EtnaUpdater @EtnaUpdater@qoto.org

Etna update, 10/03/2023

In the last week, most of the gas continued to be released at Mt Etna's Bocca Nuova. At times, gas emissions were intensified in a pulse-like manner. At the Southeast Crater complex, fumaroles persistently released gas along the inner walls of the crater located between Old and New Southeast Craters. Gas and steam were also persistently emitted along the upper northern summit area of New Southeast Crater. There, light sensitive webcams also continued to show some pulsating glow, likely generated by rising heat.
At Voragine and Northeast Crater, I still could not detect any significant gas emissions.

Analysis of the GPS station data showed no significant changes for the period between 20 February and 05 March [1, 2].
Clinometric data showed no significant changes in the slope of the volcano building between 20 Feb and 05 March [1, 2].

Due to strong winds, the measurement of infrasound activity at the summit craters was so much affected in the period between 20 Feb and 05 March that no reliable data could be obtained [1, 2].

Sulfur dioxide emissions at the summit craters remained unchanged in the period between 20.02. and 05.03. compared to the previous week and were at medium levels.
Soil carbon dioxide emissions (ETNAGAS station) hovered around the border between low and medium levels between 20.02. and 05.03. [1, 2].
The concentration of helium isotopes (3He/4He - ratio) in the Etna area, last determined on 22 February, was slightly lower than the last measurement, with a value of 0.61. The measured value continues to be at a high level [1].

Online seismograms from the ECNE station showed only sporadic, weak signals between February 25 and March 10.
The tremor decreased somewhat on 26 February and has since been subject to a slightly increasing trend. Currently, it is at a medium level [3].

On 26.02. an earthquake of magnitude 1.5 was registered at Zafferana (southeast flank). On 28.02. an earthquake of the same magnitude occurred there. On 28.02. two quakes occurred at Monte Fontane (eastern flank) reaching magnitudes of 3.2 and 1.8, respectively. On March 01, two earthquakes with magnitudes of 2.2 and 2.3 occurred in the area northwest of Adrano and southwest of Bronte (western flank), respectively. On March 01, an earthquake of magnitude 1.7 was measured at Monte Palestra (western flank). On 01.03. a small series of earthquakes occurred in the area north of Monte Collabasso (northern flank). The strongest quake reached a magnitude of 1.6 [4].

1 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 20/02/2023 - 26/02/2023
2 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 27/02/2023 - 05/03/2023
3 - INGV-Sezione di Catania. 2023. Home. TREMORE VULCANICO. ECNE
4 - INGV. Osservatorio Etneo. Sorveglianza e Monitoraggio. DATABASE TERREMOTI. Localizzazioni di sala operativa. 2023.

#Etna #volcano

Etna update, 24/02/2023

During the last week, Mt Etna remained quiet with the usual gas emissions from the summit craters. Seismic activity was low, but tremors remained elevated.

During the past week, gas emissions from Etna's summit craters continued to be concentrated at Bocca Nuova. They appeared relatively intense and were pulse enhanced. However, I could no longer detect any glow above the summit crater. At the Southeast Crater Complex, gas was emitted persistently from the crater between the old and new southeast craters. This made it's way to the surface mainly from fumaroles located along the inner crater walls. Gas was also persistently emitted from the summit area of New Southeast Crater. Light sensitive webcams showed faint glow just below the northern crater rim, where many fumaroles and a small vent from the May/June 2022 eruption are located.
At Voragine and Northeast Crater, on the other hand, I continued to observe virtually no gas releases.

Analysis of the GPS station data showed no significant changes for the period between 13 and 19 February [1].
Clinometric data showed no significant changes in the slope of the volcanic edifice between February 13 and 19 [1].

Measurement of infrasound activity at the summit craters showed only a small number of events for the period from February 13 to 19 [1].

Sulfur dioxide emissions at the summit craters remained unchanged from the previous week during the period between Feb. 13 and Feb. 19 and were at intermediate levels.
Ground carbon dioxide emissions (ETNAGAS station) hovered just above the boundary between low and medium levels between Feb. 13 and Feb. 19 [1].

