Volcano Digest - 15 Aug 2018 to 22 Aug 2018 (#2018-90)

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There are 2 messages totaling 1843 lines in this issue.

Topics of the day:

  1. Smithsonian / USGS Weekly Volcanic Activity Report 15-21 August 2018
  2. Deep Learning Postdoctoral Position at Penn State

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Date:    Wed, 22 Aug 2018 12:37:09 -0700
From:    Sean Peters <speter24@xxxxxxx>
Subject: Smithsonian / USGS Weekly Volcanic Activity Report 15-21 August 2018

 2-2-2-2-2-2-2-2-2-2

From: "Kuhn, Sally" <KUHNS@xxxxxx>

2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2


Sally Kuhn Sennert - Weekly Report Editor (kuhns@xxxxxx)

URL: https://volcano.si.edu/reports_weekly.cfm





New Activity/Unrest: Alaid, Kuril Islands (Russia)  | Kuchinoerabujima,
Ryukyu Islands (Japan)  | Merapi, Central Java (Indonesia)  | Telica,
Nicaragua



Ongoing Activity: Agung, Bali (Indonesia)  | Aira, Kyushu (Japan)  | Ambae,
Vanuatu  | Cleveland, Chuginadak Island (USA)  | Copahue, Central
Chile-Argentina border  | Dukono, Halmahera (Indonesia)  | Ebeko,
Paramushir Island (Russia)  | Fuego, Guatemala  | Ibu, Halmahera
(Indonesia)  | Karymsky, Eastern Kamchatka (Russia)  | Kilauea, Hawaiian
Islands (USA)  | Sabancaya, Peru  | Sheveluch, Central Kamchatka (Russia)
| Sierra Negra, Isla Isabela (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





Alaid  | Kuril Islands (Russia)  | 50.861°N, 155.565°E  | Summit elev. 2285
m



The Tokyo VAAC reported that on 20 August an ash plume from Alaid
identified in satellite images rose to an altitude of 2.7 km (9,000 ft)
a.s.l. and drifted SE.



Geologic Summary. The highest and northernmost volcano of the Kuril
Islands, 2285-m-high Alaid is a symmetrical stratovolcano when viewed from
the north, but has a 1.5-km-wide summit crater that is breached widely to
the south. Alaid is the northernmost of a chain of volcanoes constructed
west of the main Kuril archipelago. Numerous pyroclastic cones dot the
lower flanks of this basaltic to basaltic-andesite volcano, particularly on
the NW and SE sides, including an offshore cone formed during the 1933-34
eruption. Strong explosive eruptions have occurred from the summit crater
beginning in the 18th century. Reports of eruptions in 1770, 1789, 1821,
1829, 1843, 1848, and 1858 were considered incorrect by Gorshkov (1970).
Explosive eruptions in 1790 and 1981 were among the largest in the Kuril
Islands during historical time.



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





Kuchinoerabujima  | Ryukyu Islands (Japan)  | 30.443°N, 130.217°E  | Summit
elev. 657 m



JMA reported that earthquakes at Kuchinoerabujima’s Shindake Crater
typically occur at shallow levels, though on 15 August a swarm of deep
volcanic earthquakes was recorded, prompting JMA to raise the Alert Level
to 4 (on a scale of 1-5). The earthquake hypocenters were about 5 km deep,
below the SW flanks of Shindake, and the maximum magnitude was 1.9. They
occurred at about the same place as the swarm that occurred just before the
May 2015 eruption. Sulfur dioxide emissions had been increasing since the
beginning of August; they were 1,600, 1,000, and 1,200 tons/day on 11, 13,
and 17 August, respectively. No surficial changes in gas emissions or
thermal areas were observed during 16-20 August.



