Tuesday, December 29, 2020

Soufriere St. Vincent Volcano Begins To Build Lava Dome

***UPDATE 12/30/2020***

News coverage has begun reporting on the developments at Soufriere St. Vincent. Some reports are falsely posting articles which show an ash column above the volcano, however the eruption is purely effusive/dome building at this time and no explosions have occurred as yet. 

The alert level has been raised from Yellow to Orange, and scientists are intensely monitoring the volcano in an effort to give at least 48 hours notification to residents should an explosive eruption be imminent.

It seems that the island of Martinique has also decided to raise their alert level, as seismicity has recently been detected under the volcano. This is the first time the alert has been raised since its last eruption in 1932.

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Original article

 Soufriere St. Vincent in the West Indies islands, NE of Venezuela has begun exhibiting lava dome growth, after decades of silence, having last erupted in 1979 after years of activity. The current dome growth appears to be occurring at the South end of the main crater of Soufriere St. Vincent. Vigorous steaming was observed, followed by slow uplift of land between the 1970's lava dome, and the crater wall. 

A post from Facebook on the Vulcanología Esia page revealed the following sequence of events:

Image from Vulcanologia Esia Facebook group.

The last eruption of the volcano produced, in 1979, a VEI 3 scale eruption, and has had many eruptions of VEI 4 magnitude in the past.

Given scant news coverage of the volcano at this time, it is unknown how this eruption will progress. It could remain a mostly dome building, effusive event, or it could turn explosive if the dome event is succeeded by an explosive/pyroclastic event. 

This page will be updated as more details come in. 

The last major eruptive activity in the island chain was when Soufriere Hills on the island of Montserrat erupted unexpectedly, demolishing the capital city of Plymouth in 1995. Other submarine volcanoes may have exhibited minor activity recently, including the humorously named volcano, Kick 'em Jenny,



 


Sunday, December 20, 2020

Kilauea Roars Back to Life!

****BREAKING****

**UPDATE 12/28/2020**

There has been no significant change lately, except that weak summit inflation briefly dipped to deflation, and then back to inflation again. Down rift in the LERZ, the magma supply appears to be favoring the summit eruption, and gradual inflation is now trending towards deflation. 

The lava lake level has remained steady, and the 'island' of cooled rock that has been floating on the lava lake continues to circulate and shrink over time. 

The last active vent has 2-3 small steams of lava pouring out, and SO2 output has decreased significantly within the last day. 

All updates can be found here at Hawaiian Volcano Observatory (usgs.gov)

**UPDATE 12/26/2020**

The lava lake rose to the level of the North fissure, and appears to have stopped it. Lava appears now to be draining back into the fissure, as a 'crust ledge' has formed around the lava lake, and the molten lava is lower than the ledge. The East fissure is slowly spattering lava out back into the lake. It is entirely possible given these developments that the eruption ceases within the next several days or weeks, as the lava lake cools, and the pressure in the shallow magma chamber decreases.


Thermal Time-lapse from HVO on 12/26/2020 shows the inundation and 'death' of the North fissure, while activity from the East (lower fissure resumes).

Summit inflation has also slightly resumed, which could be due to the North fissure now being 'plugged' or receiving lava back into it. 


Summit changing from deflation to inflation, a DI event.

What this means for now is not certain, as this could be a minor inflation, deflation event, or could signal a positive pressure change. The next few days should be telling.

Down rift at Puʻu ʻŌʻō, a slight deflationary trend has been noted, likely due to lack of fresh magma supply as it erupts from the summit. 


**UPDATE 12/22/2020**


The lava lake continues to rise, and it's surface is just beginning to overtake the North fissure's edifice. Hawaii health officials have begun resuming 'vog' (volcanic fog) warnings to residents.

By tomorrow, a new dynamic in the lake should unfold as the magma source becomes lower than the lava lake surface. Spatter cones may form, the lava lake may continue to rise, or it may stop and simply circulate. There is no way of knowing at this point. Summit deflation is consistent with magma release, with the latest subsidence readings at about 0.10 meters in the last several days.