Online seismograms from station ECNE showed only isolated weak signals during the past week.
The tremor was on the border between low and medium level during the past week [2].

On 23.02. an earthquake of magnitude 1.5 was registered south of Monte San Leo (southern flank) [3]

1 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 13/02/2023 - 19/02/2023
2 - INGV-Sezione di Catania. 2023. Home. TREMORE VULCANICO. ECNE
3 - INGV. Osservatorio Etneo. Sorveglianza e Monitoraggio. DATABASE TERREMOTI. Localizzazioni di sala operativa. 2023.

#Etna #volcano

Today my time travel on #throwbackthursday goes back to June 2008. I am on the island of Vulcano on the terrace of the Hotel Eolien and enjoy the sunset over the bay of Porto Ponente with antipasti and white wine. Simply dreamlike!

#aeolian #vulcano #photo

Etna update, 17/02/2023

During the past week, Mt Etna remained relatively quiet, with the usual gas releases from Bocca Nuova and the Southeast Crater complex. Deep-seated explosions probably occurred in Bocca Nuova. The tremor still remained somewhat elevated. Seismic activity, however, was low.

Last week, initially very bad weather with large amounts of snow and storms prevented the observation of Etna by webcams. Even after an improvement in the weather from 14 February, many cameras were still down. The available webcams showed that lava was still not being produced at the New Southeast Crater. There was continued emission of gas and steam in the summit area of the cone. During the nights, faint glow smoke was visible just below the northern rim of the crater. A fumarole field is located here, as well as fractures and a former vent that was active during the May/June 2022 eruption.
Otherwise, Bocca Nuova continued to release gas vigorously and in pulses. During the night of 16 February, faint glow was sporadically visible above the summit crater by means of light-sensitive webcams. Last night, the glow intensified and became more frequent. Probably deep-seated explosions occurred. I was still unable to detect any significant gas emission from the northeast crater and Voragine.

The evaluation of the data from the GPS stations showed no significant changes for the period between 06 and 12 February [1].
The clinometric data did not show any significant changes in the slope of the volcano building between 06 and 12 February [1].

The measurement of infrasound activity at the summit craters was strongly disturbed by very bad weather in the period from 06 to 12 February. Overall, there was a slight decrease in infrasound activity. The source of the events was Bocca Nuova [1].

Sulphur dioxide emissions at the summit craters increased somewhat in the period between 06.02. and 12.02. and were at a medium level.
Ground carbon dioxide emissions (ETNAGAS station) increased slightly between 06.02. and 12.02. and reached near-medium levels [1].

The online seismograms of station ECNE showed only single weak signals last week, after initial interruption due to bad weather [2].
The tremor fluctuated on the border between low and medium level during the past week [2].

On 13.02., a quake of magnitude 1.9 was measured south of Monte San Leo (southern flank) [3].

My interpretation of the data and speculations about the further development:
So now the effusive activity at the northeastern base of New Southeast Crater, which started at the end of November 2022, has come to an end again. This was already indicated from mid-January, when the production rate began to show greater fluctuations. A total of about 6 million m3 of lava was produced, which is a relatively small amount in comparison. Analyses of the lava produced in December showed that it was more highly developed material, which was also evident from the low explosive activity. The magma had probably been stored in the mountain for some time and was able to degas via the summit craters. Then it found an outlet at the end of November and an eruption occurred. Probably also because the mountain slowly expanded due to the rising magma and probably more magma rose than could be stored within the volcanic structure. The still high readings for the helium 4 isotope show, in my opinion, that there is still plenty of fresh magma flowing in under the mountain. A small part of it will probably continue to rise in the mountain and sooner or later lead to new eruptive activity. It is not yet possible to say what this will look like. It is quite possible that the quiet eruptive activity of last winter will be repeated in a few months. However, if more gas is involved or if this has no possibility of degassing, there may also be strombolian explosions at the Southeast Crater complex. A new phase of paroxysmal eruptions cannot be completely ruled out either. So let's just be surprised what the old lady has in store for us this time!