Geologic Summary. A group of young stratovolcanoes forms the eastern end of
the irregularly shaped island of Kuchinoerabujima in the northern Ryukyu
Islands, 15 km west of Yakushima. The Furudake, Shindake, and Noikeyama
cones were erupted from south to north, respectively, forming a composite
cone with multiple craters. The youngest cone, centrally-located Shintake,
formed after the NW side of Furutake was breached by an explosion. All
historical eruptions have occurred from Shintake, although a lava flow from
the S flank of Furutake that reached the coast has a very fresh morphology.
Frequent explosive eruptions have taken place from Shintake since 1840; the
largest of these was in December 1933. Several villages on the 4 x 12 km
island are located within a few kilometers of the active crater and have
suffered damage from eruptions.



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





Merapi  | Central Java (Indonesia)  | 7.54°S, 110.446°E  | Summit elev.
2910 m



PVMBG reported that seismicity at Merapi increased on 18 July, and again on
29 July. On 11 August a large earthquake was detected, and coupled with
rumbling heard by Deles residents, possibly signaled new lava-dome
effusion. Drone photos on 12 August showed a new lava dome growing within
the fracture of the 2010 dome. By 18 August the new dome was 55 m long and
25 m wide, and about 5 m below the 2010 dome surface. The Alert Level
remained at 2 (on a scale of 1-4), and resident were warned to remain
outside of the 3-km exclusion zone.



Geologic Summary. Merapi, one of Indonesia's most active volcanoes, lies in
one of the world's most densely populated areas and dominates the landscape
immediately north of the major city of Yogyakarta. It is the youngest and
southernmost of a volcanic chain extending NNW to Ungaran volcano. Growth
of Old Merapi during the Pleistocene ended with major edifice collapse
perhaps about 2000 years ago, leaving a large arcuate scarp cutting the
eroded older Batulawang volcano. Subsequently growth of the steep-sided
Young Merapi edifice, its upper part unvegetated due to frequent eruptive
activity, began SW of the earlier collapse scarp. Pyroclastic flows and
lahars accompanying growth and collapse of the steep-sided active summit
lava dome have devastated cultivated lands on the western-to-southern
flanks and caused many fatalities during historical time.



Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known
as CVGHM) http://vsi.esdm.go.id/





Telica  | Nicaragua  | 12.606°N, 86.84°W  | Summit elev. 1036 m



SINAPRED reported that on 15 August an explosion at Telica generated an ash
plume that rose 200 m above the crater rim.



Geologic Summary. Telica, one of Nicaragua's most active volcanoes, has
erupted frequently since the beginning of the Spanish era. This volcano
group consists of several interlocking cones and vents with a general NW
alignment. Sixteenth-century eruptions were reported at symmetrical Santa
Clara volcano at the SW end of the group. However, its eroded and breached
crater has been covered by forests throughout historical time, and these
eruptions may have originated from Telica, whose upper slopes in contrast
are unvegetated. The steep-sided cone of Telica is truncated by a
700-m-wide double crater; the southern crater, the source of recent
eruptions, is 120 m deep. El Liston, immediately E, has several nested
craters. The fumaroles and boiling mudpots of Hervideros de San Jacinto, SE
of Telica, form a prominent geothermal area frequented by tourists, and
geothermal exploration has occurred nearby.



Source: Sistema Nacional para la Prevención, Mitigación y Atención de
Desastres (SINAPRED) http://www.sinapred.gob.ni/





Ongoing Activity





Agung  | Bali (Indonesia)  | 8.343°S, 115.508°E  | Summit elev. 2997 m



According to the Darwin VAAC, a webcam recorded a diffuse ash emission from
Agung rising to an altitude of 3.3 km (11,000 ft) a.s.l. and drifting W.
The Alert Level remained at 3 (on a scale of 1-4) and the exclusion zone
was stable at a 4-km radius.



Geologic Summary. Symmetrical Agung stratovolcano, Bali's highest and most
sacred mountain, towers over the eastern end of the island. The volcano,
whose name means "Paramount," rises above the SE caldera rim of neighboring
Batur volcano, and the northern and southern flanks extend to the coast.
The summit area extends 1.5 km E-W, with the high point on the W and a
steep-walled 800-m-wide crater on the E. The Pawon cone is located low on
the SE flank. Only a few eruptions dating back to the early 19th century
have been recorded in historical time. The 1963-64 eruption, one of the
largest in the 20th century, produced voluminous ashfall along with
devastating pyroclastic flows and lahars that caused extensive damage and
many fatalities.