Deflationary event post-fissure eruption and lava lake formation. Copyright HVO.


Down rift to the Lower East Rift Zone (LERZ), the inflationary trend near the 1983-2018 Puʻu ʻŌʻō vent continues a steady upward inflationary trend, apparently unaffected by the summit action at Halema'uma'u caldera. Time will tell if eruptive activity resumes at both vents, although at this point, HVO does not seem overly concerned with this.

Current inflationary trend at Puʻu ʻŌʻō. Copyright HVO.


HVO had been weighing raising the alert level at Kilauea in recent days/weeks, and purportedly were about to do so the night of the eruption, when the eruption occurred suddenly. 

Neighboring Mauna Loa was raised to Yellow alert after the cessation of Kilauea's long-lived eruption which began in 1983 and ended in late 2018. 

Lava lake surface approaching main fissure vent during 12/21-12/22, 2020.

The next few days should give an indication as to whther this lava lake and eruption will be sustained, or short lived. A minor magma intrusion did occur earlier this month at shallow depth, and on occasion, these do result in minor effusive eruptions. 

More updates will follow. 

**UPDATE 9:06pm HST 12/21/2020**

The latest image shows that the lava lake has risen even further. The rate of rise has slowed either due to less lava output, or due to the diameter of the crater widening as levels rise. It appears at least one fissure is issuing lava from beneath the lava pool surface, while two fissures on the crater rim are continuing to issue lava as well. Earlier reports indicated one fissure had ceased, but it is difficult to tell from the images whether this is still the case.

It is still unknown how long the eruption will continue for, and whether other phases will occur.

At this time there is minimal danger to the public as, according to HVO, "The eruption has stabilized" and ash emissions have ceased. HVO lowered the aviation color code from RED to ORANGE in response, after the former water lake had been completely evaporated and lava/water interactions ceased. 





**UPDATE 12:05PM HST 12/21/2020**

Animated GIF From HVO shows the rapid rise of the lava in the crater.




**UPDATE 11:00am HST 12/21/2020**

The caldera floor has now been filled up to the N eruptive fissure, according to the latest Summit Webcam shot (the quality is low, and the HVO web server appears to be under some stress at the moment).

It appears the SW fissure may now be underneath the lava lake, and that the lava lake is now nearly up to the point of overtaking the largest fissure at the N wall of the caldera. The lava lake has greatly exceeded the level of the former water lake.

Image from approximately 8am HST


It is not known how long the eruption will continue.


 Image from about 11am HST

As you can see above, the lava lake is rapidly rising. If the eruption continues throughout the day, there is the possibility that it will overtop the new collapse crater and fill the caldera in further.

   

**UPDATE 8:00am HST 12/21/2020**

According to USGS, the eruption currently consists of three crater wall fissure vents, and the lake is completely gone. A lava lake is forming within Halema'uma'u crater. The eruption so far is limited to the summit, although it is unclear whether any activity may start down rift. 

The eruption in 2018 was spurred by rapid summit lava drainage down rift to Pu'u'O'O crater, which then drained further down the LERZ to the Leilani Estates area. Given that magma still exists down rift from that eruption, and that it is still reasonably hot, it is always possible that the 2018 system can receive a new injection of magma. 

It is too soon to tell what the return of a summit lava lake will mean, or if this eruption will be long lived, or a shorter episode resulting from the minor magma dike intrusion a couple weeks ago. The eruption could go for only days, or go for on for weeks to years. The previous eruptive period on Kilauea was from 1983-2018, with lava present first at  Pu'u'O'O, and then simultaneously with Halema'uma'u, ultimately resulting in the LERZ fissure eruption.





**UPDATE 11:57pm HST 12/20/2020****

Local News now reporting Hawaii Island erupting again, new eruption in Halema'uma'u (khon2.com)

A 4.4 Mag temblor was recorded downrift on the LERZ preceding the summit eruption. It is unclear how this is related at this time.