1 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 06/02/2023 - 12/02/2023
2 - INGV-Sezione di Catania. 2023. Home. TREMORE VULCANICO. ECNE
3 - INGV. Osservatorio Etneo. Sorveglianza e Monitoraggio. DATABASE TERREMOTI. Localizzazioni di sala operativa. 2023.

#Etna #eruption #volcano #lava

Photo by INGV Catania

Etna update, 10/02/2023

Effusive activity at the northeastern base of Mt Etna's New Southeast Crater ended last week. However, the tremor has weakened only slightly and seismic activity has increased somewhat.

On 04 February, the effusive vent at the northeast base of New Southeast Crater continued to feed a lava flow. This moved northward through the Valle del Leone. On the evening of 04 February, a partial flow began to descend the steep western slope of Valle del Bove. During the night of 05 February, its front descended to an altitude of about 2300 m and moved in the area southwest of Monte Simone. In the morning of 05 February, the partial flow did not seem well fed and began to retreat. Bad weather hindered further observation until 06 February. Then, in the morning of 06 February, the entire lava field was inactive. The same picture was seen on the following days, with observations increasingly hindered by clouds and fresh snow.
At New Southeast Crater, the northern summit area showed weak pulsating glow during the nights until 05 February, apparently caused by deep-seated explosions. Gas and steam were also persistently emitted from the summit area of New Southeast Crater.
At Bocca Nuova, strong and often pulsating gas emission continued. At the other summit craters, only weak gas emissions occured.

As reported by INGV, a volume of 4.8 to 6.1 million m3 of lava was emitted by February 03. This occupied an area of about 960,000 m2 [1].

Analysis of the data from the GPS stations showed no significant changes for the period between 30 January and 05 February, but the trend toward slight deflation of the volcanic edifice that began in mid-December continued [1].
Clinometric data showed no significant changes in the slopes of the volcanic edifice between January 30 and February 05 [1].

The measurement of infrasound activity at the summit craters showed an increase in events between 30 Jan - 05 Feb compared to the previous week. However, the measurements were at times affected by strong winds. The source of the activity was Bocca Nuova and Southeast Crater [1].

Sulfur dioxide emissions at the summit craters increased somewhat during the period between 30 Jan and 05 Feb and were at intermediate levels.
Ground carbon dioxide emissions (ETNAGAS station) fluctuated at low levels between 30 Jan and 05 Feb.
The concentration of helium isotopes (3He/4He - ratio) in the Etna area, last determined on 03 Feb, was comparable to the last measurements with a value of 0.63. The measured value was on a high level [1].

On the online seismograms of station ECNE, weak long-period signals were visible every few minutes during the past week.
The tremor decreased slightly on 04 February and since then has been just above the boundary between low and medium levels [2].
As reported by INGV, the source of the tremor in the period between 30.01. and 05.02. was at about 2000 - 2800 m altitude in the area below the central crater [1].

On 05.02. a small series of earthquakes occurred in the area northwest of Adrano (western flank). The strongest tremors reached magnitudes of 2.5 and 3.7, respectively, and occurred at depths between 12 and 15 km. On 06.02. an earthquake of magnitude 1.6 was recorded near Biancavilla (southern flank) [3].

1 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 30/01/2023 - 05/02/2023
2 - INGV-Sezione di Catania. 2023. Home. TREMORE VULCANICO. ECNE
3 - INGV. Osservatorio Etneo. Sorveglianza e Monitoraggio. DATABASE TERREMOTI. Localizzazioni di sala operativa. 2023.

#Etna #eruption #volcano #lava

Today, my time travel on #throwbackthursday takes me back to 2008, to a holiday I spent on the Aeolian Islands, north of Sicily. The photo shows the crater "Grand Cratere" on the island of Vulcano. In the background you can see the northern part of the island with the cone of Vulcanello. Behind it are the islands of Lipari and Salina.

