Volcano news - Archive Nr. 22

Soufriere Hills Volcano, Montserrat, Eastern Caribbean (Philippa)
This week we remember the 21st anniversary of an eruption of Soufriere Hills Volcano, in which 19 people lost their lives and 5 others were critically injured.

Image of a pyroclastic density current on the flanks of Soufriere Hills Volcano - taken during a helicopter overflight - via Paul Cole (@PaulCole23 - formerly of Montserrat Volcano Observatory) on 25th June 1997 / via TiVonne Howe (@tivonnehowe)

The volcano on this Eastern Caribbean island had re-activated for the first time in living memory in 1995. With activity in the form of lava dome growth / collapses, explosive eruptions and pyroclastic density currents (PDCs - avalanches of hot volcanic gases, ash, and other fall-out from eruption plumes) intensifying again in 1997, the majority of Montserrat's then-12,000 inhabitants had already been evacuated from the southern half of the island, including the (former) capital of Plymouth, which became obliterated by a series of PDCs.

Some of the inhabitants permanently evacuated, either to other Caribbean islands, the U.S. or the U.K. For those who were temporarily evacuated to the undeveloped northern part of Montserrat though, where conditions rapidly degenerated, the main problem was logistics in order to bring in external food supplies. With the main port in Plymouth out of action, it was (still is!) difficult for ships to dock elsewhere on the island, and the old airport in Trants** was limited in its capacity. For this reason, residents who made a living from agriculture were granted permission in the day-time to enter the exclusion zone (southern half of Montserrat) in order to tend their farms to produce food.

The majority of the 19 people who lost their lives on the afternoon of 25th June were such people tending their land in close proximity to Soufriere Hills Volcano.*** An immediate evacuation of the area they were in had been announced on the main radio station for the island, but either these people did not have their radios switched on, or had ventured back into the exclusion zone in order to try and rescue family members.

*** Volcanic ash makes soil fertile, which is good for farming, and hence why in many countries around the world people live near volcanoes.

The National Geographic programme 'Seconds From Disaster (series 3, episode 19) explains the events of 25th June 1997.

Watch from around 29 minutes into the programme where Delia Ponde explains the lucky escape that she and her family had.

In total, there have been 6 phases of eruptive activity at Soufriere Hills Volcano since 1995, but the June 25th eruption from 1997 is the only one in which there have been fatalities. The southern half and parts of eastern Montserrat remain an exclusion zone, and there are now only 4,000 residents on the island.

** Video footage of former capital Plymouth shot in 2009 by the British volcanologists who were based at Montserrat Volcano Observatory at that time. The airport runway that features in this, based in the area of Trants on the east of Montserrat, was inundated by PDCs and lahars during the last eruption in 2010. I did fieldwork there with MVO in the summer of 2011. Only the roof and antenna of the old airport tower are still visible, and the volcanic deposits (mostly ash) at less than a metre's depth were still over 80 degrees Celcius.

via Geoff Mackley / YouTube


Weekly Volcanic Activity Report: 20 - 26 June 2018
Via Smithsonian Institution - Global Volcanism Program / US Geological Survey's Volcano Hazards Program

Fernandina | Ecuador
On 21 June Parque Nacional Galapagos reported that lava flows at Fernandina were no longer reaching the ocean, though white plumes continued to rise from flows at the coastline.

Great Sitkin | Andreanof Islands, USA
The Alaska Volcano Observatory (AVO) reported continuing low-level unrest at Great Sitkin during 20-26 June; seismic activity remained at or near background levels. A recently analyzed satellite image acquired on 11 June, one day after short-duration explosive event was recorded, showed a minor ash deposit on the snow extending 2 km from a vent in the summit crater. The Aviation Color Code remained at Yellow and the Volcano Alert Level remained at Advisory.

Ibu | Halmahera, Indonesia
(Indonesian volcano monitoring agency) PVMBG reported that at 08:57 on 21 June an event at Ibu generated an ash plume that rose at least 600 m above the crater rim and drifted north. Signals indicating that an explosion and rock avalanches were detected in seismic data. During 22-26 June ash plumes rose as high as 850 m and drifted west-north-west and west. 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 north side.

Kadovar | Papua New Guinea
According to the Darwin Volcanic Ash Advisory Centre an ash plume from Kadovar identified by a pilot and in satellite images rose to an altitude of 1.8 km (6,000 ft.) above sea level on 20 June and drifted west.

Krakatau | Indonesia
(Indonesian volcano monitoring agency) PVMBG and (national disaster response) BNPB reported that an eruption at Anak Krakatau began on 18 June, along with increased seismicity, and reminded residents that the Alert Level remained at 2 (on a scale of 1-4); visitors were warned not to approach the volcano within 1 km of the crater. Foggy conditions hampered visual observations during 19-20 June, but on 21 June grey plumes were observed rising 100-200 m above the summit. An even at 07:14 on 25 June produced a dense ash plume that rose about 1 km and drifted north.

Sierra Negra | Isla Isabela, Ecuador
On 22 June (Ecuadorian volcano monitoring agency) Instituto Geofisico (IG) reported increased seismic activity at Sierra Negra on the southern end of Isabela Island; the largest event, a M4.2, was recorded at 06:24 and felt in El Cura and San Joaquin, north east of the volcano. A M5.3 earthquake was detected at 03:15 on 26 June, occurring at a depth of 5.3 km below Sierra Negra. The event was strongly felt on the upper flanks and in Puerto Villamil (23 km south east). Several aftershocks and subsequent tremor were recorded. An earthquake swarm began at 11:17, characterized by events located 3-5 km depth. A M4.2 earthquake was recorded at 13:38, and followed by increasing amplitudes of seismic and infraound signals. Parque Nacional Galapagos staff heard noises described as bellows coming from Volcan Chico fissure vent, and coupled with the seismicity and infrasound data, suggested the start of an eruption. An IG report posted 20 minutes later described a thermal anomaly identified in satellite images in the northern area of the caldera, near Volcan Chico. Park staff observed lava flowing towards the crater's interior as well as towards the northern flank.

Telica | Nicaragua
(monitoring agency) Instituto Nicaraguense de Estudios Territoriales (INETER) and (civil defense) Sistema Nacional para la Prevencion, Mitigacion y Atencion de Desastres (SINAPRED) reported that an eruption at Telica began at 07:08 on 21 June. Explosions produced an ash plume that rose 500 m above the crater and drifted east, south, and south west, and ejected tephra that was deposited within a 1 km radius of the volcano. Ashfall was reported in areas including La Joya, Las Marias (8 km NNW), Pozo Viejo (10 km NNW), Ojo de Agua, San Lucas (11 km NNW), Las Higueras, Las Grietas (12 km NNW), and Posoltega (16 km WSW).

