The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported a continuing eruption at Kanlaon during 3-10 December and an escalation in activity on 9 December. The seismic network recorded 6-22 daily volcanic earthquakes, and sulfur dioxide emissions ranged from 1,669 to 6,432 tonnes per day. Gas-and-steam emissions that were mostly continuous and often voluminous rose 200-500 m above the summit and drifted mainly W, WSW, and SW. There were 1-6 ash emission events during 3-5 and 7-8 December, with each lasting 3-40 minutes.
An explosive eruption occurred at 1503 on 9 December and lasted three minutes and 55 seconds. A voluminous ash plume rapidly rose 4 km above the crater rim and drifted WSW. Pyroclastic flows traveled 2-3.4 km down the SE flanks. The Alert Level was raised to 3 (on a scale of 0-5) and local governments were advised to evacuate residents within a 6 km radius. According to news articles ashfall was reported in 30 cities and towns across the municipalities of Negros Occidental, Guimaras, Iloilo, and Antique. A sulfur odor was noted in several barangays and in Bago City (20 km NW). Several schools in those areas suspended classes. The Disaster Response Operations Monitoring and Information Center (DROMIC) report issued on 10 December stated that 12,172 people (3,616 families) had evacuated mainly from Bago City, La Carlota City (14 km W), and La Castellana (16 km SW), with fewer people from Moises Padilla (17 km SSW), Magalion (14 km SSW), Murcia, Pontevedra, and Canlaon City (10 km ESE). There were 12,010 evacuees spread across 24 evacuation centers and 162 people were staying with friends or relatives.
Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Disaster Response Operations Monitoring and Information Center (DROMIC), Philippine News Agency (PNA)
Phreatic explosions on 9 December 2017 with ashfall and high seismicity
A series of three explosions at Kanlaon on 18 June 2016 sent ash plumes as high as 3 km above the crater and caused minor ashfall in neighborhoods W, SW, and NW of the volcano (BGVN 42:01). This was followed by steam plumes through 25 July 2016. The active Lugud crater (figure 4) has been the source of 21 reported eruptions since 1969; the latest eruption took place in December 2017. Information summarized here for activity from September 2016 through December 2017 was provided by the Philippine Institute of Volcanology and Seismology (PHIVOLCS).
PHIVOLCS reported on 5 May 2017 that since the last phreatic eruption in June 2016 there had been a general decline in activity: seismicity was at baseline levels, no significant deformation had been detected since August 2016, sulfur dioxide emissions were low, and no steaming had been observed since 29 September 2016. The Alert Level was lowered to 0 (on a scale of 0-5), though the public was warned to not enter the 4-km-radius Permanent Danger Zone (PDZ).
Between 24 June and 18 August 2017 the seismic network detected 244 volcanic earthquakes. The PHIVOLCS report noted that the increased seismic activity could be followed by phreatic explosions at the summit crater, despite the absence of visible degassing or steaming from the active vent. The Alert Level was raised to 1. The number of daily volcanic earthquakes increased after 18 August. In their 15 November report, PHIVOLCS indicated that during the previous 24 hours there had been 279 deep volcanic earthquakes recorded (compared to five the day before). This prompted them to raise the Alert Level to 2 (moderate level of unrest), where it remained for the rest of the year. The next day, the number recorded was 217. After that the daily number of volcanic events dropped considerably, especially after 21 November. Based on PHIVOLCS reports, the number of daily volcanic earthquakes during the first eight days of December 2017 varied from one to seven.
On 9 December an approximately 10-minute-long, low-energy phreatic explosion began at 0947 that was heard as far away as La Castellana, Negros Occidental (15 km SW). A plume of voluminous steam and dark ash rose 3-4 km above the summit vent (figure 5), and minor amounts of ash fell in Sitio Guintubdan (23 km W), and barangays W of the volcano (Ara-al, Sag-ang, and Ilihan). The eruption was preceded by the resumption of degassing at the summit crater at 0634, detectable as continuous low-energy tremor during periods when the summit was not visible; degassing was last observed September 2016.
Only three volcanic earthquakes were detected on 10 December, but then the number increased to 155 the next day. The number of daily events earthquakes increased again to 578 on 13 December, rose to 1,007 the next day, and peaked at 1,217 on the 15 December. The earthquake count dropped to 149 on 16 December before returning to six or fewer through 19 December. White steam plumes rose 800 and 300 m above the crater on 13 and 14 December, respectively. White plumes were diffuse on 15 December; weather clouds prevented views of the summit area during 16-18 December. Sulfur dioxide emissions were 603-687 tons per day during 13-14 December.
PHIVOLCS reported that during 19-20 December there were 412 volcanic earthquakes. A low-energy, explosion-type earthquake was detected at 0233 on 21 December associated with gas emissions from the summit area. Later in the day steam plumes rose 400 m and drifted NE. The number of daily volcanic earthquakes increased to 957 the next day and then decreased to less than 20 per day during 22-23 December. The daily earthquake count increased to 382 and 776 events on 24 and 25 December, respectively, decreased to 82 on 26 December, and the dropped to three or fewer over the last days of the year. Weather clouds often prevented observations , but white plumes rose 300 m and drifted NE, NW, and SW on 21 December, and 700 m on 26 December. A steam plume on 30 December was seen rising 500 m above the crater rim and drifting SW. On 30 December 2017, sulfur dioxide levels were measured at an average of 1,946 tonnes/day.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, University of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/); Billy Lopue, flickr (URL: https://www.flickr.com/photos/21905294@N03/).