#aeolian #vulcano #lipari #salina #volcano #photo

Etna update, 03/02/2023

Last week, the effusive vent at the northeast base of Mt Etna's New Southeast Crater continued to release lava. However, the flowrate fluctuated significantly.
On 28.01., the front of the lava flow initially stagnated at about 2300 m altitude. On 29.01. it retreated to the rim of Valle del Bove at about 2500 m, but during the day a new partial flow developed, which now took a slightly more southerly course. On January 30, the southern branch descended a few hundred meters down the escarpment of Valle del Bove, and the northern branch also became better fed. On January 31, the flows stagnated or retreated again. On the other hand, the southern stream was well fed on 01 February and widened significantly. During the night of February 02, the lava flow decreased significantly and during the day practically no strong thermal anomalies were visible. Towards evening, however, a new surge of lava set off again. Today, the new lava flow continued to move slowly northward through the Valle del Leone.
Meanwhile, in the summit area of the New Southeast Crater, gas was emitted persistently, but in contrast to the previous week, only few ash was visible. Instead, pulsating glow was visible in the upper northern section of the cone during the nights on light sensitive webcams. Presumably, the escaping steam was illuminated from below, from the depth of the vent. Whether this was caused by deep-seated explosions or simply by heat remained unclear.
During last week Bocca Nuova released the most gas of the summit craters. Again, the emissions were pulse-like enhanced and at least once a gas ring was observed. At Voragine and Northeast Crater only weak gas emission was visible.

As reported by INGV, a volume of 4.4 to 5.6 million m3 of lava was emitted by January 29. This occupied an area of about 880,000 m2 [1].

The analysis of the data from the GPS stations showed no significant changes for the period between January 23 and 29. However, the slight deflation already observed in recent weeks continued [1].
Clinometric data showed no significant changes between January 23 and 29 [1].

The measurement of infrasound activity at the summit craters in the period between January 23 and 29 showed a low number of events. However, there was a slight increase in explosive activity in the last days. The source of the events was the Bocca Nuova [1].

Sulfur dioxide emissions at the summit craters were at intermediate levels during the period between 23 and 29 January.
Ground carbon dioxide emissions (station ETNAGAS) decreased slightly between 23 and 29 Jan, reaching low levels [1].

Weak long-period signals were occasionally visible on the online seismograms of station ECNE during the past week [2].
The tremor fluctuated in the lower range of the mean level during the last week and was subject to a slight increasing trend during the last days [2].
As reported by INGV, the source of the tremor in the period between 23 and 29 January was at about 2400 - 2800 m altitude in the area below Southeast Crater [1].

On 28.01. an earthquake of magnitude 1.7 was registered at Pizzi Deneri (northeast flank). On 02.02. an earthquake of magnitude 2.0 occurred at Pozzillo (eastern flank) [3].

1 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 23/01/2023 - 29/01/2023
2 - INGV-Sezione di Catania. 2023. Home. TREMORE VULCANICO. ECNE
3 - INGV. Osservatorio Etneo. Sorveglianza e Monitoraggio. DATABASE TERREMOTI. Localizzazioni di sala operativa. 2023.

#Etna #eruption #volcano #lava

Once again I look back on an eruption of Mt Etna on #throwbackthursday .I took the photo in the evening of 18 July 2006. Watching the eruption of Southeast Crater at sunset was an unforgettable experience.

#Etna #eruption #lava #volcano #photo

At the eruptive fissure of 2008, Mt Etna May 2009

#VolcanoMonday #photomonday #Fotomontag #photo #etna

Etna update, 27/01/2023

During past week, lava continued to be released at the northeast base of Mt Etna's New Southeast Crater, but the production rate was subject to strong fluctuations. Tremor and seismic activity remained inconspicuous.