Source: Darwin Volcanic Ash Advisory Centre (VAAC) http://www.bom.gov.au/a
viation/volcanic-ash/darwin-va-advisory.shtml





Aira  | Kyushu (Japan)  | 31.593°N, 130.657°E  | Summit elev. 1117 m



JMA reported that there were four events and nine explosions at Minamidake
crater (at Aira Caldera’s Sakurajima volcano) during 13-20 August, with ash
plumes rising as high as 1.7 km above the crater rim and material ejected
as far as 900 m. Crater incandescence was visible at night. The Alert Level
remained at 3 (on a 5-level scale).



Geologic Summary. The Aira caldera in the northern half of Kagoshima Bay
contains the post-caldera Sakurajima volcano, one of Japan's most active.
Eruption of the voluminous Ito pyroclastic flow accompanied formation of
the 17 x 23 km caldera about 22,000 years ago. The smaller Wakamiko caldera
was formed during the early Holocene in the NE corner of the Aira caldera,
along with several post-caldera cones. The construction of Sakurajima began
about 13,000 years ago on the southern rim of Aira caldera and built an
island that was finally joined to the Osumi Peninsula during the major
explosive and effusive eruption of 1914. Activity at the Kitadake summit
cone ended about 4850 years ago, after which eruptions took place at
Minamidake. 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: Japan Meteorological Agency (JMA) http://www.jma.go.jp/jma/





Ambae  | Vanuatu  | 15.389°S, 167.835°E  | Summit elev. 1496 m



According to news reports all 10,000 residents of Ambae had been evacuated
to Espiritu Santo (W) and Maewo (NE) islands by 14 August.



Geologic Summary. The island of Ambae, also known as Aoba, is a massive
2500 km3 basaltic shield that is the most voluminous volcano of the New
Hebrides archipelago. A pronounced NE-SW-trending rift zone dotted with
scoria cones gives the 16 x 38 km island an elongated form. A broad
pyroclastic cone containing three crater lakes (Manaro Ngoru, Voui, and
Manaro Lakua) is located at the summit within the youngest of at least two
nested calderas, the largest of which is 6 km in diameter. That large
central edifice is also called Manaro Voui or Lombenben volcano.
Post-caldera explosive eruptions formed the summit craters about 360 years
ago. A tuff cone was constructed within Lake Voui (or Vui) about 60 years
later. The latest known flank eruption, about 300 years ago, destroyed the
population of the Nduindui area near the western coast.



Source: Radio New Zealand https://www.radionz.co
.nz/international/pacific-news/364054/vanuatu-s-ambae-island
-completely-evacuated





Cleveland  | Chuginadak Island (USA)  | 52.825°N, 169.944°W  | Summit elev.
1730 m



AVO reported that unrest at Cleveland continued during 15-20 August, though
nothing significant was detected in seismic or infrasound data. Steaming
from the crater was sometimes visible in clear webcam views, and elevated
surface temperatures were occasionally identified in satellite images. The
Aviation Color Code remained at Orange and the Volcano Alert Level remained
at Watch.



Geologic Summary. The beautifully symmetrical Mount Cleveland stratovolcano
is situated at the western end of the uninhabited, dumbbell-shaped
Chuginadak Island. It lies SE across Carlisle Pass strait from Carlisle
volcano and NE across Chuginadak Pass strait from Herbert volcano. Joined
to the rest of Chuginadak Island by a low isthmus, Cleveland is the highest
of the Islands of the Four Mountains group and is one of the most active of
the Aleutian Islands. The native name, Chuginadak, refers to the Aleut
goddess of fire, who was thought to reside on the volcano. Numerous large
lava flows descend the steep-sided flanks. It is possible that some
18th-to-19th century eruptions attributed to Carlisle should be ascribed to
Cleveland (Miller et al., 1998). In 1944 Cleveland produced the only known
fatality from an Aleutian eruption. Recent eruptions have been
characterized by short-lived explosive ash emissions, at times accompanied
by lava fountaining and lava flows down the flanks.



