Philosophical Transactions of the Royal Society, London, Ser A, 200: 353-553. https://doi.org/10.1098/rsta.1903.0010, Heath E, Macdonald R, Belkin H, Hawkesworth C, Sigurdsson H, 1998. The lack of significant seismic activity supports our interpretation of the present events as a relatively quiet eruption of a gas-poor lava. Confirmed Eruption Card 1321 (01 December 1971) Lava dome growth in crater lake continues. After this explosion, the seismicity consisted primarily of 30-50 small explosion events per hour, which could be correlated with the ejection of steam puffs that sometimes contained a little ash. A period of high tremor began at 1649 on 18 April. Conditions on the Caribbean island of St. Vincent have worsened as La Soufrire volcano continues to push ash and debris into the atmosphere. The number of individual events declined irregularly through the morning of 16 April. The following 270 samples associated with this volcano can be found in the Smithsonian's NMNH Department of Mineral Sciences collections, and may be availble for research (contact the Rock and Ore Collections Manager). Available webcams . A few small daily earthquakes were recorded. Credit: NOAA, Initial ash plume seen by GEOS-16 from the April 9, 2021 eruption at La Soufriere on St. Vincent. The Alert Level remained at Orange (the second highest level on a four-color scale). There is some indication that this eruption is similar to what occurred during the 1902 activity at La Soufriere. During 20-21 April seismicity was characterized by a few rockfalls and volcano-tectonic (VT) earthquakes, and an increasing number of small long-period (LP) and hybrid earthquakes. Powered by www.VolcanoDiscovery.com References: Cole P D, Robertson R E A, Fedele L, Scarpati C, 2019. Observations made during the afternoon indicated that pyroclastic flows had reached the ocean in every valley extending from Larikai to Wallibou, a length of about 5 km. Several vents were identified or inferred by emissions points of gas-and-steam and ash plumes. Trees brought down by lahars were swept to the sea; floating logs created hazardous conditions for small boats along the coastline. La Soufrire is one of the most active volcanoes in the Lesser Antilles and has a long history of eruptions with the historical records showing eruptions in 1718, 1812, 1814, 1902-1903, 1971-72 and 1979. Seismic data are transmitted from field sites to the Belmont Observatory (9 km SSW), which is operated by the SMU. . Pyroclastic flows descended several valleys on the S and W flanks, reaching the coast at Morne Ronde (4.3 km W), Larikai (3.5 km WNW), and Trois Loupes Bay (3.5 km NW). Another large explosion was detected at 2300, according to UWI-SRC. Confirmed Eruption We and our partners use data for Personalised ads and content, ad and content measurement, audience insights and product development. Unfortunately, this survey had to be abandoned due to unfavorable conditions on the lake. The Grantley Adams International Airport (GAIA) in Barbados also closed. - 1718 Mar 29 The crater was observed and photographed during 11-12 June; observers saw no signs of lava domes. MIROVA (Middle InfraRed Observation of Volcanic Activity) analysis of MODIS satellite data detected a single thermal anomaly during mid-March 2021, followed by a brief break in activity (figure 34). These earthquakes were more intense and averaged 50/hour; the 23-25 March swarm averaged 1.5/hour. Shepherd, J. and drifted mainly N over the sea. A small lahar signal was recorded at 0740 on 7 May. Almorales, Seismic Research Unit, University of the West Indies. The Seismic Research Unit (SRU) collaborates with a small local unit called the Soufrire Monitoring Unit (which operates from the Ministry of Agriculture in Kingstown). Worldwide animated weather map, with easy to use layers and precise spot forecast. While the N of the island continues to rise, the S end shows little or no increase in height. Rate of lava extrusion in the summit crater of Soufrire St. Vincent, 25 May-25 October 1979, calculated by John Tomblin. This depth is 48.5 ft less than the maximum obtained during the previous sounding survey on 27 January, and confirms that the lava dome is still expanding horizontally across the former lake floor. Card 1358 (23 February 1972) W. Aspinall and H.J. The fact that many of these populated islands are dominated by volcanoes means they can be especially perilous when these volcanoes rumble back to life. Both the 1979 and 1902 explosive eruption cycles at La Soufrire were quite significant, ranking. Table 4 contains mean values for all available wet chemical analyses of Soufrire rocks, summarized from UWI Seismic Research Special Publication No. A hot avalanche from one of the earlier explosions traveled 2.5 km SE from the summit, down the Rabacca Valley, and the 17 April explosion produced numerous hot avalanches that moved down several valleys on the flanks of the cone. An "explosive" volcanic eruption