Volcanic eruption on La Palma in 2021

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Eruption crater with lava flow towards El Paraiso (September 20, 2021)
La Palma: Location of the volcanic eruption and the lava flow (as of November 23, 2021)

The volcanic eruption on La Palma in 2021 began on September 19, 2021 on the western slope of the north-south mountain ridge Cumbre Vieja on the Canary island of La Palma . Its eruption points are between 900 and 1000 m above sea level, about 1200 m east of the old volcano Montaña Rajada and 1700 m northwest of the Llano del Banco volcano , one of three volcanoes of the San Juan eruption in 1949 .

There were several chimneys at two longer crevices from which lava fountains emerged. The lava flowed westwards down the slope to the sea and destroyed a large number of houses in villages and scattered settlements in the communities of El Paso , Los Llanos de Aridane and Tazacorte . Todoque (part of the municipality of Los Llanos de Aridane) was particularly hard hit .

The eruption is considered to be the longest known eruption of a volcano on La Palma. By December 13, 2021, the outbreak lasted 85 days and 18 hours. So far, the eruption of the Tehuya volcano in 1585 with 84 days was considered the longest on the Atlantic island. No reliable data is available on previous outbreaks.

Volcanic characteristics

It is a fissure eruption with a Strombolian character and interspersed water vapor explosions . Several chimneys created one after the other are grouped in a line along an underground system of columns. In addition, there is a strong effusive component in which abundant lava flows emerge, sometimes from several openings at the same time.

During the explosive event, volcanic gas and volcanic ash are emitted, which pile up in eruption columns up to 5000 m high and can be widely distributed. The frequently seen lava fountains reach a height of 600 m. The pyroclastic material in the form of welded lava fragments , ash, lapilli and volcanic bombs builds up a cinder cone over time, the flanks of which repeatedly collapse. The lava from the lava lake inside the crater is suddenly released, which leads to spectacular lava cascades and the loss of blocks as high as a house.

Course of the volcanic eruption

prehistory

For decades there were no earthquakes announcing volcanic eruptions on La Palma. More recently there have been earthquakes only southeast of Tenerife and on El Hierro. On La Palma there were tremors only on February 19, 2013. A first noticeable quake took place on February 10, 2014 with a magnitude of 3.7. Larger swarmquakes that were not noticeable occurred from October 7th to 14th, 2013 and from February 11th to 15th, 2018.

The last larger swarms of earthquakes occurred from January 30th to February 2nd and from June 25th to 27th, 2021.

The three affected communities (from right to left):
El Paso , Los Llanos de Aridane and Tazacorte
underlined in red : village (additionally outlined in red) or settlement
cores covered by the lava purple words and lines : names and boundaries of the districts (barrios)

September 2021

Exit points (black) and spread of the lava (red)
(date: see situation as of ... in the picture legend at the top)

On September 11th, a more intense swarm of earthquakes began to rise over the next few days, which was interpreted as an indication of a possible impending volcanic eruption on the Cumbre Vieja.

The further increase in seismic activity prompted the authorities on September 13 to activate the "Volcanic Emergency Plan" (PEVOLCA) and to switch the volcanic traffic light for the communities on the west side of the Cumbre Vieja from green to yellow. Associated with this were instructions on how the affected residents should prepare for a possible evacuation.

On the morning of September 19 , in addition to the numerous weaker earthquakes , there were also five shallow earthquakes that were above magnitude 3.0, the strongest with 3.8 mbLg. Later, around 4:00 p.m. CEST, the volcanic tremor rose sharply. The feared volcanic eruption then began at 4:12 p.m. CEST (3:12 p.m. local time, 2:12 p.m. UTC) at an altitude of about 920 m above sea level in Barrio Tacande in the municipality of El Paso . That was about 5 km further north than the respective epicenter of most of the recorded earthquakes. The centers of the last quakes were only 1 km deep. Initially, lava fountains formed in two longer crevices in several places and two lava flows flowed westwards down the lightly wooded slope towards the inhabited area. After an hour, an ash cloud formed above the first eruption site, which reached a height of 1,500 m.

The authorities set the warning level to red and began evacuating the endangered towns west of the outbreak site. In addition, the disaster management mission (EMSR546: Volcano eruption in La Palma, Spain) of the Copernicus earth observation program was started in order to record the effects of the eruption.