***UPDATE 11:09pm HST 12/20/2020****

HVO Has now raised the alert level to RED for Kilauea. Kīlauea - Volcano Updates (usgs.gov)

Shortly after approximately 9:30 p.m. HST, the USGS Hawaiian Volcano Observatory (HVO) detected glow within Halemaʻumaʻu crater at the summit of Kīlauea Volcano. An eruption has commenced within Kīlauea’s summit caldera. The situation is rapidly evolving and HVO will issue another statement when more information is available.

Accordingly, HVO has elevated Kīlauea’s volcano alert level to WARNING and its aviation color code to RED.

Alert levels and aviation color codes are explained here: https://www.usgs.gov/natural-hazards/volcano-hazards/about-alert-levels

HVO continues to monitor the volcano closely and will report any significant changes.

Stay informed about Kīlauea by following volcano updates and tracking current monitoring data on the HVO web page (https://www.usgs.gov/volcanoes/kilauea/volcano-updates) or by signing up to receive updates by email at this site: https://volcanoes.usgs.gov/vns2/.

HVO is in communication with Hawai‘i Volcanoes National Park as this situation, which is taking place within the park, evolves.

HVO is in contact with the County of Hawai‘i Civil Defense Agency.

Recent Observations:

For the past several weeks, the USGS Hawaiian Volcano Observatory (HVO) has recorded ground deformation and earthquake rates at Kīlauea Volcano’s summit and upper East Rift Zone that have exceeded background levels observed since the conclusion of the 2018 lower East Rift Zone eruption and summit collapse.

Beginning in September 2020, increased rates of uplift were observed by GPS stations in Kīlauea’s upper East Rift Zone. In the past month, increased uplift has also been measured at GPS stations in Kīlauea’s summit region. While uplift related to post-collapse inflation of the summit reservoir has been occurring since March of 2019, rates have been steadily increasing in recent months and are currently higher than they have been since the end of the 2018 eruption.

In late November 2020, increased earthquake rates began when seismic stations recorded an average of at least 480 shallow, small-magnitude earthquakes (97% of which were less than or equal to magnitude-2) per week occurring at depths of less than 4 km (2.5 miles) beneath Kīlauea's summit and upper East Rift Zone. This compares to a rate of fewer than 180 per week following the end of Kīlauea’s 2018 eruption and through early November 2020.

On December 2, 2020, GPS stations and tiltmeters recorded a ground deformation event at Kīlauea’s summit. Accompanied by earthquake swarms, the patterns of ground deformation observed were consistent with a small dike intrusion of magma under the southern part of Kīlauea caldera. The injection resulted in about 8 cm (3 inches) of uplift of the caldera floor, and modeling suggests that it represented 0.4–0.7 million cubic meters (yards) of magma accumulated approximately 1.5 km (1 mile) beneath the surface. Though the intrusion did not reach the surface and erupt, it represented a notable excursion from trends observed in Kīlauea summit monitoring data streams following the end of the 2018 eruption.

On December 17, 2020, seismometers detected a notable increase in occurrence and duration of long-period seismic signals beneath Kīlauea’s summit, which are attributed to magmatic activity. Whereas this type of seismicity was observed on average once every few weeks following the 2018 eruption, rates have increased to over a dozen in the past several days.

Other monitoring data streams including volcanic gas and webcam imagery were stable until this eruption.

An earthquake swarm began on the evening of December 20, accompanied by ground deformation detected by tiltmeters. An orange glow was subsequently observed on IR monitoring cameras and visually beginning approximately 21:36 HST.

***Original post below***

10 minutes ago HST, Kilauea has now roared back to life, according to HVO.


This marks the first resumption of eruptions from Kilauea since the cessation of eruptive activity after the 2018 Leilani Estates/LERZ eruption, which destroyed over 700 homes and displaced twice as many people. 

It is unknown what role the water lake has had in the eruption at this time, however according to the above image, it appears to have been vaporized. There appears to be no trace of it in new images, and due to the time of night, is it unclear if a phreatic eruption has occurred, which was hypothesized. 


Current screen grab from HVO's Kilauea Summit Cam



More news will follow.

Right now, you can follow the Facebook page of Hawaii Volcanoes National Park for updates.