June 28, 2018

El Hierro volcano, El Hierro, Canary Islands, Spain
A small swarm is currently going on off the coast of the island with the latest one in the direct area of the underwater vent. The depth is however still too deep to speak of a real new activity. Deformation is in general not affected on the exception of 1 slight abnormality around El Pinar. We will of course keep an eye on it the following hours and days. (Thx to Kirsten Hederstierna for waking me up 🙂 )


Weekly Volcanic Activity Report: 6 - 12 June 2018
Via Smithsonian Institution - Global Volcanism Program / US Geological Survey's Volcano Hazards Program

Fuego | Guatemala
During 6-12 June INSIVUMEH and CONRED reported that strong lahars at Fuego were often hot, steaming, and had a sulfur odor, and were generated from heavy rains and the recent accumulation of pyroclastic-flow deposits from the 3 June events. On 6 June lahars descended the Santa Teresa, Mineral, and Taniluyá drainages (tributaries of the Pantaleón river) and possibly the Honda drainage, halting search-and-rescue efforts. The lahars were 30-40 m wide, 2-5 m deep, and carried blocks (2-3 m in diameter) and tree parts. CONRED noted on 9 June that deposits on roads were being cleaned at a rate of 150 m per day, and that exposed deposits were as hot as 150 degrees Celsius. Significant hot lahars, 40 m wide and 5 m deep, traveled down the Seca, Mineral, Niágara, and Taniluyá drainages, carrying rocks and tree branches. On 10 June a strong lahar traveled down the Seca, Mineral, Niagara, Taniluyá, and Ceniza drainages. It was 35 m wide, 3 m deep, and carried blocks up to 1 m in diameter, tree trunks, and branches. Lahars that traveled down the Seca and Mineral drainages on 11 June were 40 m wide and 3 m deep. Lahars on 12 June were 20-45 m wide and 2-5 m deep, and flowed down the Ceniza and Mineral rivers.
During 6-11 June as many as nine weak explosions per hour produced ash plumes that rose as high as 1.1 km above the crater and drifted 8-15 km W, SW, and S. Avalanches of material descended the Las Lajas and Santa Teresa ravines. Some explosions vibrated local structures. At 0820 on 8 June a pyroclastic flow descended the Las Lajas and El Jute drainages, producing an ash plume that rose as high as 6 km and drifted W and SW. Explosive activity increased during 11-12 June, with dense ash plumes rising 1.3 km and drifting as far as 25 km N and NE. Pyroclastic flows traveled down the Seca drainage. According to CONRED, as of 12 June, the number of people that had died due to the 3 June pyroclastic flows was 110, and 197 more were missing. In addition, 12,578 people had been evacuated.

Great Sitkin | Andreanof Islands (USA)
Seismicity at Great Sitkin was elevated during the previous five days, though at 1139 on 10 June a seismic signal indicating a possible short-lived steam explosion prompted AVO to raise the Aviation Color Code to Yellow and the Volcano Alert Level to Advisory. No infrasound signal associated with the event was detected, and no volcanic clouds rose about the meteorological cloud deck at 2.4 km (8,000 ft) a.s.l.

Ibu | Halmahera (Indonesia)
PVMBG reported that at 1206 on 6 June an eruption at Ibu generated an ash plume that rose at least 500 m above the crater rim and drifted N. An event at 1750 on 12 June produced an ash plume that rose 600 m and drifted N. 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.

Kerinci | Indonesia
Based on satellite data, the Darwin VAAC reported that on 10 June an ash plume from Kerinci rose to an altitude of 4 km (13,000 ft) a.s.l. and drifted W.

Manam | Papua New Guinea
Based on a pilot observation, the Darwin VAAC reported that on 10 June an ash plume from Manam rose to an altitude of 1.8 km (6,000 ft) a.s.l. The ash plume was not identifiable in satellite images.

Ruapehu | North Island (New Zealand)
On 5 June GeoNet reported that a new heating cycle at Ruapehu’s summit Crater Lake began, as indicated by a recent rise in the water temperature. The increasing lake temperature began 29 May, at a rate of about 1°C per day. Volcanic tremor also increased, representing a greater flow of hydrothermal fluids into the lake. Many heating and cooling cycles have occurred in the past; the current cycle does not indicate an unusual sign of unrest. The Volcanic Alert Level remained at 1 (minor volcanic unrest) and the Aviation Color Code remained at Green.

Sierra Negra | Isla Isabela (Ecuador)
On 8 June IG reported a continuing high level of seismicity at Sierra Negra, characterized by a larger number and magnitude of earthquakes, indicating magma movement. The number of events per day had been significantly increasing since mid-2016. In the previous 10 days there was an average of 42 local events/day; on 25 May there were 104 events, the largest number of earthquakes per day recorded since 2015. In addition, in a 24-hour period during 7-8 June there were a total of 48 volcano-tectonic events, two long-period events, and three hybrid earthquakes; a M 4.8 long-period earthquake was recorded at 0715 on 8 June. The earthquake epicenters were mainly located on the edges of the crater, in two NE-SW trending lineaments; the first covered the N and W edges of the crater and the second went from the NE part around to the S edge. Data showed very large deformation at the caldera’s center, compared with lower levels of deformation outside of the caldera.

Ulawun | New Britain (Papua New Guinea)
According to the Darwin VACC, a NOTAM (Notice to Airmen) stated that on 8 June an ash plume from Ulawun rose to an altitude of 2.1 km (7,000 ft) a.s.l. and drifted W.

June 14

Volcanic hazards - world (Philippa)
We have just been reminded of this really useful and informative series of videos on different volcanic hazards. These cover topics such as pyroclastic density currents (PDCs - avalanches of hot volcanic gases, volcanic ash, and other fall-out), lahars (floods of water, ash, and larger debris), lava flows, ash fall, volcanic gases, and so on.

Currently there are versions of these videos in English, French, Spanish, and Baha Indonesian, and future plans to create versions in Italian and Turkish too.

Please spread this link far and wide, in particular to the media in your country, who in their attempts to report volcano stories quickly, often confuse the terminology and phenomena.

via VolFilm / Vimeo


Kilauea volcano, Big Island, Hawaii, USA (Philippa)
Hawaii County Civil Defense Alerts: http://www.hawaiicounty.gov/active-alerts
HVO dashboard for Kilauea: https://volcanoes.usgs.gov/observatories/hvo/activity_2018.html
HVO lava flow maps:
Frequently asked questions - Health & safety: https://www.facebook.com/notes/usgs-volcanoes/k%C4%ABlauea-eruption-faqs-health-and-safety/2028377117190839/
Frequently asked questions - Hawaiian volcanoes & hazards:
Hawaii National Park Services:
Vog forecast:
Information about vog:
Information about volcanic ashfall:
Halema'uma'u Crater (live webstream):
Honolulu Civil Beat (live webstream):

For those of you interested in how volcanoes are monitored, you might want to take a look at the resources on the Hawaiian Volcano Observatory's website right now. In particular, we are fascinated by how they are using drones and satellite imagery from other agencies to supplement the observations that their field crews are making from the ground and now twice-daily helicopter overflights.