has blanketed the Caribbean island of St Vincent in ash and smoke and forced thousands of people out of . It is, however, similar to the second half of the two large historic eruptions of Mt. A VEI 4 is defined as between 10 8 and 10 9 m 3 of ash and tephra. Successive explosions and ash pulses fed the plume for hours, rising to 16 km altitude. On 22 April at 1108 explosions generated an ash plume that rose to 8 km altitude and drifted mainly N over the ocean (figure 31). A change in character of an eruption like this is not uncommon. However, monitoring of the volcano by the Seismic Research Unit, University of the West Indies, continues. "We quickly determined that the reported 'activity' was due to an unusual southerly wind combined with the phenomena of Sahara dust which is common around this time of the year in St. Vincent and which results in very hazy conditions. Get unlimited access for as low as $1.99/month, The volcanoes of the West Indies have produced some of the. Max VEI: 4, 1979 Apr 13 - 1979 Oct 26 5 days No comprehensive survey of the island has been carried out during this period but from visual observation the general shape is still as previously described. The water level is rising faster again with a 38-cm increase in the last 48 hours, but the temperature at the lake edge remains steady at 82C. Around 2100 the seismic network recorded multiple lahars, though their location could not be determined. Water temperature at the observation point on the S edge of the lake has dropped from 74C to a nearly constant value of 69C. to be taken to nearby islands for the time being. William C. Buell IV (Washington, D.C.) reports that Soufrire is a "very dangerous" volcano and that the heat level has recently risen from 20 to 84C, a very significant change. The fact that many of these populated islands are dominated by volcanoes means they can be especially perilous when these volcanoes rumble back to life. The only noteworthy features of the above figures are that 1) aeolian differentiation of the 7-8 May 1902 ash appears to have been negligible at 100 miles but considerable at the 275-mile range; and 2) pyroclasts erupted at the end of the 1902-03 eruption were about 2% lower in silica than at the beginning of this eruption. St. Vincent evacuated ahead of 'imminent' eruption of La Soufrire volcano - CNN Video JUST WATCHED Caribbean island evacuated ahead of 'imminent' volcano eruption Replay MUST WATCH World. In: Latter J H (ed), Volcanic Hazards - Assessment and Monitoring, Berlin: Springer-Verlag, p 292-311. MODIS looks at every square km of the Earth every 48 hours, once during the day and once during the night, and the presence of two MODIS sensors in space allows at least four hot-spot observations every two days. Expand each entry for additional details. Almorales, Seismic Research Unit, University of the West Indies. Activity during December 2020. Max VEI: 3, 1480 150 years Sources: University of the West Indies Seismic Research Centre (UWI-SRC), National Emergency Management Organisation (NEMO), Government of Saint Vincent and the Grenadines, Intermittent explosions, ash plumes, seismicity, and a growing lava dome during March-April 2021. "In Card 1336 it was stated by Sigurdsson and Shepherd that 'the new hot lava is significantly more basaltic, i.e., lower in silica (55.3%) than the products of the most violent phases of the 1902 eruption, which were more andesitic in composition, with silica content of 56-58%.' Subsequent explosive events were reported at 1115, 1700, and 2050 on the 13th, 0300 and 1200 on 14 April, 1705 on 17 April, 0635 on 22 April, and 2355 on 25 April. Seismicity began to increase in early November through 23 December 2020, which included 126 earthquakes described as volcano-tectonic events and rockfall signals that were captured on one reliable seismic station (SVB) located 9 km from the volcano. Fiske R S, Shepherd J B, 1982. It. The frequency of crater tremors continued on a greatly diminished scale and only six tremors were recorded during the past three weeks. The crater lake waters have found an outlet through the flank of the cone and are seeping out. During the night of 10-11 April tremor lasting up to 20 minutes continued at intervals of 1.5-3 hours, associated with periods of explosions and ash emissions. Island growth continues; historical comparisons, Card 1350 (03 February 1972) Analyses of volcanic products. UWI-SRC noted that over the previous few days continuing lahars had mobilized boulders 5 m in diameter and were steamy in areas where they contacted hot deposits. As of 2004, the monitoring network had consisted of five seismic stations, eight GPS stations, and several dry tilt sites. | March Five seismograph stations continue to operate on a 24-hour basis but three of these stations are within 2 km of the crater. Courtesy of the Seismic Research Unit. A new effusive eruption had built a lava dome in the summit crater of Soufrire St. Vincent