On the evening of September 20, a new eruption fissure opened a little further north, 700 m from the previous eruption center. Subsequent settlements in the north in the barrios Tajuya and Tacande were evacuated. A total of 6,000 residents were affected by the evacuations.

On September 22nd, the lava front, with a thickness of 8 to 15 m, only advanced at a speed of 4 m / h. The first maps of the Copernicus mission were published showing the extent of the lava flow and the destruction of 320 houses.

On September 23 350 houses were destroyed, according to the Copernicus mission; the lava covered an area of ​​166 hectares. The uplift caused by the rising magma stabilized at a maximum of 28 cm.

On September 24th, the tremor increased significantly. The eruption increasingly turned into an explosive phase. At 3:15 p.m. there was a big explosion. A Wilson cloud was seen on video . In the explosion, window panes in the area were broken. As a result, the crater developed cracks and a new eruption fissure with fast flowing lava opened up. Due to the many explosions, the ash cloud increased, and due to a change in the wind direction, ash also fell on the east side of the island. The area around the volcano was covered with a thick layer of ash and lapilli . The ash cloud reached 3500 m. The Spanish Prime Minister Pedro Sánchez , who made himself a picture of the situation on site, promised financial compensation for the destroyed houses and also for the lost belongings. According to RTVC / TelevisionCanaria, 452 houses had already been destroyed in the evening.

On September 25, there was a partial collapse of the new volcanic cone, with part of the western flank slipping off.

On September 26th, the northern lava flow was reactivated at its previous end. A few days earlier he was in Todoque only about 30 meters in front of the church on the main road (LP 213) San Pío X stopped. The church fell victim to lava rolling on the afternoon of September 26th and was completely destroyed. On the steep coast near the port of Tazacorte, a small rock slide may have occurred due to the ongoing tremors from the volcano on the island , in which masses of stones fell into the sea. According to an evaluation of stereo images from the Pléiades earth observation satellites, the lava covered an area of ​​262 hectares at an average height of 12 m and a maximum height of 50 m.

On September 27th there was a rest period of several hours for the volcano. Between 6 and 7 a.m. local time, the volcanic tremor and the eruptions at the volcanic vent decreased. During the day there were only minor ash eruptions. Between 5 p.m. and 6 p.m. local time the volcanic tremor increased again and shortly after 6 p.m. local time new eruptions followed, initially mainly with ash ejection and about an hour later again of the strombolian type .

Spread of the lava on certain days in September (continuously from right to left)

However, on September 28 , the Instituto Geográfico Nacional determined that one of the volcanic exits in the northern part of the volcano had changed its activity and therefore the Hawaiian type of volcanic eruption now predominates. In this type of eruption, the process is usually quieter because the lava is even more fluid, the gases are easily released and there are no explosions. As a result, large amounts of lava emerged; the lava reached the coast at Playa Nueva on the night of September 29 and flowed into the Atlantic. As a result, the coastal and last still open road connection between north and south on the west side of La Palma was interrupted. The government in Madrid declared La Palma a disaster area. During the day, the lava pushed an estuary 500 m wide out into the sea. It is located about 1 km (center to center) north of the lava platform formed in the 1949 San Juan eruption . The area of ​​the island has increased by 17.2 hectares due to the lava emergence; the lava has flowed 24 m deep into the sea there. The rest of the lava flows are practically inactive. According to the Copernicus Mission on September 29, a land area of ​​338.3 hectares was covered by lava; the ash ejection affected 1753 hectares. So far 981 buildings have been affected by the lava flow, of which 855 have been destroyed. The Institute for Geosciences (IGEO) published for the first time the current classification of the eruption in level 2 on the scale from 0 to 8 of the volcanic explosion index (VEI).

October 2021

On October 1st , 18 earthquakes with a magnitude of 2.0 to 3.6 were registered, four of them stronger than 3.0, as many as in the previous days. More intense volcanic activity resulted, inter alia. to break up two new crevices at a distance of only 15 m from each other, about 600 m northwest of the active volcanic cone in an already inhabited area. The new lava flow destroyed other parts of El Paraíso before it later rejoined the main flow. The new lava delta has already advanced 475 m into the sea, with a maximum depth of 30 m, and now covers an area of ​​27 hectares.

On the evening of October 3 , part of the western crater wall collapsed, causing the inner lava lake to be buried and larger blocks to be carried away by the flowing lava. Increasing explosive activity hurled several decimeter large lava bombs up to 800 m.