Kilauea was previously at Green alert, after a little over two years of quiescence. Following the 2018 eruptive episode, long periods of inflation were recorded, including a recent dike intrusion event. These events were apparently not enough for HVO to become concerned that a new eruption may take place, even though the intrusion was quite shallow, as had been many recent quakes.

Hawaii Island has been hit both by the COVID-19 pandemic, as well as the recent eruption of Kilauea in its Lower East Rift Zone, which erupted in the middle of a neighborhood development, and near a geothermal power planet, the Puna Geothermal Plant. This plant only recently reopened for power generation, and it is unclear whether or not renewed activity at Halema'uma'u will change this.

I expect that the aviation color code will be raised to orange/red, and that the local code be changed accordingly as well in the next USHS HVO Update. 

This is a developing situation, and more updates will be posted as the eruption progresses.

Mauna Loa is also on Yellow alert at this time. A recent deflation event at the summit may or may not have contributed to pressurization of Kilauea, but it is possible. Mauna Loa had been consistently inflating until just a few days ago when a dike intrusion was detected at Kilauea Summit. Whether this is a true correlation is a mystery at this time. 

Residents near the volcano should heed the warnings of local authorities, and evacuate immediately if necessary. Kilauea's behavior of late is not exactly predictable, and quakes have been detected down-rift of last as well. A 2.8 quake, and many smaller magnitude, but still over 2.0 quakes had been detected today down to Mauna Ulu, the site of the eruption preceding that of Pu'u'O'O in 1983.

This is a rapidly developing situation, and many new updates will be posted. 

Hawaiian local news is not yet reporting on the eruption. 






Friday, January 31, 2020

Quake Swarm And Rapid Surface Deformation Continues In Iceland

On Iceland's Reykjanes Peninsula, an ongoing swarm of concentrated temblor activity, coupled with rapid surface inflation is raising the possibility of the first volcanic eruption in nearly two centuries near the famed Blue Lagoon. The area has many geothermal features and is once of Iceland's largest producer of geothermal energy.

According to an article released on January 26th, 2020 on Iceland's Met Office website, "An inflation has been detected since January 21st and is centred just west of Mt. Thorbjorn on Reykjanes peninsula. The inflation is unusually rapid, around 3-4 mm per day and has accumulated to 2 cm to date. It has been detected both on continuous GPS stations and in InSAR images. The inflation is most likely a sign of magma accumulation at a depth of just a few km. If magma accumulation is causing the inflation, the accumulation is very small, with the first volume estimate is around 1 million cubic meters (0,001 km3)."

However, that was then, this is now...

Today's quake sequence now records larger quakes up to magnitude 4.4, with three others measuring 4.0, 3.4 and 3.2. Dozens of smaller magnitude temblors dare occurring at the moment.


Screenshot from Iceland Met Office


Today's activity marks a large increase from the initial activity. While magma accumulation has been confirmed, it is far too soon to say whether this will result in an eruption. The activity after the first rash of quakes subsided significantly in the past few days, but today it has surged with some of the strongest quakes in the sequence to date. 

The town of Grindavik lies near the swarm, as does the Blue Lagoon geothermal pools. If an eruption should occur, it would likely form along a SW-NE trend as a fissure eruption, as is the most common eruption type in this area. The lava would likely resemble a Hawaiian style effusive eruption. The area of activity is related to the Reykjanes volcanic system.

The last confirmed historical eruption in this system was a VEI 3 eruption in March of 1831, with two unconfirmed (VEI 0) eruptions in 1966 and 1970 - although the Smithsonian GVP may consider these to be doubtful. 

The Reykjanes system is part of the Mid-Atlantic rift, a spreading rift between the European and American tectonic plates, of which the entirety of Iceland is a result.

Sunday, January 12, 2020

Taal Volcano in Philippines Has Phreatic Eruption

**LIVE CAM NOW AVAILABLE**



Three hours later, a stronger explosion occurred.

The last major eruption of Taal occured in 1965, which sent pyroclastic flows and tsunami style waves through the lake which surrounds its currently active center. This was one of the Philippines most deadly eruptions.