when observed on 29 December by personnel from the National Emergency Management Organisation (NEMO), St. Vincent and the Grenadines, and the Alert Level was raised to Orange (the second highest level on a four-color scale). When one is found the date, time, location, and intensity are recorded. During the period 13-26 May 1972, the situation at the crater continued along the lines stated in the last report. This activity marks the beginning of the effusive eruption and the formation of the new lava dome. Le Friant A, Boudon G, Arnulf A, Robertson R E A, 2009. A single rockfall event was detected at 0139, possibly due to the growing lava dome, though there was no visual confirmation. Seismicity remained low through 11 May with only a few long-period earthquakes recorded by the seismic network. The water temperature varied between 40-41C. The occurrence of crater tremors was practically zero, with one tremor recorded during the last two weeks. There is one tiltmeter site being set up on the eastern flank of the volcano. University of the West Indies Seismic Research Centre (UWI-SRC) and National Emergency Management Organisation (NEMO) reported that seismicity at Soufrire St. Vincent (often simply referred to as La Soufriere) remained low during 17-24 May, with a few long-period and volcano-tectonic earthquakes occasionally recorded. Extensive damage to vegetation was noted along the W coast, extending from Larikai Bay to Turner Bay. A spike in seismicity was recorded during June-July 2019 (figure 5), though no cause was reported. Water level is dropping at a slower rate than before 7 March, when the daily drop was 9 inches on the average. Anomalous winds spread sulfurous odors, causing unwarranted fears. Courtesy of John Tomblin, UWI. The new dome had spread over the remnants of the old crater lake by about 20 May, but a new lake had begun to form at the beginning of June because of the onset of the rainy season. Soufrire in St. Vincent. Starting at 1653 the network also detected volcano-tectonic (VT) earthquakes, some of which had been felt in communities, including Fancy, Owia, and Sandy Bay. Interpretation. It is sponsored by the, The IAVCEI Commission on Volcanic Hazards and Risk has a, Middle InfraRed Observation of Volcanic Activity (. Successive explosions and ash pulses fed the plume for hours and it rose to 16 km (52,000 ft) a.s.l. Five long-period earthquakes and two brief swarms of VT events occurred in between the tremor episodes; ash venting occurred with the last episode. Simon Carn noted that this makes the La Soufriere eruption the largest tropical SO2 emission since the 2011 Nabro eruption, and the largest in the Caribbean since satellite measurements began in 1979. Most of the evidence tends to suggest that there is a slight new lava being extruded at a slower rate into the crater, but whether this decrease in activity is temporary or not is too early to comment on at this stage. La Soufrire or Soufrire Saint Vincent ( French pronunciation: [sufj s vs]) is an active stratovolcano on the Caribbean island of Saint Vincent in Saint Vincent and the Grenadines. The rate of LP and hybrid events dropped significantly at 2000. . The following report on the subject comes from SRU's Richard Robertson. University of the West Indies Seismic Research Centre (UWI-SRC) reported that seismicity at Soufrire St. Vincent (often simply referred to as La Soufriere) remained low during 28 April-4 May, with a few long-period, hybrid, and volcano-tectonic earthquakes recorded daily. In addition, a number of pinnacles and small islands are sticking out of the water NW of this larger island. Most of the explosions occurred close to diurnal earth tide maxima, and the 17 April explosion also fell on the fortnightly earth tide minimum (calculations from F.J. Mauk). Lahars in the Red and Orange zones were recorded by the seismic network at 0900 and 1000 on 27 April, during and after rainfall. No local earthquakes have been recorded by tremors associated with rockfalls on the island continue to occur. respectively. Lightning was visible in the rising plume. Unpublished PhD thesis, Univ West Indies, 282 p. Shepherd J B, 1989. An explosion at 0615 on 16 April generated an ash plume that rose about 8 km (26,200 ft) a.s.l. Steam from the dome was visible from Belmont Observatory through 4 January. At about 2000 on the 16th, the seismicity changed entirely to rock fracture events, which continued until the explosion of 17 April. A series of Vulcanian explosions that began at 0630 on 13 April, and lasted about 30 minutes, was accompanied by large seismic tremors followed by more than three hours of smaller continuous tremors (figure 26). The number and frequency of the VTs increased until about 0830 and then stabilized. However, the summit and Rabacca station are back in operation, and repairs are continuing on the Wallibou station. A swarm of volcano-tectonic (VT) earthquakes began at 0638 on 5 April. Active gas-and-steam