On October 5th , the number of destroyed buildings was corrected downwards considerably by comparing them with the cadastral data. By October 4, 726 buildings had been destroyed, including 605 residential buildings. The evaluations of the Copernicus satellite data showed 1046 destroyed buildings, but could not distinguish their type.

Spread of the lava on certain days in October (1st half, continuously from right to left)
Spread of the lava on certain days in October (2nd half, continuously from right to left)

On the night of Saturday, October 9, part of the northern flank of the old crater collapsed. More lava flows were created. In the course of Saturday other structures collapsed on the north side, thinner lava emerged in several streams and in even larger quantities. In the process, boulders the size of multi-story houses drifted down the lava flow.

On October 10, the new lava flow destroyed the few remaining buildings on the northern edge of Todoque. The number of destroyed houses increased to around 1200. Further areas of the banana plantations in the very south of Tazacorte near Playa Nueva , which owe their existence to the volcanic eruption of 1949, were buried by the southern tongue of lava.

By October 21, around 7,500 people had to be evacuated since the volcano erupted. 2185 buildings had been destroyed by then. By October 21, the lava masses had spread to 866 hectares and had penetrated to La Laguna, which is adjacent to Todoque to the north .

On October 26th , the IGN announced that at the measuring station LP03 at Jedey an inflation of 10 cm had taken place in one day, while at all other stations no noticeable changes were observed. On October 26th the deformation decreased again, on October 27th the measured values ​​were back to the level of October 24th. A temporary accumulation of magma under this station is considered to be the cause.

On October 30th, noon, there were sustained audible explosions that released large amounts of ash. Once again, lightning could be observed in the eruption column. The friction of the ash particles in the eruption column results in static charges that can generate such an eruption thunderstorm .

November 2021

Spread of the lava on certain days in November (1st half, continuously from right to left)
Spread of the lava on certain days in November (2nd half, continuously from right to left)

On November 9th, the height of the cinder cone was given as 1131  msnm for the first time .

On November 10th , a second lava flow reached the coast at Playa Guirres and flowed into the Atlantic. The number and strength of the quakes at depths of more than 20 km had increased in the last few hours. At medium depths, however, the earthquakes remained small compared to the previous weeks. The volcanic tremor also remained at a low level. The day before, sulfur dioxide emissions, contrary to the long-term downward trend, reached a relatively high daily value of 31,000 to 43,000 tons.

On November 20 , the volcano was upgraded from index 2 to 3 (VEI-3) in the volcanic explosion index by reaching 10 million m³ of ejected pyroclastic material. The upgrade is based solely on the accumulated loose material, such as ash, lapilli and bombs, which was not only scattered over the island but was also used to build the volcanic cone. The index does not take into account the amount of lava that has flowed out. It was emphasized that the upgrade does not mean an increased risk, as the general behavior of the volcano has not increased.

On November 26th, a crevice opened 900 m southwest of the first eruption in an area so far only affected by ash a few meters west of an evacuated house . The initial speed of this effusive burst was 600 m / h. It dried up again a day later.

On November 28th, 7 crevices opened at the base of the north flank of the cone, producing abundant lava. The chimneys are in the rectangle [ , ].

On November 30th, several hundred earthquakes and lava fountains from 500 m high occurred again. In addition to the main crater spewing lava, there are ash ejections on the southern flank. The chimneys formed two days earlier are still active.

December 2021

Spread of the lava on certain days in December (continuously from right to left)

The tremors and lava closures continued in December as well. On December 12, 2021, the outbreak had lasted 85 days. The eruption is considered to be the longest known eruption of a volcano on La Palma. So far, the eruption of the Tehuya volcano in 1585 was the longest at 84 days. No reliable data is available on previous outbreaks.

The outbreak ended abruptly on December 13, 2021. The number and intensity of the registered earthquakes also fell to very low values ​​within a few days.

On December 25, 2021, the end of the volcanic eruption was officially declared by representatives of the responsible Pevolca Emergency Committee.