Source: US Geological Survey Alaska Volcano Observatory (AVO)
https://avo.alaska.edu/





Copahue  | Central Chile-Argentina border  | 37.856°S, 71.183°W  | Summit
elev. 2953 m



The Buenos Aires VAAC reported that during 14-15 August diffuse steam
emissions with possible ash were visible in webcam views rising to an
altitude of 3.6 km (12,000 ft) a.s.l.



Geologic Summary. Volcán Copahue is an elongated composite cone constructed
along the Chile-Argentina border within the 6.5 x 8.5 km wide Trapa-Trapa
caldera that formed between 0.6 and 0.4 million years ago near the NW
margin of the 20 x 15 km Pliocene Caviahue (Del Agrio) caldera. The eastern
summit crater, part of a 2-km-long, ENE-WSW line of nine craters, contains
a briny, acidic 300-m-wide crater lake (also referred to as El Agrio or Del
Agrio) and displays intense fumarolic activity. Acidic hot springs occur
below the eastern outlet of the crater lake, contributing to the acidity of
the Río Agrio, and another geothermal zone is located within Caviahue
caldera about 7 km NE of the summit. Infrequent mild-to-moderate explosive
eruptions have been recorded at Copahue since the 18th century.
Twentieth-century eruptions from the crater lake have ejected pyroclastic
rocks and chilled liquid sulfur fragments.



Source: Buenos Aires Volcanic Ash Advisory Center (VAAC)
http://www.smn.gov.ar/vaac/buenosaires/productos.php





Dukono  | Halmahera (Indonesia)  | 1.693°N, 127.894°E  | Summit elev. 1229 m



Based on satellite data, wind model data, and notices from PVMBG, the
Darwin VAAC reported that during 15-21 August ash plumes from Dukono rose
to altitudes of 1.8-2.4 km (6,000-8,000 ft) a.s.l. and drifted NNW, NE, and
E.



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 north-flank cone
of Gunung Mamuya. This complex volcano presents a broad, low profile with
multiple summit peaks and overlapping craters. Malupang Wariang, 1 km SW of
the 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.bom.gov.au/a
viation/volcanic-ash/darwin-va-advisory.shtml





Ebeko  | Paramushir Island (Russia)  | 50.686°N, 156.014°E  | Summit elev.
1103 m



Volcanologists in Severo-Kurilsk (Paramushir Island), about 7 km E of
Ebeko, observed explosions during 11-17 August that sent ash plumes as high
as 4.5 km (14,800 ft) a.s.l. An ash plume drifted 52 km SE during 10-11
August, and a thermal anomaly was identified in satellite images on 12
August. The Aviation Color Code remained at Orange (the second highest
level on a four-color scale).



Geologic Summary. The flat-topped summit of the central cone of Ebeko
volcano, one of the most active in the Kuril Islands, occupies the northern
end of Paramushir Island. Three summit craters located along a SSW-NNE line
form Ebeko volcano proper, at the northern end of a complex of five
volcanic cones. Blocky lava flows extend west from Ebeko and SE from the
neighboring Nezametnyi cone. The eastern part of the southern crater
contains strong solfataras and a large boiling spring. The central crater
is filled by a lake about 20 m deep whose shores are lined with steaming
solfataras; the northern crater lies across a narrow, low barrier from the
central crater and contains a small, cold crescentic lake. Historical
activity, recorded since the late-18th century, has been restricted to
small-to-moderate explosive eruptions from the summit craters. Intense
fumarolic activity occurs in the summit craters, on the outer flanks of the
cone, and in lateral explosion craters.