emissions originated dominantly at contact areas between the pre-existing 1979 dome and the 2020/21 dome, as well as at the top of the new dome. On 23 April the sulfur dioxide flux was 992 tons per day, recorded again from the W coast. Measurements have been made on near-vertical air photos of the crater taken on 11 February and kindly placed at our disposal by Mrs. M. Barnard. As of 19 March the dome was 105 m tall, 921 m long, 243 m wide, and had an estimated volume of 13.13 million cubic meters. Sulfur dioxide emissions were 232 and 391 tons per day on 17 and 18 April, respectively. Many of the evacuees were moved onto cruise ships to be taken to nearby islands for the time being. This conclusion is supported by the constancy of the rate of lava emission (~0.5 x 106 m3/day) from the beginning of November 1971 to the present, and by the small total volume so far erupted (80 x 106 m3) in comparison with the total fresh lava produced in 1902-03 (2,600 x 106 m3). Confirmed Eruption, 2135 BCE 50 years All Rights Reserved. The true amount of horizontal expansion of the dome is therefore 44 m. The W half of the dome is now 10-20 feet higher than the E half, and the two halves are still separated by a N-S valley. On 12 April at 0415 a large explosion produced an ash plume that rose to 12.8 km altitude. Operator: madinina.webcam Webcam Tartane, Martinique - 63.5 miles from Soufriere: La Caravelle Operator: madinina.webcam Synonyms of features appear indented below the primary name. The SO2 plume initially fanned out to the NE, E, and SE across the Atlantic Ocean. Ash rises into the air as La Soufriere volcano erupts on the eastern Caribbean island of St. Vincent, seen from Chateaubelair, Friday, April 9, 2021. Ash venting continued through the night and into 10 April. Two thermal hotspots were detected using the MODVOLC thermal algorithm on 24 April. The Alert Level remained at Orange (the second highest level on a four-color scale). Lahar deposits were reported in the Sandy Bay area. The northern peak was at 216 feet and the eastern summit at 201 feet. The installation of instruments, initial adjustments, and readings to establish reference levels is scheduled for the next two weeks. Max VEI: 4, 1814 Jan 9 - 1814 Jan 9 The dome's growth rate was difficult to estimate, but was probably <0.5 x 106 m3/day in late May. Gas-and-steam plumes were also visible from Belmont Observatory. The water level is decreasing at an average rate of 1.5 inches/day, as evaporation over the crater lake continues. A second explosion at 1445 produced a vigorous ash plume that initially rose to 4 km altitude with lightning visible in the plume (figure 22). ", Card 1330 (15 December 1971) Eruption continues during 8-13 December with dome growth. The noon explosion on 14 April produced a 100 km-diameter cloud, and two explosions on 13 April also produced sizeable clouds, 60-km-diameter at 1700 and 40 km at 2050. No lava dome was visible, but a possible spine-like protrusion was seen through the clouds. During 17 and 18 April the average SO2 flux was 232 and 391 tons/day, respectively. UWI-SRC stated that a large explosion was recorded around 2300. Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Fumarolic activity from the top of the dome was moderately strong during the early stages of its growth, but had stopped by 20 May. Card 1359 (29 February 1972) Comparison of current eruption with historical activity. A small lava dome with fresh magma emerged at the base of the existing dome in the crater of the La Soufriere volcano in St. Vincent on Wednesday. Table 4. Saint Lucia Webcams in Caribbean Islands - Live Beaches Webcams in St Lucia Webcams - Caribbean Islands Anguilla (9) Antigua & Barbuda (7) Aruba (13) Bahamas (12) Barbados (13) Belize (9) Bermuda (9) British Virgin Islands (10) Cancun (18) Cayman Islands (9) Cozumel (10) Cuba (3) Curacao (8) Dominica (3) Dominican Republic (14) Grenada (4) The first explosive activity was observed at dawn (about 0500) on 13 April. Scientists visited on 16 January and recorded temperatures of 590C at the dome surface (figure 12). The eruption of 1979 was characterized by ashfall, pyroclastic flows, and lahars, in addition to a series of Vulcanian explosions during 13-26 April 1979 that destroyed the lava dome in the summit crater, which had formed during a 1971 effusive eruption (SEAN 04:04). The Alert Level remained at Orange (the second highest level on a four-color scale). Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. Analysis of satellite imagery by UWI-SRC indicated that the explosions that began on 9 April destroyed the pre-existing 1979 and 2020-21 lava domes and created a crater 800 m in diameter. The NE rim of the 1.6-km-wide summit crater is cut by a crater (500 m wide and 60 m deep) that formed in 1812. The temperature was 40C on 15 May, 41C on 18 May, 40C on 22 May, and 41C on 25 May. These statements are incorrect. 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