The current statement from PHIVOLCS is below:




Several social media posts have shown first hand footage and imagery:



The last historical eruption of Taal was in 1977 with a VEI of 2. The largest historical eruption occurred in 1965 with a VEI of 4, killing many.

The new activity suggests there has been new magma injected into the system. This does not necessarily mean that a larger eruption is imminent, but it does typically mean that enough magma that has a heat flashpoint with water got close enough to flash water into steam, creating the latest explosion.

Phreatic eruptions are the result of a minor (or major) volume of water coming into close contact with molten rock. The rock could be older 'crystal mush', or cooler magma which did not have enough gas content to erupt until it came into contact with a water source, or in rare cases fresh magma from the injection source.

Taal volcano has been inflating, and the lake temperatures in the middle vents fluctuating, for years so this eruption is not entirely surprising. PHIVOLCS is monitoring the situation closely, and will be providing updates as soon as they can.

In the last several minutes, it appears an even larger eruption is now underway.



*****UPDATE 1/12/2020*****

Lava fountaining is now observed in the main crater of Taal:



Everyone on the central island has been evacuated. There is not currently an evacuation mandate for the residents around the larger lake (the central crater lake is now completely obliterated).

The latest (Translated to English) update from PHIVOLCS:

"DOST-PHIVOLCS indicates an increase in Alert Level 4 (hazardous eruption imminent) from Alert Level 3 (magmatic unrest) to the current status of the Long Range. Starting at 5:30 pm (PST), volcanic activity is intensified which includes continuous eruption of steam-laden tephra columns with a height of 10 to 15 kilometers with occasional lightning and rainfall. ash extends north of the volcano to Quezon City. Volcanic tremor was also recorded starting at 11:00 am, with two earthquakes of magnitude 2.5 (6:15 pm) and 3.9 (6:22 pm) in Tagaytay City and Alitagtag, Batangas in force Intensity III.

In the event, DOST-PHIVOLCS raises Alert Level 4 to the state of the High Volcano where dangerous eruption is possible within hours to days. DOST-PHIVOLCS strongly recommends total evacuation from Taal Volcano Island and further evasion of hazardous or high-risk areas within a 14-kilometer radius from Taal Main Crater due to possible threat of having a pyroclastic density current (fast waves of very hot smoke and ash) and volcanic tsunami. Areas north of the Taal Volcano are advised to guard and beware of the effects of continuous and long-term rainfall. Civil aviation authorities should advise aircraft to avoid flying around the volcano because of the danger of ash and ballistic fragments from the eruption column. DOST-PHIVOLCS will continue to monitor the Taal Volcano's activity and release an update to the public."

Next update:

"Taal Volcano entered a period of intense unrest beginning with phreatic or steam-driven activity in several points inside the Main Crater at 1:00 PM of 12 January 2020 that progressed into magmatic eruption at 02:49 AM to 04:28 AM of 13 January 2020. This magmatic eruption is characterized by weak lava fountaining accompanied by thunder and flashes of lightning. At 2:00 PM yesterday, booming sounds were heard at Talisay, Batangas.

The Philippine Seismic Network has recorded a total of seventy-five (75) volcanic earthquakes in Taal region as of 5:00 AM, January 13, 2020. Thirty-two (32) of these earthquakes were felt with intensities ranging from Intensity II – V in Tagaytay City, Cabuyao, Laguna, Talisay, Alitagtag, Lemery and Bauan, Batangas. Such intense seismic activity probably signifies continuous magmatic intrusion beneath the Taal edifice, which may lead to further eruptive activity.

Alert Level 4 still remains in effect over Taal Volcano. This means that hazardous explosive eruption is possible within hours to days. DOST-PHIVOLCS strongly reiterates total evacuation of Taal Volcano Island and areas at high risk to pyroclastic density currents and volcanic tsunami within a 14-kilometer radius from Taal Main Crater. Areas in the general north of Taal Volcano are advised to guard against the effects of heavy and prolonged ashfall. Civil aviation authorities must advise aircraft to avoid the airspace around Taal Volcano as airborne ash and ballistic fragments from the eruption column pose hazards to aircraft. DOST-PHIVOLCS is continually monitoring the eruption and will update all stakeholders of further developments."