Emissions: gases and particulate matter

Ash cloud over the Cumbre Vieja (October 21, 2021)

In addition to ash and lava, the gases escaping from a volcanic eruption represent a further problem for the population. Due to the geographical location of La Palma, most of the gas quantities are driven out to sea. In certain weather conditions, the gases can also be concentrated in the immediate vicinity, so that staying outdoors without a gas mask is dangerous. An FFP2 mask can filter volcanic particles, but it does not keep gases out. The quantities of carbon dioxide and sulfur dioxide emitted by the Pevolca are estimated on the basis of various measuring stations and published in a daily press conference. On individual days, the Pevolca imposed curfews in the nearby areas because the values ​​exceeded critical levels. The total amounts are estimated and only provide a rough guide on how the outbreak will proceed. For other gases such as the toxic hydrogen sulfide that smells like rotten eggs or the odorless and also highly toxic carbon monoxide , no regular figures are available. The gas emissions are subject to strong fluctuations. High levels indicate a progressive outbreak. An imminent end to the outbreak indicates a decline in sulfur dioxide emissions to a few hundred tons per day. The highest daily value given in October was 53,600 tons on October 24, 2021. In the last week of October, the initially high total amount of sulfur dioxide emitted per day tended to decrease, while the total amount per day for carbon dioxide rose slightly. At the beginning of November high sulfur dioxide values ​​were measured again, albeit with strong fluctuations from day to day.

Emissions Total amount of sulfur dioxide and carbon dioxide at Cumbre Vieja
date mass emitted per day
SO 2 CO 2
2021-10-24 >53 600 t 0803 t
2021-10-25 >40 800 t 1121 t
2021-10-26 >37 350 t 1320 t
2021-10-30 0>7 700 t 1450 t
2021-10-31 0>4,990 tons 1500 t
2021-11-06 > 10,000 t 1200 t
2021-11-09 31,000 ... 43,000 t 1800 ... 2000 t
2021-11-27 30,000 ... 50,000 t ?

Inhaled sulfur dioxide can cause coughing, shortness of breath and inflammation of the respiratory organs or the mucous membranes. Sulfur dioxide and hydrogen sulfide are fatal if inhaled above a certain concentration. The EU limit value for sulfur dioxide in the outside air is 50 µg / m³ as an annual mean, the WHO has been calling for a limit value of 40 µg / m³ as a 24-hour mean since 2021. The Spanish authorities have set the daily limit value at 125 µg / m³ and the hourly limit value at 350 µg / m³ sulfur dioxide. The daily limit value for fine dust with particles smaller than 10 µm (PM10) was set at 50 µg / m³. On October 31, for example, 198 µg / m³ fine dust particles PM10 were measured at the Los Llanos de Aridane station. An FFP2 mask serves as protection for the fine dust particles . The fine PM10 particles in particular can get deep into the lungs.

The volcanic eruption in La Palma led globally to increased sulfur dioxide values ​​in the atmosphere, especially in higher air layers from 3000 m altitude. As of the end of October 2021, no conspicuous values ​​were measured near the ground in Central Europe. The increased values ​​in the higher air layers influence the solar radiation and can cause glowing, orange-red effects in the sky at sunrise or sunset. This phenomenon was observed in Switzerland, for example, at the end of October.

Destroyed area and buildings

Destroyed areas and buildings
date surface building
2021-09-19 0000.8 ha 0000
2021-09-26 0237.5 ha 0513
2021-10-03 0434.7 ha 1046
2021-10-17 0811.8 ha 1956
2021-10-24 0903.7 ha 2154
2021-10-31 0974.6 ha 2574
2021-11-07 0993.6 ha 2593
2021-11-13 1024.4 ha 2618
2021-11-22 1074.6 ha 2676
2021-11-28 1147.7 ha 2748

The areas, buildings and streets destroyed by the lava flows were published daily by the Copernicus Emergency Management Service.

The Copernicus data on destroyed buildings are only raw data and are regularly corrected downwards by the island government by comparing them with the cadastral data . According to a comparison on November 8, 1452 buildings had been destroyed or damaged by then, of which 1177 were residential buildings. According to the land registry office, the lava masses destroyed more than 1,600 buildings, 1,300 of which were residential buildings. The lava has also buried more than 70 kilometers of roads and 370 hectares of banana plantations.

The volcanic ash can also cause considerable damage if it z. B. accumulates on house roofs and causes them to collapse due to the additional weight. The risk increases when rainwater leads to additional pollution. That is why the fire brigade was deployed in the meantime to clear roofs. The military has taken on this task; several hundred soldiers are still on clearing operations after the outbreak has ended.

earthquake

The earthquake swarm that began on September 11th moved increasingly closer to the surface as the magma rose until September 19th. A shallow earthquake on the morning of September 19 with a magnitude of 3.8 mbLg is considered to be the initial quake for the eruption. After the eruption, the earthquakes manifested themselves in two different depths. While the earthquakes up to magnitude 4.0 mbLg occurred at a depth of 9 to 14 km - in the upper magma chamber - the earthquakes were stronger at depths of 34 to 39 km. It should be noted that the IGN in Spain uses the local magnitude scale mbLg. Due to a different calculation method, this shows slightly higher values ​​than the EMSC's ML Richter scale .