After the mountain had been completely wrapped in clouds all day on 22 January, the Monte Cagliato thermal camera showed a significant weakening of the lava flow on 23 January. This had previously been released from the effusive vent at the northeast base of New Southeast Crater in an easterly direction. Only some spots of the flow, which had previously stagnated at the base of the steep western wall of Valle del Bove, were still hot. Then, on the morning of 24 January, a new powerful thermal anomaly appeared just below the effusive vent. It was caused by a new gush of lava that poured eastwards again over the meanwhile cooling flow of the previous days. The new lava flow progressed slowly and on the morning of 25 January its front stagnated at the edge of the Valle del Bove, above the escarpment. Later, clouds moved in again and hid the mountain until the morning of 26 January. Through gaps in the clouds it was visible that the flow continued to stagnate and had even weakened somewhat compared to the previous day. In the evening of 26 January, the thermal anomalies below the effusive vent intensified and again a surge of fresh lava started moving eastwards. During the previous night, this flow then moved down the steep western wall of the Valle del Bove and reached about 2300 m high terrain in the morning. As the day progressed, however, the front stagnated again and this evening the lava flow did not look quite as well fed as yesterday.
At the summit craters, Bocca Nuova again showed the most gas emission last week, which was still frequently intensified in a pulse-like manner. Voragine and Northeast Crater continued to release only few amounts of gas. At the New Southeast Crater, gas was persistently emitted from the summit area. In the morning of 26 January, some brownish ash clouds mixed with the gas clouds from about 11:30. Around 14:45 I could see an even stronger ash emission there, which was nevertheless comparatively weak. The point of emission was apparently the upper northern summit area, which also generated some weak glow at times during the nights of the last weeks.

The volume of lava released since 27 November is calculated by INGV to be 3.7 - 4.8 million m3.
In the meantime, a sample of the current material, taken on 20 December 2022, was chemically analysed. It showed that the lava, with a CaO/Al2O3 ratio of 0.46 and an FeOtot/MgO ratio of 3.3, was more evolved than the lava emitted in 2022 during the paroxysmal phases of the Southeast Crater complex or during the May eruption. According to the INGV, this means that hardly any material was produced from greater depths [1].

The evaluation of the data from the GPS stations showed no significant changes for the period between 16 and 22 January [1].
The clinometric data showed no significant changes between 16 and 22 January [1].

The measurement of infrasound activity at the summit craters was massively disturbed by strong winds during the period 16 - 22 January and thus no data could be provided [1].

Sulphur dioxide emissions at the summit craters remained unchanged in the period between 16 and 22 January compared to the previous week and remained in the lower-medium range.
Soil carbon dioxide emissions (ETNAGAS station) held at medium levels between 16 and 22 January and were subject to a slight downward trend [1].

On the online seismograms of station ECNE, weak long-period signals as well as weak explosion signals were occasionally visible during the past week [2].
The tremor initially hovered on the border between low and medium levels last week, but then increased slightly and remained at lower-medium levels [2].

On 22.01., a quake of magnitude 1.6 was registered southeast of Monte Fontane (eastern flank). On 25.01., a quake of magnitude 1.7 occurred in the area of the summit craters [3].

My interpretation of the data and speculation about further development:
The analysis of the lava released in December showed that it was more evolved than the lava from the May 2022 eruption and significantly higher than the material emitted from New Southeast Crater during the paroxysmal phases in February 2022. This is also not surprising, because it was already largely degassed magma that generated practically no explosive activity, but flowed out very quietly. This magma had been stored in the mountain for some time and had time to evolve.
Unfortunately, there is no analysis (yet) of the lava currently being released. It is quite possible that it is somewhat more primitive than the December lava. However, as there is still no significant explosive activity, the proportion of more highly evolved and degassed magma still seems to be high. However, this could change in the near future and fresher magma could reach the surface.
Yesterday there were some ash emissions in the summit area of New Southeast Crater. It is possible that these were caused by deep-seated explosions, but smaller collapse events are more likely. However, if more fresh magma rises, the gases could cause strombolian explosions in the New Southeast Crater. Perhaps the ash emissions yesterday were already a first indication? Interesting is also the currently strongly fluctuating emission rate; a behaviour that has prevailed since mid-January and always causes new lava spurts. This could also be an indication that another, more gas-rich magma is now beginning to rise. But it could also mean that sufficient pressure can no longer build up to produce lava on a sustained basis. The temporary sinking and rising of the magma column under the New Southeast Crater could then also generate collapse events.
Thus, in my opinion, two developments are conceivable in the near future: 1. onset of strombolian explosions in the summit area of New Southeast Crater, with lava emission at the effusive vent remaining intensified in a push-like manner. 2. weakening or even end of the eruption and collapse events in the summit area or along the northern flank of New Southeast Crater associated with ash emissions.
In any case, Etna remains exciting!