The image below is a screen shot from a video from the drone, which was filmed on 4th June. The drone is able to hover more steadily than a helicopter over the hot lava flows, despite the air turbulence caused from this heat. The USGS are then able to use a method known as particle image velocimetry (PIV) in order to best determine the velocity (speed - with direction) of the lava streams. There are two ways in which this can be calculated: either i) visually following a point in the lava stream to determine how far it has traveled over time (recall: speed = distance divided by time), or ii) by observing how quickly the lava flows past a specific fixed location for a given time.

via US Geological Survey / Hawaiian Volcano Observatory

With regards to satellite observations from Space in helping with responses to volcanic eruptions:


The GIF in the link below shows satellite radar imagery from the Italian Space Agency's Cosmo-SkyMed system of changes in the summit area of Kilauea volcano, i.e. the Overlook Crater, Halema'uma'u Crater, and the surrounding area of the Hawaii Volcanoes National Park. Following an explosive eruption at the summit area yesterday (6th June 2018) at around 4:07 p.m. local time, there is now some concern for the stability of Halema'uma'u Crater wall on the side nearest HVO's building and the Jagger Museum, both of which are currently closed. This particular eruption generated the equivalent energy release to a M5.6 earthquake, and the ash plume reached an altitude of around 10,000 ft / 3048m above sea level. The volcanic ash fall was in the direction of the trade winds, i.e. over the Ka'u Desert and Pahala in south western Big Island.


All of these aerial observations are assisting HVO with providing relevant information to the Hawaii County Civil Defense in order to advise local residents in affected areas of road closures and evacuation notices in a timely manner.

Nyiragongo and Nyamuragira volcanoes, Democratic Republic of Congo (Philippa)
For those of you in the UK and British Isles, Ireland, BeNeLux and other countries where the BBC broadcast, make a note in your diary: the fantastic (and now award-winning!) tv programme 'Expedition Volcano' is being re-broadcast later this month.

Episode 1 will be on BBC2 at 8 p.m. on Sunday 17th June; we assume that Episode 2 will then be on a week later. Both episodes will then be available to watch again also via BBC iPlayer (UK-only) (whispers - although someone has also put it out on YouTube for everywhere else - go find!)

Via Chris Jackson (@seis_matters)

We at Earthquake-Report.com cannot help but be a little excited about this, as it is the first tv programme that we have seen that focuses not just on the eruptive activity of volcanoes and technological advances in how they are monitored, but also the impacts of the people living around them.

'Expedition Volcano' features Nyiragongo and Nyamuragira in the Democratic Republic of Congo. Near to the former is the city of Goma, which has a population of over 1 million people. These volcanoes are characterised by particularly hot and fast-flowing lava flows, which during the last eruption inundated the city. The programme highlights how it was not even the eruptions which turned the situation into a disaster, but rather the compounding effects of these with the already-existing problems of human displacement following civil wars in the DRC and neighbouring Rwanda, which then lead to an outbreak of cholera and other infectious diseases causing high mortality rates.

Click on the link below for the BBC trailer:


As well as staff from the volcano observatory in Goma, rangers from Virunga National Park, and other local organisations, 'Expedition Volcano' also features:

  • Dr Xand van Telleken (medical doctor) (@xandvt), who investigates both the cholera outbreak from the last eruption, long-term health effects of living near a volcano, and what people in Goma are doing to lessen the health impacts upfront of future eruptions of Nyiragongo
  • Aldo Kane (former royal marine; expedition leader and safety officer) (@AldoKane)
  • Professor Christopher Jackson (geoscientist - UCL) (@seis_matters) - provides much of the commentary and further explanations that links together the volcanic processes and the human impacts
  • Dr Kayla Iocovino (geoscientist - Arizona State University) (@kaylai) - attempts to test some new kit to determine the levels of volcanic gases from both volcanoes, which tells us something about whether there is new magma coming into the systems, and if so, at roughly which depths
  • Professor Jeff Johnson (geophysicist - Boise State University) - one of my former supervisors, who uses air pressure sensors to detect the low frequency (infrasound) aero-acoustic emissions from Nyiragongo to try and detect changes in the levels of the lava lake within the crater
  • ...and several researchers from Belgium, who use drones and other visual methods to see if they also can detect changes in the levels of the lava lake

Did we say that 'Expedition Volcano', as well as being hugely informative, looks and sounds absolutely stunning? All credit to the tv crew. The background music by Segun Akinola is also worth checking out (https://soundcloud.com/segunakinola )

La Palma and Tenerife, Canary Islands (Philippa)
GeoTenerife have just taken in their first batch of summer interns for INVOLCAN, which will mean lots of lovely photos for us from various volcanic locations around the Canary Islands. Here are the first ones posted.

If any of you are looking to do some geo-tourism, as well as Tenerife (for Mount Teide) and La Palma, I can highly recommend Lanzarote, where I did a 2 week field trip during my undergraduate degree in geophysics. The volcanic landscape, which in geological terms is young (last eruption <200 years ago) is stunning and easily accessible by car or coach. In particular I would recommend the Cueva de los Verdes (lava caves) in Jameos, and Timanfaya National Park.

June 7th, 2018

Volcan de Fuego, Guatemala (Philippa)
Trying to get an update on the situation following the eruption of Fuego this week is proving tricky. However, the latest statement has just been released by Relief Web for Guatemala:

192 people have been registered as missing. Rescue work has re-commenced to try and find them despite red alerts still being in place for the worst affected regions around the volcano: Chimaltenango, Sacatepequez and Escuintla. There have been 78 incidents since Sunday registered as being connected with the eruptive activity and ensuing pyroclastic density currents (PDCs - avalanches of hot volcanic gases, ash, and other plume fall-out) and lahars (flows of water and volcanic debris).

75 people are confirmed dead. 58 people have been admitted to hospitals with 2nd and 3rd degree burns as a result of being caught by the edge of a PDC. 44 others have been admitted with other injuries.

1.71 million people have been affected in this immediate aftermath. Of these, 12,089 people have been registered as having been evacuated from villages and hamlets around Fuego, of which 3,319 people have been temporarily re-housed and 3,271 treated for minor injuries.

With regards to infrastructure: the main electric power grid, two main roads, and a vital bridge have been destroyed. Seven schools in the area have been damaged.

CONRED (Civil Defense and National Disaster Response for Guatemala) report that the voluntary fire brigade are working to get machinery into these areas to try and clear the blocked and destroyed roads as quickly as possible.

