajutla Peninsula. 
Reconstruction of the volcano rapidly filled the collapse scarp. The broad 
summit of the volcano is cut by several crescentic craters, and a series of 
parasitic vents and cones have formed along a 20-km-long fissure system that 
extends from near the town of Chalchuapa NNW of the volcano to the San 
Marcelino and Cerro Chino cinder cones on the SE flank. Historical activity, 
largely consisting of small-to-moderate explosive eruptions from both summit 
and flank vents, has been documented since the 16th century. The San Marcelino 
cinder cone on the SE flank produced a lava flow in 1722 that traveled 11 km 
to the E. 

Source: Servicio Nacional de Estudios Territoriales http://www.snet.gob.sv/

Santa Ana Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1403-02= 


SANTA MARÍA Guatemala 14.756°N, 91.552°W; summit elev. 3,772 m; All times are 
local (= UTC - 6 hours)

During 1-3 February, weak-to-moderate explosions occurred at Santa María's 
Santiaguito lava-dome complex, producing plumes that rose to a maximum height 
of 1 km above the volcano (or 15,650 ft a.s.l.). On 1 February at 0657 and 
0708, moderate explosions occurred that were accompanied by pyroclastic flows. 
Lava extrusion at Caliente Dome produced block-and-ash flows that descended 
the dome's S,E, and W sides. 

Background. 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, Meterologia, e 
Hidrologia http://www.insivumeh.gob.gt/geofisica/boletin%20formato.htm

Santa María Information from the Global Volcanism Program
http://www.volcano.si.edu/world/volcano.cfm?vnum=1402-03= 


SOUFRIÈRE HILLS Montserrat, West Indies 16.72°N, 62.18°W; summit elev. 1,052 m

Volcanic and seismic activity at Soufrière Hills were at elevated levels 
during 27 January to 3 February. Images taken by a remote camera at the 
beginning of the report period indicated that the lava dome continued to grow 
over a broad sector extending from the SW around to the NE. A pair of spines 
was observed on the SE side of the dome on 29 January, although both these and 
the fin-like structures (relatively thin, vertical planar spines) on the SE 
flank of the dome collapsed during the report period. Numerous small rockfalls 
were observed emanating from the S,E, and NE flanks of the lava dome, adding 
to the talus in the upper reaches of the Tar River Valley. Continued lava-dome 
growth was observed, particularly at the southern end, which was higher than 
the northern end of the dome. The sulfur-dioxide flux averaged 594 metric tons 
per day. 

Background. 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 east, was formed 
during an eruption about 4000 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 http://www.mvo.ms/

Soufrière Hills Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1600-05=  


ST. HELENS Washington, USA 46.20°N, 122.18°W; summit elev. 2,549 m

Growth of the new lava dome inside the crater of Mount St. Helens continued 
during 1-7 February, accompanied by low rates of seismicity, low emissions of 
steam and volcanic gases, and minor production of ash. Occasional clear views 
of the volcano revealed incandescence on the currently growing lava lobe and a 
few incandescent rockfalls. St Helens remained at Volcano Advisory (Alert 
Level 2); aviation color code Orange.
  
Background. Prior to 1980, Mount St. Helens formed a conical, youthful volcano 
sometimes known as the Fuji-san of America.  During the 1980 eruption the 
upper 400 m of the summit was removed by slope failure, leaving a 2 x 3.5 km 
horseshoe-shaped crater now partially filled by a lava dome.  Mount St. Helens 
was formed during nine eruptive periods beginning about 40-50,000 years ago, 
and has been the most active volcano in the Cascade Range during the 
Holocene.  The modern edifice was constructed during the last 2,200 years, 
when the volcano produced basaltic as well as andesitic and dacitic products 
from summit and flank vents.  Historical eruptions in the 19th century 
originated from the Goat Rocks area on the N flank, and were witnessed by 
early settlers.

Source: USGS Cascades Volcano Observatory 
http://vulcan.wr.usgs.gov/Volcanoes/MSH/CurrentActivity/framework.html

St. Helens Information from the Global Volcanism Program 
http://www.volcano.si.edu/world/volcano.cfm?vnum=1201-05- 


SUWANOSE-JIMA Ryukyu Islands, Japan 29.53°N, 129.72°E; summit elev. 799 m

Based on information from JMA, the Tokyo VAAC reported that several explosions 
occurred at Suwanose-jima during 6-7 February. A resultant plume from an 
explosion on the 6th rose to 1.2 km (4,000 ft) a.s.l. and extended NW. 

Background. 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 E 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 around 
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 
http://www.ssd.noaa.gov/VAAC/OTH/JP/messages.html 

Suwanose-jima Information from the Global Volcanism Program
http://www.volcano.si.edu/world/volcano.cfm?vnum=0802-03= 


TUNGURAHUA Ecuador 1.47°S, 78.44°W; summit elev. 5,023 m; All times are local 
(= UTC - 5 hours)

During 1-7 February, emissions of gas and ash occurred at Tungurahua. On 5 
February at 0600, a moderate explosion occurred. A steam plume, with a small 
amount of ash, rose to ~1 km above the volcano (or 19,750 a.s.l.) and drifted 
SW. Light rainfall on the 7th generated a lahar in La Pampa area NW of the 
volcano. 

Background. 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 been 
restricted to 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 Geofisico-Escuela Poltecnica Nacional 
http://www.igepn.edu.ec/vulcanologia/tungurahua/actividad/informet.htm, 
Washington Volcanic Ash Advisory Center 
http://www.ssd.noaa.gov/VAAC/messages.html

Tungurahua Information from the Global Volcanism Program
http://www.volcano.si.edu/world/volcano.cfm?vnum=1502-08=


*********************************************************
Gari Mayberry
US Geological Survey/Global Volcanism 
Program                                                                    
Smithsonian Institution
National Museum of Natural History MRC-119
Dept. of Mineral Sciences               
Washington, DC 20560-0119

Phone: 202.633.1805 
Fax: 202.357.2476
mayberry@xxxxxxxxxxxxxx
http://www.volcano.si.edu/reports/usgs/
**********************************************************  

==============================================================
To unsubscribe from the volcano list, send the message:
signoff volcano
to: listserv@xxxxxxx, or write to: volcano-request@xxxxxxxx

To contribute to the volcano list, send your message to:
volcano@xxxxxxxx  Please do not send attachments.
==============================================================

[Index of Archives]     [Yosemite Backpacking]     [Earthquake Notices]     [USGS News]     [Yosemite Campgrounds]     [Steve's Art]     [Hot Springs Forum]

  Powered by Linux