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





Fuego  | Guatemala  | 14.473°N, 90.88°W  | Summit elev. 3763 m



INSIVUMEH reported that during 18-21 August explosions at Fuego generated
ash plumes that rose as high as 850 m above the crater and drifted 12 km
NW, W, and SW. Incandescent material was ejected 150 m above the crater
rim, and caused avalanches of material within the crater area and down
drainages on the flanks. According to CONRED, as of 22 August, the number
of people confirmed to have died due to the 3 June pyroclastic flows was
169, and 256 remained missing.



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 3763-m-high Fuego and its twin volcano to the north, Acatenango.
Construction of Meseta dates back to about 230,000 years and continued
until the late Pleistocene or early Holocene. Collapse of Meseta may have
produced the massive Escuintla debris-avalanche deposit, which extends
about 50 km onto the Pacific coastal plain. Growth of the modern Fuego
volcano followed, continuing the southward migration of volcanism that
began at Acatenango. In contrast to the mostly andesitic Acatenango,
eruptions at Fuego have become more mafic with time, and most historical
activity has produced basaltic rocks. Frequent vigorous historical
eruptions have been recorded since the onset of the Spanish era in 1524,
and have produced major ashfalls, along with occasional pyroclastic flows
and lava flows.



Sources: Coordinadora Nacional para la Reducción de Desastres (CONRED)
http://conred.gob.gt/;

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





Ibu  | Halmahera (Indonesia)  | 1.488°N, 127.63°E  | Summit elev. 1325 m



PVMBG reported that at 1742 on 20 August an event at Ibu generated an ash
plume that rose 1.2 km above the crater rim. The Alert Level remained at 2
(on a scale of 1-4), and the public was warned to stay at least 2 km away
from the active crater, and 3.5 km away on the N side.



Geologic Summary. The truncated summit of Gunung Ibu stratovolcano along
the NW coast of Halmahera Island has large nested summit craters. The inner
crater, 1 km wide and 400 m deep, contained several small crater lakes
through much of historical time. The outer crater, 1.2 km wide, is breached
on the north side, creating a steep-walled valley. A large parasitic cone
is located ENE of the summit. A smaller one to the WSW has fed a lava flow
down the W flank. A group of maars is located below the N and W flanks.
Only a few eruptions have been recorded in historical time, the first a
small explosive eruption from the summit crater in 1911. An eruption
producing a lava dome that eventually covered much of the floor of the
inner summit crater began in December 1998.



Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known
as CVGHM) http://vsi.esdm.go.id/





Karymsky  | Eastern Kamchatka (Russia)  | 54.049°N, 159.443°E  | Summit
elev. 1513 m



KVERT reported that a thermal anomaly over Karymsky was identified in
satellite images on 10 August; cloud cover prevented views during 11-17
August. The Aviation Color Code remained at Orange (the second highest
level on a four-color scale).



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 during the early Holocene. The caldera cuts
the south side of the Pleistocene Dvor volcano and is located outside the
north margin of the large mid-Pleistocene Polovinka caldera, which contains
the smaller Akademia Nauk and Odnoboky calderas. Most seismicity preceding
Karymsky eruptions originated beneath Akademia Nauk caldera, located
immediately south. The caldera enclosing Karymsky formed about 7600-7700
radiocarbon years ago; construction of the stratovolcano began about 2000
years later. The latest eruptive period began about 500 years ago,
following a 2300-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.



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





Kilauea  | Hawaiian Islands (USA)  | 19.421°N, 155.287°W  | Summit elev.
1222 m



On 17 August HVO lowered the Alert Level for Kilauea to Watch (the Aviation
Color Code remained at Orange), noting reduced activity over the previous
several days. Specifically, no collapse events had occurred at the summit
since 2 August, lava ceased flowing in the channel from the Fissure 8 cone
on 6 August, seismicity and ground deformation at the summit were
negligible, and the combined rate of sulfur dioxide emission from the
summit and the LERZ were lower than any time since late 2007. The small
lava pond in Fissure 8 had crusted over by 17 August, with no observed
incandescence. Lava continued to ooze into the ocean at a few areas,
causing minimal laze plumes. During an overflight on 20 August gas jets
ejected spatter from a small incandescent area deep within the Fissure 8
cone.