Part of the problem though is that the deposits from PDCs are still hot, so much so that the hot ash is melting the soles of the rescue workers boots. (NOTE: From my time working with Montserrat Volcano Observatory in the Eastern Caribbean, when we measured the surface temperature of pyroclastic density current deposits a year on from an eruption of Soufriere Hills Volcano, they were still around 80 degrees Celcius. Because the volcanic ash in these deposits is glassy, they retain heat for a long time).

via Francisco Paez (@paezfrancisco)

This footage shows how deep the PDC deposits are in some places around Fuego.

via Evelyn de Leon (@evelynndeleon)


Popocatepetl, Mexico (Philippa)
Following on from the volcanic disaster this week in Guatemala, research volcanologists based at UNAM have re-issued the hazard maps for Popocatepetl volcano in Mexico. If you live in the vicinity of this volcano (and I know that there is at least one earthquake-report.com reader who does), please take the time to have a look at these, as a little knowledge prior to any eruption could help save a life, particularly with regards to understanding your location and evacuation routes. The poster is in Spanish, and covers tephra (volcanic ash fall), ballistics, Pyroclastic Density Currents, lahars, lava flows, and avalanches.

via Hugo Delgado Granados, UNAM

Click on this image to watch one with all possible details

Kilauea, Big Island, Hawaii, USA (Philippa)
Hawaii County Civil Defense Alerts: http://www.hawaiicounty.gov/active-alerts
HVO dashboard for Kilauea: https://volcanoes.usgs.gov/observatories/hvo/activity_2018.html
HVO lava flow maps:
Frequently asked questions - Health & safety: https://www.facebook.com/notes/usgs-volcanoes/k%C4%ABlauea-eruption-faqs-health-and-safety/2028377117190839/
Frequently asked questions - Hawaiian volcanoes & hazards:
Hawaii National Park Services:
Vog forecast:
Information about vog:
Information about volcanic ashfall:
Halema'uma'u Crater (live webstream):
Honolulu Civil Beat (live webstream):

What a difference a month makes! It was only at the end of April this year that the lava lake within the Overlook Crater was overflowing onto the floor of Halema'uma'u Crater at the summit area of Kilauea volcano. Then the lava lake suddenly started draining down to below the water table, as it did also at the Pu'u O'o vent, leading to deflation and more explosive, steam-driven eruptions at the summit, and lava fountaining from fissures (cracks in the ground) further along the East Rift Zone.

The latest image of Halema'uma'u Crater (below) shows just how much this has widened and deepened in just this one month period. The Hawaiian Volcano Observatory and the Jagger Museum are to the top-right of shot. The museum and this part of Hawaii Volcanoes National Park remain closed, and staff from HVO have had to re-locate to safety elsewhere on Big Island.

via USGS Volcanoes (@USGSVolcanoes)

Video on tracking the active lava flows in the Lower East Rift Zone - via USGS / YouTube

Lower East Rift Zone:
Vigorous lava flows continue from fissures (cracks in the ground) within Leilani Estates and Lanipuna Gardens Sub-Division within the Lower Puna area of south eastern Big Island. In particular, lava fountaining from Fissure #8 has been reaching heights of 150-180 ft. / 45-55 m, and is feeding channels of lava with are flowing into the sea, generating laze, which is hydrochloric acid steam from the chemical reaction between the hot lava and cool sea water. These lava flows have now filled Kapoho Bay, creating an unstable lava delta.

via USGS Videos (@usgs_videos) - enhanced audio description video - 4th June 2018


Several roads in the vicinity of Kapoho and Vacatioland were closed as a precaution in case potential evacuation routes became cut off by lava flows.

Steamboat Geyser, Yellowstone National Park, Wyoming, USA (Philippa)
Steamboat Geyser, which is one of the biggest geysers in the world, has this week been erupting again. You may wish to turn down the volume before pressing play on the video (below) to avoid being deafened...not by the geyser, but by the shrill excitement of one particular geyser gazer!

via Art Haeussler / YouTube - 4th June 2018 around 09:04 local time

Geysers produce purely steam-driven eruptions. They require a delicate combination of 3 factors: a supply of water that is capable of re-charging; a constant supply of heat from the surrounding bed rock; a plumbing system with a constriction (to act as a bubble trap) within a silicic bed-rock. Water heats up to above its boiling temperature (which at these locations is less than 100 degrees Celcius), but remains in a liquid state under pressure underground, i.e. it becomes super heated. Once the plumbing system has fully re-charged with this heated water, it begins to overflow at the surface during a phase prior to eruption known as pre-play. This surface overflow lowers the pressure underground, causing the super-heated water underground to flash to steam and erupt.

Over half of the world's geysers are found at Yellowstone National Park, with most of the others found in Iceland, New Zealand, and Chile, i.e. in volcanic areas of the world.

Mount Rainier and Mount St Helens, Washington State, USA (Philippa)

Mount Merapi, Java, Indonesia (Philippa)
Following on from earthquake-report.com mentioning the phreatic (steam-driven) eruption at Mount Merapi on 1st June, we have just managed to find this footage also of the start. It was filmed from the hamlet of Balerante, which is 5 km away from the summit area. The footage appears to be in real-time, so the jetting at the base of the plume is quite incredible to watch!

via Sutopo Purwo Nugroho (@Sutopo_PN) / BPBD Central Java CCTV camera

Mount Sinabung, Sumatra, Indonesia (Philippa)
This fantastic shot, taken with a telephoto lens, reminds us that Mount Sinabung is still active. Given that this particular volcano generates pyroclastic density currents (PDCs - avalanches of hot volcanic gases, volcanic ash, and other fall-out from an eruption plume) on a regular basis, the Indonesians from the island of Sumatra have much understanding and sympathy for those affected by this week's eruption of Volcan de Fuego in Guatemala.

via Endro Lewa (https://www.facebook.com/endrolewa/) - taken 5th June 2018 ~1:44 p.m. local

Novarupta-Katmai, Alaska, USA (Philippa)
The largest eruption of the 20th Century began on this day in 1912 at Novarupta-Katmai volcanic complex on the Alaska peninsula. The eruption plumes reached altitudes corresponding to the stratospheric layer of the atmosphere, which has strong winds that carried the volcanic ash around the globe. Tephra deposits from the eruption plumes and associated Pyroclastic Density Currents (PDCs) filled the Valley of Ten Thousand Smokes with more than 600 ft. / 183 m of volcanic ash!

Read the full story from eye-witness accounts in this fantastic booklet produced by the National Park Services in Alaska.


NOTE: For any of you who are students, there is a field class that you can take with the University of Alaska Fairbanks that goes to this particular area. Probably too late to apply for this year, as both this field school and the one to Kamchatka in the Far East of Russia take place during the summer, but let us know if you are interested, and we shall put you in contact with the relevant people.