1 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 16/01/2023 - 22/01/2023
2 - INGV-Sezione di Catania. 2023. Home. TREMORE VULCANICO. ECNE
3 - INGV. Osservatorio Etneo. Sorveglianza e Monitoraggio. DATABASE TERREMOTI. Localizzazioni di sala operativa. 2023.

#Etna #eruption #volcano #lava

Once again, I look back at an interesting stay on Mt Etna on #throwbackthursday. On the afternoon of 01 August 2012, I climbed the summit craters, where strombolian explosions had been occurring in the Bocca Nuova since the beginning of July. I stayed until nightfall and was able to take great photos of the activity.

#etna #volcano #photo #lava

Ice and ash, Mt Etna May 2009

#VolcanoMonday #photomonday #Fotomontag #photo #etna

Etna update, 20/01/2023

Last week, lava emission at the north-eastern base of Mt Etna's New Southeast Crater temporarily decreased. As a result, a new lava flow developed, which is now heading directly towards Valle del Bove.

On 14 January, the fronts of the lava tongues fed by the effusive vent at the northeastern base of New Southeast Crater stagnated at about 2200 - 2300 m altitude. During the evening, the associated thermal anomalies recorded by the Monte Cagliato thermal imaging camera weakened more and more. On 15 January, the lava flow was only active in the upper section, within the Valle del Leone. On 16 January, new small lava tongues were again working their way down the steep western slope of the Valle del Bove, but were no longer as well fed as in the previous weeks. On 17 January, only very small thermal anomalies were visible and it looked as if the lava emission had stopped completely. On the morning of 18 January, a new thermal anomaly appeared near the effusive vent. A new lava flow was now moving in an easterly direction, leaving the previously created lava field. By the evening of 19 January, the lava flow had continued on its easterly course, but progressed slowly despite the steepening terrain. This morning, its front stagnated at a roughly estimated altitude of about 2400 metres. Later, clouds moved in and hindered further observation.
Meanwhile, the summit craters continued their usual gas emissions during last week. They were strongest at Bocca Nuova and often pulsed. At New Southeast Crater, some gas was persistently emitted from the summit area. At Voragine and Bocca Nuova no gas emission was visible.

As INGV reports, the front of the most advanced lava flow was observed on 14 January at 2250 m elevation. By 14 January, a lava field with an area of 700,000 m2 had developed. The volume was calculated at 3.5 - 4.5 million m3 [1].

The analysis of the data from the GPS stations showed no significant changes for the period between 09 and 15 January [1].
The clinometric data did not show any significant changes in the Inclinations of the volcano between 09 and 15 January [1].

The measurement of infrasound activity at the summit craters was frequently disturbed by strong winds during the period 09 - 15 January. During the calm phases, activity similar to that of the previous week was recorded [1].

Sulphur dioxide emissions at the summit craters remained at the lower-medium level during the period 09-15 January.
Ground carbon dioxide emissions (station ETNAGAS) remained at a medium level between 09 and 15 January and were subject to only minor fluctuations.
The concentration of helium isotopes (3He/4He - ratio) in the Etna area, which was last determined on 09 January, was with a value of 0.63 similar to the last measurement in December. The value was thus still at a high level [1].

On the online seismograms of the ECNE station, weak explosion signals as well as individual long-period signals were regularly visible during the past week. From 18 January, there were also repeated phases of stronger noise that lasted only 1 - 3 minutes [2].
The tremor fluctuated between low and medium levels during the past week. The strongest decrease occurred on 17 January. Subsequently, the tremor increased again somewhat [2].
The source of the tremor was located between 09 and 15 January in the area below the central crater at an altitude between 1000 m and 2800 m [1].