Geologic Summary. Kilauea, which overlaps the E flank of the massive Mauna
Loa shield volcano, has been Hawaii's most active volcano during historical
time. Eruptions are prominent in Polynesian legends; written documentation
extending back to only 1820 records frequent summit and flank lava flow
eruptions that were interspersed with periods of long-term lava lake
activity that lasted until 1924 at Halemaumau crater, within the summit
caldera. The 3 x 5 km caldera was formed in several stages about 1500 years
ago and during the 18th century; eruptions have also originated from the
lengthy East and SW rift zones, which extend to the sea on both sides of
the volcano. About 90% of the surface of the basaltic shield volcano is
formed of lava flows less than about 1100 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 km2,
destroying nearly 200 houses and adding new coastline to the island.



Source: US Geological Survey Hawaiian Volcano Observatory (HVO)
https://volcanoes.usgs.gov/observatories/hvo/





Sabancaya  | Peru  | 15.787°S, 71.857°W  | Summit elev. 5960 m



Observatorio Vulcanológico del Sur del IGP (OVS-IGP) and Observatorio
Vulcanológico del INGEMMET (OVI) reported that explosions at Sabancaya
averaged 27 per day during 13-19 August. Hybrid earthquakes were infrequent
and low-magnitude. Gas-and-ash plumes rose as high as 3.7 km above the
crater rim and drifted 50 km SE, E, and NE. The MIROVA system detected nine
thermal anomalies, and on 19 August the sulfur dioxide gas flux was high at
3,100 tons/day. The report noted that the public should not approach the
crater within a 12-km radius.



Geologic Summary. Sabancaya, located in the saddle NE of Ampato and SE of
Hualca Hualca volcanoes, is the youngest of these volcanic centers and the
only one to have erupted in historical time. The oldest of the three,
Nevado Hualca Hualca, is of probable late-Pliocene to early Pleistocene
age. The name Sabancaya (meaning "tongue of fire" in the Quechua language)
first appeared in records in 1595 CE, suggesting activity prior to that
date. Holocene activity has consisted of Plinian eruptions followed by
emission of voluminous andesitic and dacitic lava flows, which form an
extensive apron around the volcano on all sides but the south. Records of
historical eruptions date back to 1750.



Sources: Instituto Geológico Minero y Metalúrgico (INGEMMET)
http://www.ingemmet.gob.pe/;

Instituto Geofísico del Perú (IGP) http://www.igp.gob.pe/





Sheveluch  | Central Kamchatka (Russia)  | 56.653°N, 161.36°E  | Summit
elev. 3283 m



KVERT reported that satellite images showed a thermal anomaly over
Sheveluch during 12-13 August; cloudy weather prevented views of the
volcano on the other days during 10-17 August. The Aviation Color Code
remained at Orange (the second highest level on a four-color scale).



Geologic Summary. The high, isolated massif of Sheveluch volcano (also
spelled Shiveluch) rises above the lowlands NNE of the Kliuchevskaya
volcano group. The 1300 km3 volcano is one of Kamchatka's largest and most
active volcanic structures. The summit of roughly 65,000-year-old Stary
Shiveluch is truncated by a broad 9-km-wide late-Pleistocene caldera
breached to the south. Many lava domes dot its outer flanks. The Molodoy
Shiveluch lava dome complex was constructed during the Holocene within the
large horseshoe-shaped caldera; Holocene lava dome extrusion also took
place on the flanks of Stary Shiveluch. At least 60 large eruptions have
occurred during the Holocene, making it the most vigorous andesitic volcano
of the Kuril-Kamchatka arc. Widespread tephra layers from these eruptions
have provided valuable time markers for dating volcanic events in
Kamchatka. Frequent collapses of dome complexes, most recently in 1964,
have produced debris avalanches whose deposits cover much of the floor of
the breached caldera.