Weekly Volcanic Activity Report: 30 May - 4 June 2018
Via Smithsonian Institution - Global Volcanism Program / US Geological Survey's Volcano Hazards Program

Fuego | Guatemala
In a special bulletin from 0600 on 3 June INSIVUMEH noted increased activity at Fuego. Strong explosions were accompanied by rumbling sounds, and shock waves that vibrated local structures. Dense ash plumes rose 2.3 km above the crater and drifted SW, W, NW, and N. Pyroclastic flows descended the Seca (Santa Teresa) drainage on the W flank, and possibly other drainages, though poor weather conditions prevented clear views of the summit area. Ash plumes drifted in westerly directions, causing ashfall (on roofs and cars) in Sangre de Cristo (8 km WSW) and San Pedro Yepocapa (8 km NW). By 1000 pyroclastic flows were descending the Cenizas (SSW) drainage. Ashfall was reported in additional areas including La Soledad (10 km ESE), Quisache, and the municipality of Acatenango (8 km E).
Based on information from multiple agencies, the Washington VAAC reported an ash plume rising to 9 km (30,000 ft) a.s.l. at 1130 from an explosive eruption. In a report from 1340, INSIVUMEH described large pyroclastic flows traveling down the Seca, Cenizas, Mineral, Taniluya (SW), Las Lajas (SE), and Honda (E) drainages, producing dense ash plumes that rose 6.2 km above the summit (or 32,800 ft a.s.l.). A news article stated that the pyroclastic flows traveled at least 8 km and reached temperatures of 700 degrees Celsius. Tephra and lapilli fell in areas more than 25 km away, including in La Soledad, San Miguel Dueñas (10 km NE), Alotenango, Antigua Guatemala (18 km NE), and Chimaltenango (21 km NNE). Ashfall was reported as far away as Guatemala City, 70 km E. Explosions rattled structures within 20 km of Fuego. The La Aurora International Airport closed at 1415. Eyewitness accounts described the fast-moving pyroclastic flows inundating fields people were working in, overtaking bridges, and burying homes up to their roof lines in some areas. San Miguel Los Lotes, Alotenango, and El Rodeo (10 km SSE) were the worst affected.
According to Simon Carn, satellite data analysis showed that the event produced the highest SO2 loading measured from a Fuego eruption in the satellite era (since 1978), and therefore most likely the highest since the major 1974 eruption. He went on to note that the SO2 mass was about ~2 orders of magnitude than the 1974 eruption, which had a significant stratospheric impact.
At 1650 INSIVUMEH noted reports of lahars descending the Pantaleón drainage (fed by the Santa Teresa and El Mineral rivers) and other drainages. CONRED had evacuated communities near Fuego, including Sangre de Cristo, finca Palo Verde, and Panimache. At 2200 (~16.5 hours after the increased activity began), the eruption waned, with activity characterized by weak-to-moderate explosions, crater incandescence, and ash plumes that rose almost 800 m. The seismic station (FG3) recorded the last pyroclastic flow at 1845. By 0725 on 4 June seismicity had returned to normal levels. Explosions occurring at a rate of 5-7 per hour produced ash-rich plumes that rose as high as 900 m and drifted 15 km SW, W, NW, and N. Avalanches of material descended the flanks. The La Aurora International Airport reopened and flights resumed at 0930.
On 5 June INSIVUMEH reported that activity again increased. Explosions occurring at a rate of 8-10/hour, some strong, generated ash plumes that rose 5 km and drifted E and NE. At 1928 a pyroclastic flow traveled down the Las Lajas drainage. News articles noted that authorities called for another evacuation.
CONRED reported that by 0630 on 6 June a total of 12,089 people had been evacuated, with 3,319 people dispersed in 13 shelters. One bridge and two power networks had been destroyed. According to news sources on 6 June, Guatemala's National Institute of Forensic Sciences stated that 75 people were confirmed to have died and 192 were still missing. Many, possibly thousands, received burns and other injuries. Weather conditions, continuing activity at Fuego, poor air quality, hot pyroclastic flow deposits, and rain made rescue efforts difficult.

Kerinci | Indonesia
Based on satellite data, the Darwin VAAC reported that on 5 June a minor ash emission from Kerinci rose to an altitude of 4.3 km (14,000 ft) a.s.l. and drifted W.

Kilauea | Hawaiian Islands (USA)
HVO reported that the eruption at Kilauea’s Lower East Rift Zone (LERZ) and at Overlook Crater within Halema`uma`u Crater continued during 30 May-6 June. Lava fountaining and spatter was concentrated at Fissure 8, feeding lava flows that spread through Leilani Estates and Lanipuna Gardens subdivisions, and reached the ocean at Kapoho Bay. Fissures 22, 6, and 13 were periodically active on 30 May, and fissures 6/13 spattered on 4 June. Sluggish lava flows were present around Fissure 18.
Inward slumping of the crater rim and walls of Halema`uma`u continued, and earthquake activity beneath the caldera was mostly high, as the summit area adjusted to the withdrawal of magma from Overlook Crater. Passive degassing of SO2 from the summit decreased, but emission rates were high enough to impact air quality downwind. Ash emissions were intermittent and low, though around 1100 on 30 May an ash plume rose to 3.6 km (12,000 ft) a.s.l. A small explosion was detected at 1339 on 1 June. A preliminary M 5.5 earthquake was recorded at 1550 on 3 June, producing an ash plume that rose to 2.4 km (8,000 ft) a.s.l. A small explosion and accompanying M 5.5 earthquake was detected at 0432 on 5 June; an ash plume rose to 1.6 km (5,100 ft) a.s.l.
During the beginning of the reporting period Fissure 8 generated tall lava fountains, rising 80 m, and some secondary fountains that rose 18 m. Pele's hair and other volcanic glass from the high fountaining fell in areas W of the fissure and within Leilani Estates. A small (30 m high) spatter cone formed at the downwind side of the fountain. Volcanic gas emissions from the fissures were very high; trade winds blew vog to the S and W parts of the island.
The lava flow fed by Fissure 8 advanced NE at a rate of 550 m/hour during 29-30 May, but then slowed to 90 m/hour on 31 May. High eruption rates led to the formation of a leveed channel along the W edge of the lava flow; small overflows from the channel occurred along its length. On 2 June lava flowed around the N part of Kapoho Crater and then turned S, entering the Vacationland neighborhood. At 0700 the flow front had entered Kapoho Beach Lots, moving about 75 m/hour. Lava entered Green Lake (70 m x 120 m in dimension, and 60 m deep) at 1000, creating a large steam plume. By 1500 lava had completely filled the lake and boiled off the water. Locals reported that lava (with a flow front 800 m wide) entered the ocean at Kapoho Bay around 2230. By late afternoon on 4 June lava had built a delta extending almost 700 m into the bay.
Overnight during 4-5 June lava fountaining at Fissure 8 was less vigorous, with a maximum height of 55 m. By 0630 on 5 June lava had completely filled Kapoho Bay, creating a new coastline 1.1 km away from the former coastline. To the S lava had overtaken most of the Vacationland subdivision and was entering the tidepools. All but the northern part of Kapoho Beach Lots had been covered.