The following live feed is now available:



*****UPDATE 1/12/2020*****

The interest in Taal volcano has apparently brought he Smithsonian Global Volcano Program (GVP) offline, this is likely due to too much Internet traffic.

*****UPDATE 1/12/2020*****

There is now a live camera provided by rt.com https://www.rt.com/on-air/478090-taal-volcano-eruption-philippines/

*****UPDATE 1/13/2020*****

Taal volcano is still erupting. PHIVOLCS has recommended a 17-km (10.5 mi) exclusion zone around the eruptive center, which covers the towns and villages around the larger Lake Tall. Despite the urgent warnings from PHIVOLCS, some people are sneaking back to their homes in desperation, attempting to grab belongings or livestock.

Heavy ash mixing with rainfall has created a black sludge rain made of ash and mud which is making life miserable for many. The fine ash mixed with water is extremely heavy, so building collapses are now a serious risk. Ash suspended in air is hazardous to breathing, as volcanic ash is made of small volcanic glass shards. Inhaling these seriously damages lungs, so masks are essential.

PHIVOLCS is expecting a larger eruption 'within hours or days', which could end up being as large, or larger, than the eruption of Mt. Pinatubo in 1991.

Their latest update is below:






The main airport is reportedly reopened after the winds shifted to the SW, so there is an opportunity for some to flee the volcano while there is still time.

*****UPDATE FROM PHIVOLCS 1/14/2020  (Philippines Local Time)*****

"For the past 24 hours, Taal Volcano’s activity has been characterized by continuous eruption of the Main Crater due to magmatic and hydrovolcanic activity. This ongoing eruption generated 500-meter tall lava fountains topped by dark gray steam-laden plumes reaching approximately 2 kilometers tall that dispersed ash to the southwest and west of the Main Crater. Flashes of volcanic lightning were observed at the base of the degassing plumes this morning. New vents opened up on the northern flank where short 500-meter lava fountains, and within the main crater where steam plumes, have emanated.

Since the last update, heavy ashfall from the ongoing continuous activity of Taal Volcano has reportedly fallen on the municipalities of Lemery, Talisay, Taal, and Cuenca, Batangas.

The Philippine Seismic Network has recorded a total of two hundred twelve (212) volcanic earthquakes in Taal region as of 2:00 AM, January 14, 2020. Eighty-one (81) of these earthquakes were felt with intensities ranging from Intensity I – V in Tagaytay City, Cavite. Such intense seismic activity probably signifies continuous magmatic intrusion beneath the Taal edifice, which may lead to further eruptive activity.

Sulfur dioxide (SO2) emission was measured at an average of 5299 tonnes/day on 13 January 2020.

Alert Level 4 still remains in effect over Taal Volcano. This means that hazardous explosive eruption is possible within hours to days. DOST-PHIVOLCS strongly reiterates total evacuation of Taal Volcano Island and areas at high risk to pyroclastic density currents and volcanic tsunami within a 14-kilometer radius from Taal Main Crater. Areas in the general north of Taal Volcano are advised to guard against the effects of heavy and prolonged ashfall. Civil aviation authorities must advise aircraft to avoid the airspace around Taal Volcano as airborne ash and ballistic fragments from the eruption column pose hazards to aircraft. DOST-PHIVOLCS is continually monitoring the eruption and will update all stakeholders of further developments."

*****UPDATE 11/14/2020*****

A live video stream is now available at the top of the blog.

PHIVOLCS is now reporting that 'fissures and cracks' have appeared SW of Taal Volcano Island, near the coastal cities. This could mean that the magma intrusion under Tall extends beyond the boundaries of the larger caldera Lake Taal. This of course could mean that a much larger eruption is possible.

I did look up the names of the mentioned towns on Google Earth, and all but one were closely clustered to the SW, which may suggest that these reports are accurate, and that new cracks and fissures are opening up a long distance from the central eruptive vent. Time will tell. If this is true, the magma chamber has made multiple paths to the surface, and effusion of lava will be likely.