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





Sierra Negra  | Isla Isabela (Ecuador)  | 0.83°S, 91.17°W  | Summit elev.
1124 m



IG reported that lava effusion at Sierra Negra continued at variable
intensities. The most intense pulses, recorded on 4 and 9 August, were
accompanied by major episodes of seismic tremor; activity slightly declined
after 9 August. On 15 August satellite images showed lava from Fissure 4
continuing to enter the ocean.



Geologic Summary. The broad shield volcano of Sierra Negra at the southern
end of Isabela Island contains a shallow 7 x 10.5 km caldera that is the
largest in the Galápagos Islands. Flank vents abound, including cinder
cones and spatter cones concentrated along an ENE-trending rift system and
tuff cones along the coast and forming offshore islands. The 1124-m-high
volcano is elongated in a NE direction. Although it is the largest of the
five major Isabela volcanoes, it has the flattest slopes, averaging less
than 5 degrees and diminishing to 2 degrees near the coast. A sinuous
14-km-long, N-S-trending ridge occupies the west part of the caldera floor,
which lies only about 100 m below its rim. Volcán de Azufre, the largest
fumarolic area in the Galápagos Islands, lies within a graben between this
ridge and the west caldera wall. Lava flows from a major eruption in 1979
extend all the way to the north coast from circumferential fissure vents on
the upper northern flank. Sierra Negra, along with Cerro Azul and Volcán
Wolf, is one of the most active of Isabela Island volcanoes.



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

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------------------------------

Date:    Wed, 22 Aug 2018 12:36:59 -0700
From:    Sean Peters <speter24@xxxxxxx>
Subject: Deep Learning Postdoctoral Position at Penn State

 1-1-1-1-1-1-1-1-1-1

From: Christelle Wauthier <cuw25@xxxxxxx>

1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1


The College of Earth and Mineral Sciences, at The Pennsylvania State
University, invites applications for a post-doctoral research position in
adapting deep learning methods for use in the earth sciences. This position
will provide the successful candidate with experience conducting
cross-cutting research working under the supervision of three faculty
members Dr. Guido Cervone from the Dept. of Geography, Dr. Christelle
Wauthier from the Dept. of Geosciences, and Dr. Melissa Gervais from the
Dept. of Meteorology and Atmospheric Sciences. They will conduct
collaborative research that will advance the use of deep learning within
the earth sciences through its application to several scientific questions
that require the identification of patterns of spatio-temporal variability.
The successful candidate will have access to significant computing
resources and be involved in the high performance computing activities of
the Institute for CyberScience at Penn State. Applicants must hold a Ph.D
in Computer Science, Mathematics, Statistics, Geoscience, Atmospheric
Science, Geography or other related field with a strong Computational
Science component. Experience with advanced programing, deep learning, or
machine learning methods, an interest in conducting cross-cutting research,
and a willingness to work in a multidisciplinary team is highly desired.
This position will be funded for 18-months from the date of hire, with a
strong possibility of refunding. Applicants must upload a letter of
research interest, a CV, and contact information for three references.
Review of applications will begin immediately and continue until the
position is filled. For any questions please contact Melissa Gervais at
mmg62@xxxxxxx, Guido Cervone at cervone@xxxxxxx, or Christelle Wauthier at
cuw25@xxxxxxx.


The job posting is located at:
https://psu.jobs/job/79865


Sincerely,
Christelle Wauthier

==============================================================

Volcano Listserv is a collaborative venture among Arizona State University (ASU), Portland State University (PSU), the Global Volcanism Program (GVP) of the Smithsonian Institution's National Museum of Natural History, and the International Association for Volcanology and Chemistry of the Earth's Interior (IAVCEI).

ASU - http://www.asu.edu/
PSU - http://pdx.edu/
GVP - http://www.volcano.si.edu/
IAVCEI - http://www.iavcei.org/

To unsubscribe from the volcano list, send the message:
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To contribute to the volcano list, send your message to:
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End of Volcano Digest - 15 Aug 2018 to 22 Aug 2018 (#2018-90)
*************************************************************




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