Merapi | Central Java (Indonesia)
PVMBG reported that at 0820 on 1 June an event at Merapi generated an ash plume that rose at least 6 km above the crater rim and drifted NW, but then winds changed to the SW. Ashfall was reported at the Selo observation post. Observers noted white smoke rising from a forested area 1.5 km NW, possibly indicating burning vegetation. The report noted that volcano-tectonic events were occurring at about 3 km below the crater. Later that day at 2024 an ash plume from a 1.5-minute-long event rose 2.5 km above the crater rim and drifted NE and W. At 2100 an ash plume rose 1 km and drifted NW. The Alert Level remained at 2 (on a scale of 1-4), and PVMBG noted that all people within 3 km of the summit should be evacuated.

June 6th, 2018

Fuego, Guatemala (Armand)
Very sad to report that a total of 192 people remain missing after the Fuego volcano's eruption that killed at least 73.

Kilauea, Hawaii, USA (Armand)


While i was looking for only 5 minutes, i witnessed this small explosion

Fuego, Guatemala (Philippa)
Please bear with us this morning as we update you in stages on the situation.

Volcanological Activity - Special Report from INSIVUMEH Guatemala -#35-2018 (4th June 2018, 10:30 local time - via @insivumehgt)
The explosive eruption plumes have been reaching altitudes of around 4.5-4.6 km above sea level (~14,765-15,090 ft.) dissipating in south-westerly, west, northwest and north directions up to 15 km away from source. A volcanic ash advisory was issued to the civil aviation industry, and the airport in Guatemala City was temporarily closed, but according to AGN (the agency for pubic notices in Guatemala - via @AGN_noticias) has since re-opened in order to conduct inter-agency rescue and relief efforts.

The greatest concerns for the monitoring agency in the hours immediately following this week's VE1 3 explosive eruption has been pyroclastic density currents (PDCs), which are fast-flowing avalanches of hot volcanic gases, volcanic ash, and other fall-out from eruption plumes as they collapse. These flow faster than a car can drive, and death by one of these is particularly gruesome (the intense heat causes immediate paralysis of the body's muscles, due to proteins in the muscles de-naturing above 40 degrees Celcius. Furthermore, this heat not only burns the skin, but also burns the throat and lungs). The general public is being asked to stay away from ravines, which are the most likely routes that both PDCs and lahars (fast-flowing floods of water, volcanic ash and debris) follow. However, PDCs can also flow up and over ravines as well as along them, making them particularly dangerous.

We can see from this footage (below) of people filming an on-coming PDC how the volcanic gases make them buoyant. NOTE: if you should ever find yourself in such a situation on a volcano, do not hang around to film. Get out of the way to safety immediately! We cannot emphasize enough how dangerous PDCs are!

via Entropia (@Sunlight_lovee)

This must have been absolutely terrifying for anyone trying to escape from the fall-out areas around Fuego.

via Jorge Becerril JB/8 (@MrElDiablo8)


Is anyone on here able to translate from Guatemalan Spanish what this lady says. It would seem that she had a lucky escape!

via Jorge Becerril JB/8 (@MrElDiablo8)


INSIVUMEH have advised CONRED Guatemala to continue rescue attempts where possible, but to take their own safety into account in case of further eruptive activity with PDCs and lahars over the next coming days.

INSIVUMEH will issue another special report if there are either any changes in the volcanic seismicity or morphological changes to the summit area of Fuego.

Emergency response map (via IAVCEI Hazard & Risk - @IAVCEI_Hazards)
The European Commission issued this emergency response map (below) following the VEI 3 eruption of Fuego this week. Note that the death toll has sadly risen to 62, with more fatalities likely to be announced as emergency responders reach more of the affected areas.

This video from a helicopter overflight shows some of the areas which were affected yesterday.

via Jorge Becerril JB/8 (@MrElDiablo8)



Statistics: released yesterday (4th June 2018) by CONRED Guatemala (@ConredGuatemala)

Press conference:
A press conference was held earlier today, featuring one of the monitoring volcanologists, representatives from CONRED Guatemala (National Co-ordinator for Disaster and Risk Reduction - i.e. Civil Defense), Minster for Public Health, Ministry of Defense, and others. It was broadcast live on social media (https://www.facebook.com/guatemalagob/videos/2064237186938639/) and also on Twitter via Gobierno Guatemala (@GuatemalaGob).

According to (volcanologist) Eddy Sanchez, Fuego had 9 eruptions last year and 2 eruptions prior to this one this year, which was driven by an increase in volcanic gas content of the magma**. Rumours of this eruption being connected to an Earthquake and of the volcano developing a new crater are false. The volcanologists' greatest concern at the moment is if the weather conditions change over the next few days, particularly if the rainfall intensifies, which could re-mobilise volcanic ash, producing lahars,  causing further destruction of agricultural areas. Any re-mobilisation of this ash could also potentially lead to long-term respiratory problems for residents.

** This to us would indicate either an up-welling of younger, more gas rich magma triggering this week's eruption, and/or a new batch mingling with an older batch which had been in place underground for a while. This, however, is speculation on our part, and would require analysis of samples of the volcanic ash to confirm.

Government officials have been to hospitals to visit some of the injured, visited hostels to provide immediate short-term accommodation for those displaced, and met with people from business sectors in Guatemala to get (financial) support.*** An infrastructure and aid plan are going to be presented to the government cabinet later today.

*** 'Natural' disasters, and in particular rescues and evacuations, are costly.

Infrastructure (via Elsa Coronado Q - @elsacoronadogt)
CIV Guatemala (The Ministry of Communications, Infrastructure, and Living) have announced that the focus will be on clearing road RN14 Guatemala and re-building Las Lajas bridge.

The image (below) shows fire fighters and other first responders working hard meanwhile to try and clear national route #14 of the volcanic deposits from this week in order to try and rescue others who might be trapped.

via Jorge Becerril JB/8 (@MrElDiablo8)

This is possibly one of the most heart-breaking reports we have ever read in connection with a volcanic eruption. If you are not of a strong disposition, look away now.