My interpretation of the data and speculations about the further development:
The tremor was subject to some fluctuations in the last few days and the rate of lava production temporarily decreased significantly on 17 January. This could indicate that the supply of fresh magma to the effusive vent is gradually stalling. Presumably, not enough magma is rising at the moment or it has sought another path in the mountain along which it is migrating. Sulphur dioxide emissions from the summit craters have also been declining in recent weeks and there has been slight deflation of the volcanic edifice.
This suggests, in my opinion, that the current eruption may be slowly coming to an end. However, the still high Helium-3 concentration shows that fresh magma continues to rise under the mountain, which will be erupted sooner or later, at least in part. So it remains difficult to make a prognosis.

1 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 09/01/2023 - 15/01/2023
2 - INGV-Sezione di Catania. 2023. Home. TREMORE VULCANICO. ECNE

#Etna #lava #eruption #volcano

@ZenobiaVayne

I have tried to introduce #VolcanoMonday here. Unfortunately, there has been no participation so far, but of course there aren't that many people here who have any photos at all.

Etna update, 13/01/2023:

Last week, lava emission continued at the effusive vent at the northeast base of Mt Etna's New Southeast Crater. Different partial flows continued to be fed, moving through a system of tunnels and channels to the rim of the Valle del Bove. There, the fronts of two or three lava flows stagnated at about 2100 m above Monte Simone. From 08 January, the tongues retreated. Bad weather with fresh snow hampered observations until 10 January. From 11 January visibility was very good again and the hot, fan-shaped lava field stood out very well as a dark area on the snow-covered mountain. During the day, the fronts of the lava tongues descended again a little further down the slope and reached about 2200 m high terrain.
On 12 January, the southernmost lava tongue advanced even further down the slope, but then stagnated today at about 2100 - 2200 m high terrain.
Meanwhile, the usual gas emissions continued at the summit craters of Etna, which were still strongest at Bocca Nuova. During the nights, however, I could no longer observe any glow there. On the other hand, from 11 January onwards, some glow appeared on light sensible webcams in the upper northern summit area of New Southeast Crater. This was probably caused by rising heat or high-temperature fumaroles.

As reported by INGV, the front of the most advanced lava flow reached 2170 m high terrain between 04 and 07 January. The average production rate could be estimated at about 3 m3 lava/s with the help of satellite data. On 07 January, the volume of lava produced since the beginning of the eruption on 27.11.2022 was calculated to be about 2.5 - 4.3 million m3 [1].

The evaluation of the data from the GPS stations showed no significant changes between 02 and 08 January. However, the slight trend towards deflation of the volcanic edifice continued [1].
The clinometric data showed no significant changes in the slopes of the volcano between 02 and 08 January [1].

The infrasound activity at the summit craters was characterised by a relatively high frequency of events in the period from 02 - 08 January. However, the amplitude was low, indicating weak to moderate activity. The source of the events was Bocca Nuova [1].

The sulphur dioxide emissions at the summit craters decreased slightly in the period between 02 and 08 January compared to the previous week and were in the lower medium level.
Ground carbon dioxide emissions (station ETNAGAS) remained at a medium level between 02 and 08 January and were subject to only minor fluctuations [1].

The online seismograms of station ECNE showed occasional weak explosion signals or long-period signals during the past week.
The tremor was initially still on the border between low and medium levels last week, but then rose again somewhat from 10 January and has been slowly decreasing since then [2].
Until 05 January, the source of the tremor was located at an altitude of 2700 - 2900 m in the area between Southeast Crater and the effusive vent. From 05 January on a shift to the area northwest of Southeast Crater at an altitude of 2300 - 2700 m was detected [1].

On 07.01. a quake of magnitude 1.5 was recorded in the area of Grotta del Gelo (northern flank). On 12.01., two earthquakes with magnitudes of 2.3 and 1.9 were recorded near Biancavilla (southern flank) [3].

1 - INGV-Sezione di Catania. 2023. Etna - BOLLETTINO SETTIMANALE - SETTIMANA DI RIFERIMENTO 02/01/2023 - 08/01/2023
2 -INGV-Sezione di Catania. 2023. Home. TREMORE VULCANICO. ECNE
3 - INGV. Osservatorio Etneo. Sorveglianza e Monitoraggio. DATABASE TERREMOTI. Localizzazioni di sala operativa. 2023.

#Etna #eruption #volcano #lava