Earthquakes from magnitude 4.5 ML (EMSC) and higher
Time ( UTC ) Magnitude Max intensity Coordinates (IGN) Depth (IGN)
mbLg (IGN) ML (EMSC) Mercalli (IGN)
Oct 15, 2021, 7:02:19 am 4.5 4.5 III-IV 28.5760 ° N, 17.8228 ° W 36 km
Oct 16, 2021, 6:07:02 am 4.5 4.5 IV-V 28.5843 ° N, 17.8175 ° W 34 km
Oct. 19, 2021, 9:48 p.m. 4.8 4.5 IV-V 28.5855 ° N, 17.8192 ° W 39 km
Oct 23, 2021, 3:34:49 pm 4.9 4.7 IV 28.5697 ° N, 17.8064 ° W 38 km
Oct. 26, 2021, 4:25:37 pm 4.8 4.7 IV 28.5697 ° N, 17.8064 ° W 34 km
Oct. 26, 2021, 11:53:16 pm 4.8 4.7 IV 28.5770 ° N, 17.8224 ° W 35 km
Oct 27, 2021, 6:19:56 am 4.6 4.6 IV-V 28.5854 ° N, 17.8099 ° W 38 km
Nov 3, 2021, 7:27:34 am 4.8 and 5.0 4.9 IV-V 28.5704 ° N, 17.8338 ° W 35 km
Nov 10, 2021, 11:10:07 a.m. 4.8 4.7 IV 28.5729 ° N, 17.8234 ° W 34.5 km
Nov 17, 2021, 12:33:35 p.m. 4.7 and 4.8 4.5 IV 28.5854 ° N, 17.8065 ° W 36 km
Nov 19, 2021 01:08:47 AM 5.1 4.9 IV 28.5730 ° N, 17.8234 ° W 36 km

Effects on air traffic

Volcanic ash on the runway (runway) leads to increased wear and tear up to failure of the engines during take-off as well as problems during landing, especially on the 2200 m short runway from La Palma airport . Reverse thrust on landing leads to engine damage. Flying through clouds of volcanic ash, which cannot be seen on the radar, increases the wear and tear on the engines and, in extreme cases, can lead to engine failure. In addition to safety aspects, cost aspects play a role in whether airlines still fly to an airport.

The Spanish Ministry of Tourism announced on September 20, 2021 that there were no restrictions on air traffic for the time being and also not for holidaymakers traveling to La Palma in the next few days.

On September 24th, operations at La Palma Airport ceased in the afternoon because the runway and taxiways were covered with ash. Although the airport was able to reopen on September 26th, some airlines decided not to resume operations for the time being. Some flights to Tenerife were relocated and the passengers were brought to La Palma by ferry .

From October 7th to 9th, the airport was closed again due to ash deposits. At the same time, some of the ash reached the north of Tenerife. Several flights were diverted from Tenerife north to the south airport , but there was no take-off and landing ban.

The airport was again closed for several days from November 20, 2021.

Repairs and planning

Even before the foreseeable end of the outbreak, drafts, planning and the first measures for the repair of the infrastructure were started. The two most important points here are the transport links between the towns of Las Manchas, Jedey and Puerto Naos in the south and their administrative centers, as well as the resumption of the supply of drinking and irrigation water in the area south of the lava flows. For this purpose, a supply with tankers was initially taken up; at the same time, two plants for seawater desalination were built.

A continuation of the (provisionally built) ferry connection and above all a new road from Tazacorte to Puerto Naos below (to the west) of the Montañas La Laguna and Todoque, whose route is also to be used for sewage disposal , energy supply and telecommunications , is being discussed Vulkan was interrupted in other places as well. A 2.2-kilometer connection between the LP211 and the LP213 (between Puerto Naos and Las Manchas) has been under construction since November 9, 2021.

Web links

Commons : Volcanic eruption La Palma 2021  - Collection of pictures, videos and audio files

annotation

  1. This ancient volcano is to the west of the LP-212 road and 1 km further north than its confluence with the LP-2 road

Individual evidence

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Coordinates: 28 ° 37 ′  N , 17 ° 52 ′  W