When first responders managed to reach this particular area near Fuego volcano, this dog alerted them to the whereabouts of its human family. Unfortunately, all 8 people had succumbed in the aftermath of the eruption.

via Jorge Becerril JB/8 (@MrElDiablo8)

Kilauea volcano, Big Island, Hawaii, USA (Philippa)
Hawaii County Civil Defense Alerts: http://www.hawaiicounty.gov/active-alerts
HVO dashboard for Kilauea: https://volcanoes.usgs.gov/observatories/hvo/activity_2018.html
HVO lava flow maps:
Frequently asked questions - Health & safety: https://www.facebook.com/notes/usgs-volcanoes/k%C4%ABlauea-eruption-faqs-health-and-safety/2028377117190839/
Frequently asked questions - Hawaiian volcanoes & hazards:
Hawaii National Park Services:
Vog forecast:
Information about vog:
Information about volcanic ashfall:
Honolulu Civil Beat (live webstream):

An information sheet on the past 30 days of eruptive activity at Kilauea volcano
- via USGS Volcanoes (@USGSVolcanoes)

The latest volcanic hazard map of the Lower East Rift Zone (LERZ) in the Lower Puna area of southeastern Big Island - via USGS Volcanoes (@USGSVolcanoes)

Mount Merapi, Java, Indonesia (Philippa)
With the world's attention focused on Volcan Fuego in Guatemala and Kilauea volcano in Hawaii, we missed this phreatic (steam-driven) eruption of Mount Merapi on the Indonesian island of Java on 1st June 2018. This occurred around 08:20 a.m. local time that day, and lasted around 2 minutes. The eruption plume reached a height of around 6 km.

In addition to towns and villages, the major city of Yogyakarta is located less than 30 km away from Merapi, so all eyes are on the volcano at the moment in case it fully re-awakens. The last major eruptions of Merapi were in 2010, followed in 2014 with some lesser activity.

via Sutopo Purwo Nugroho (@Sutopo_PN)

Image of Merapi taken from Balerante hamlet, which is just 5.7 km from the summit area. Here we can clearly see the opening in the crater from the 2010 eruption, which generated extensive pyroclastic density currents and later lahars.

via Sutopo Purwo Nugroho (@Sutopo_PN)

June 5th, 2018

Kilauea, Hawaii, USA

Kīlauea Volcano Lower East Rift Zone
Vigorous eruption of lava continues from the lower East Rift Zone (LERZ) fissure system in the area of Leilani Estates and Lanipuna Gardens.
Fissure 8 fountaining persisted throughout the day to heights up to 220 feet, and the channelized flow continued to deliver lava northeast along Highway 132 to the Kapoho area. Lava is advancing along a 0.5-mile-wide front towards the ocean at Kapoho Bay between Kapoho Beach Road and Kapoho Kai Drive. As of 5:45 PM HST, the lava flow was about 245 yards from the ocean at its closest approach point. Other branches of the Fissure 8 lava flow were inactive.
All other fissures are inactive, although observers on the late afternoon overflight noted abundant gas emission from Fissures 9 & 10 and incandescence without fountaining at fissures 16 & 18.
Pele's hair and other lightweight volcanic glass from high fountaining of Fissure 8 are falling downwind of the fissure and accumulating on the ground within Leilani Estates. Winds may waft lighter particles to greater distances. Residents are urged to minimize exposure to these volcanic particles, which can cause skin and eye irritation similar to volcanic ash.
HVO field crews are on site tracking the fountains, lava flows, and spattering from multiple fissures as conditions allow and are reporting information to Hawaii County Civil Defense.
Volcanic gas emissions remain very high from the fissure eruptions. Trade wind conditions are bringing vog to the south and west sides of the Island of Hawaii. Afternoon easterly winds may bring vog to communities in the Volcano area.
Magma continues to be supplied to the lower East Rift Zone. Earthquake locations have not moved farther downrift in the past few days and the number of located earthquakes remains low. Seismicity remains relatively low with numerous small magnitude earthquakes and low amplitude background tremor.
Additional ground cracking and outbreaks of lava in the area of the active fissures are possible. Residents downslope of the region of fissures should heed all Hawaii County Civil Defense messages and warnings.
USGS/HVO continues to monitor the lower East Rift Zone activity 24/7 in coordination with Hawaii County Civil Defense.

Kīlauea Volcano Summit
Earthquake activity at the summit was high overnight and through the day. A moderate earthquake (5.5 preliminary) resulting from a volcanic explosion and continued collapse around Halemaumau occurred at 15:50 HST. National Weather Service radar observations confirmed an ash column was produced and reached 8,000 ft. asl.
Volcanic gas emissions at the summit remain high.

Fuego, Guatemala

The number of people killed by the powerful eruption of the Fuego Volcano in Guatemala increased to 25, Guatemala's disaster agency reported, while the number of injured people has risen to some 300.

June 4, 2018

Manaro Voui, Ambae, Vanuatu (Philippa)
A recent image taken at Manaro Voui crater lake on Ambae appears to show calmer conditions in comparison to the vigorous, explosive phreato-magmatic (interaction between magma and water) eruptive activity from March-April of this year. We are trying to ascertain from the volanologist who posted the image if this is in fact the case, and also whether that orange-red is the true colour of the remainder of the crater lake around the active vent. If so, this has been caused by the turn-over of volcanic gases and ash-fall making the water highly acidic.

via Philipson Bani (@philipsonbani)

Aerial shot (below) from satellite imagery captured on 22nd May 2018. From this we can see that much of the crater lake has either interacted directly with the volcanic system of Manaro Voui and/or evaporated

- via Planet Labs (@planetlabs)

As previously reported here on Earthquake-Report.com, due to this recent resurgence in eruptive activity, which has led to heavy ash-fall over most of the island, house collapses, crop failure, affected livestock and contaminated drinking water supplies, all 11,000 inhabitants of Ambae are being evacuated to the neighbouring island of Santo this June.

There are concerns until then that there could be an outbreak of infectious diseases on Ambae:


Both the relief efforts up to this point and the evacuation, which is likely to be long-term or even permanent, have been problematic, both due to lack of funds and lack of available lands to resettle people to. The land that Ambae's residents will be moved to on Santo is only available for a 6 month period as a rental, creating further uncertainty as these people try to re-build their lives, including re-establishing their livelihoods on another island.

There are some rays of light though. UNICEF Pacific, for example, have posted an image on social media of a new school that has been established on Santo in preparation for the arrival of children from Ambae. They also mention that psycho-social support will be provided for the children to help them settle in when they arrive. For the younger children, Save the Children have established safe play areas.

via Jamie Isbister (@AusHumanitarian)

Volcan de Fuego, Guatemala (Philippa)
Fantastic footage captured of an eruption on 26th May 2018 at Volcan de Fuego. Turn your sound up as well to hear the noise at the very start, which for a volcano acoustician such as yours truly is a real treat!

via Massimo (@Rainmaker1973) / Tiemposdelfin Ya / YouTube

Weekly Volcanic Activity Report: 23 - 29 May 2018
Via Smithsonian Institution - Global Volcanism Program / US Geological Survey's Volcano Hazards Program

Kilauea  | Hawaiian Islands (USA)
HVO reported that the eruption at Kilauea’s Lower East Rift Zone (LERZ) and at Overlook Crater within Halema`uma`u Crater continued during 23-29 May. Lava fountaining and spatter was concentrated in the middle portion of the fissure system, feeding lava flows that spread through Leilani Estates and Lanipuna Gardens subdivisions, and also traveled to the ocean.

Earthquakes beneath the summit and ash emissions from Overlook Crater continued as the summit area subsided and adjusted to the withdrawal of magma. Ash emissions were small and frequent, punctuated by larger plumes. The Overlook crater vent continued to widen to the W, and by 25 May the vent area was about 36 hectares. At 1244 on 25 May a M 4 earthquake was located in the summit region. That same day a new pit opened on the N part of Halema`uma`u Crater floor. Three explosions (at 0042, 0144, and 0500) on 26 May generated ash plumes that rose 3-3.3 km (10,000-10,800 ft) a.s.l. A small explosion at 0156 on 29 May sent an ash plume vertically to 4.6 km (15,000 ft) a.s.l. and drifted slightly NW. The explosion was felt by residents in Volcano, and ejected incandescent blocks within Halema`uma`u Crater. On 28 May a M 4.1 earthquake occurred at 1739 along the Koa'e fault zone, S of the caldera.

Lava fountains from Fissure 22 continued to form a channelized lava flow that entered the ocean NE of MacKenzie State Park, causing explosions and generating a plume of hazardous laze (lava haze, a mixture of condensed acidic steam, hydrochloric acid gas, and tiny shards of volcanic glass). On 23 May relatively tall lava fountains at fissures 6 and 13 fed another channelized flow that created a second ocean entry. Observers noted that a perched lava pond/channel was 11 m above ground level, and that methane was seen overnight that burned blue in road cracks. On 24 May lava was entering the ocean at three points between Pohoiki Bay and MacKenzie State Park, though by the next day only two were active.

Overnight during 25-26 May vigorous spatter was observed from a cone on Fissure 8, and multiple booming gas emissions occurred at Fissure 17. By the morning of 26 May an estimated 9.6 square kilometers had been covered by new lava. Fissures 7 and 21 fed a perched lava pond and sent flows NE; the lava-flow fronts became ‘a’a. A perched pond on the W side of Fissure 7 was breached, sending short flows W. Later that day the flows turned S, and by dusk were cascading into Pawaii crater, adjacent to the W margin of the Fissure 6 flow that fed one of the ocean entries. Lava from Fissure 21 flowed onto Puna Geothermal Venture (PGV) property.

During 26-27 May activity at Fissure 7 increased; lava from fountains 45-60 m tall built a large, 30-m-high spatter rampart. Large cracks were observed overnight on Kupono St., near Fissure 9. Three vents active at Fissure 8 spattered and flamed, and doubled in size in one day. On 27 May lava flows from fissures 7 and 8 advanced NE on PGV property; at about 1900 a flow broke out in this area and advanced rapidly to the N and W, through the E portion of Leilani Estates, prompting several residents to evacuate. Three minor ocean entries were again active. Fissure 24 opened in Leilani Estates.

On 28 May the vents that fed the ocean entries stopped erupting, leading to only residual lava in the channel to occasionally enter the ocean. During 28-29 May fountains, lava flows, and spattering from multiple fissures persisted. Pele's hair from vigorous fountaining (60 m high) at Fissure 8 drifted downwind, with some strands falling in Pahoa. According to a news article, the LERZ eruption had destroyed at least 94 structures, including 53 homes, by 29 May. The flows also cut off road access to PGV, which had been evacuated.

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 Halema`uma`u 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.

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

KIII-TV https://www.kiiitv.com/article/news/nation-now/hawaii-lava-flow-destroys-12-more-homes-as-kilauea-volcano-continues-exploding/465-afd62fc3-91d2-4764-9eb9-c3dee473033d

Klyuchevskoy  | Central Kamchatka (Russia)
KVERT reported that a thermal anomaly over Klyuchevskoy was identified in satellite images during 19-20 and 24 May. The Aviation Color Code remained at Orange (the second highest level on a four-color scale).

Geologic Summary. Klyuchevskoy (also spelled Kliuchevskoi) is Kamchatka's highest and most active volcano. Since its origin about 6000 years ago, the beautifully symmetrical, 4835-m-high basaltic stratovolcano has produced frequent moderate-volume explosive and effusive eruptions without major periods of inactivity. It rises above a saddle NE of sharp-peaked Kamen volcano and lies SE of the broad Ushkovsky massif. More than 100 flank eruptions have occurred during the past roughly 3000 years, with most lateral craters and cones occurring along radial fissures between the unconfined NE-to-SE flanks of the conical volcano between 500 m and 3600 m elevation. The morphology of the 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 numerous major explosive and effusive eruptions from flank craters.

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

Merapi  | Central Java (Indonesia)
PVMBG reported that a two-minute-long phreatic eruption at Merapi which began at 1349 on 23 May was heard from the Babadan observation post. A plume was not visible due to inclement weather, though minor ashfall was reported in Ngepos post. On 24 May an event at 0256 generated an ash plume that rose 6 km above the crater rim and drifted W. Roaring was heard from all of the Merapi observation posts. A two-minute-long event at 1048 produced an ash plume that rose 1.5 km and drifted W. The Alert Level remained at 2 (on a scale of 1-4), and PVMBG noted that all people within 3 km of the summit should be evacuated.

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/

Piton de la Fournaise  | Reunion Island (France) 
OVPF reported that the eruption at Piton de la Fournaise which began on 27 April from fissures at Rivals Crater continued through 29 May. Tremor levels continued to decrease slightly, though were mostly stable at low levels. Observations on 24 May indicated flowing lava was mostly confined to tubes, though a small area of incandescence was visible at the main crater.

Geologic Summary. The massive Piton de la Fournaise basaltic shield volcano on the French island of Réunion in the western Indian Ocean is one of the world's most active volcanoes. Much of its more than 530,000-year history overlapped with eruptions of the deeply dissected Piton des Neiges shield volcano to the NW. Three calderas formed at about 250,000, 65,000, and less than 5000 years ago by progressive eastward slumping of the volcano. Numerous pyroclastic cones dot the floor of the calderas and their outer flanks. Most historical eruptions have originated from the summit and flanks of Dolomieu, a 400-m-high lava shield that has grown within the youngest caldera, which is 8 km wide and breached to below sea level on the eastern side. More than 150 eruptions, most of which have produced fluid basaltic lava flows, have occurred since the 17th century. Only six eruptions, in 1708, 1774, 1776, 1800, 1977, and 1986, have originated from fissures on the outer flanks of the caldera. The Piton de la Fournaise Volcano Observatory, one of several operated by the Institut de Physique du Globe de Paris, monitors this very active volcano.

Source: Observatoire Volcanologique du Piton de la Fournaise (OVPF) http://www.ipgp.fr/

May 31, 2018