2024: April
| May
| June
| July
| August
| September
| October
| November
| December
2023: April
| May
| July
| September
| November
2022: January
| February
| June
2021: February
2020: March
| June
2019: October
2018: April
2017: May
| August
| December
2016: March
| June
| July
2015: November
| December
2010: May
2009: August
2008: February
| April
2006: June
| July
| November
2005: January
| March
| April
| May
2004: March
2003: June
| July
2002: January
| November
2001: March
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported a continuing eruption at Kanlaon during 3-10 December and an escalation in activity on 9 December. The seismic network recorded 6-22 daily volcanic earthquakes, and sulfur dioxide emissions ranged from 1,669 to 6,432 tonnes per day. Gas-and-steam emissions that were mostly continuous and often voluminous rose 200-500 m above the summit and drifted mainly W, WSW, and SW. There were 1-6 ash emission events during 3-5 and 7-8 December, with each lasting 3-40 minutes.
An explosive eruption occurred at 1503 on 9 December and lasted three minutes and 55 seconds. A voluminous ash plume rapidly rose 4 km above the crater rim and drifted WSW. Pyroclastic flows traveled 2-3.4 km down the SE flanks. The Alert Level was raised to 3 (on a scale of 0-5) and local governments were advised to evacuate residents within a 6 km radius. According to news articles ashfall was reported in 30 cities and towns across the municipalities of Negros Occidental, Guimaras, Iloilo, and Antique. A sulfur odor was noted in several barangays and in Bago City (20 km NW). Several schools in those areas suspended classes. The Disaster Response Operations Monitoring and Information Center (DROMIC) report issued on 10 December stated that 12,172 people (3,616 families) had evacuated mainly from Bago City, La Carlota City (14 km W), and La Castellana (16 km SW), with fewer people from Moises Padilla (17 km SSW), Magalion (14 km SSW), Murcia, Pontevedra, and Canlaon City (10 km ESE). There were 12,010 evacuees spread across 24 evacuation centers and 162 people were staying with friends or relatives.
Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Disaster Response Operations Monitoring and Information Center (DROMIC); Philippine News Agency (PNA)
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported a continuing eruption at Kanlaon during 26 November-3 December. The seismic network recorded 5-26 daily volcanic earthquakes, and sulfur dioxide emissions ranged from 2,524 to 9,377 tonnes per day. Moderate gas-and-steam emissions rose 100-750 m above the summit and drifted mainly SW, W, and NE. There were 1-5 daily ash emission events during 26-29 November and on 1 December, with each lasting 5-35 minutes. According to the Tokyo VAAC the ash emissions on those same days rose 2.7-3.4 km (9,000-11,000 ft) a.s.l. and drifted SW, NNW, and NE. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Tokyo Volcanic Ash Advisory Center (VAAC)
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported a continuing eruption at Kanlaon during 19-25 November. The seismic network recorded 3-23 daily volcanic earthquakes, and sulfur dioxide emissions ranged from 5,125 to 8,040 tonnes per day; weather clouds obscured views on 19 November. Moderate gas-and-steam emissions high as 300 m above the summit and drifted SW and WSW. There was one ash emission event on 21 November and two on 23 November, with each lasting 4-8 minutes long. According to the Tokyo VAAC the ash emissions rose as high as 2.7 km (9,000 ft) a.s.l. and drifted W and SW. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Tokyo Volcanic Ash Advisory Center (VAAC)
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 13-19 November. The seismic network recorded 3-13 daily volcanic earthquakes, and sulfur dioxide emissions ranged from 4,246 to 7,818 tonnes per day. Daily moderate-to-voluminous gas emissions with intermittent ash rose as high as 1 km above the summit and drifted several directions. During 15-17 and 19 November there were 4-6 daily ash emission events, each lasting as short as 2 minutes and as long as one hour and 43 minutes. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 6-12 November. Daily moderate-to-voluminous gas emissions with intermittent ash rose as high as 1 km above the summit and drifted several directions. Between 0546 and 0702 on 9 November an “ashing” event generated light gray plumes that rose 750 m above the summit and drifted SW. Trace ashfall was reported in Barangay Yubo (6.5 km WSW), La Carlota City (14 km W), Barangay Sag-ang (10 km SW), and La Castellana (16 km SW); the smell of sulfur was also reported in Yubo and Sag-ang. Microscopic examination of ash samples from events on 19 October, 2 November, and 5 November revealed that the ash is primarily old material and not from new magma. The seismic network recorded daily volcanic earthquakes, and sulfur dioxide emissions ranged from 2,125 to 7,378 tonnes per day. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 30 October-5 November. The seismic network recorded daily volcanic earthquakes, but between 0000 and 1030 on 31 October a total of 64 volcano-tectonic (VT) earthquakes were recorded with maximum magnitude of M 2.9 concentrated 2-8 km beneath the W flanks of the volcano. Sulfur dioxide emissions ranged from 2,066 to 7,087 tonnes per day. On most days voluminous emissions with intermittent ash were observed rising as high as 900 m above the summit and drifting several directions. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 22-29 October. The seismic network recorded 1-6 daily volcanic earthquakes. The summit was obscured by weather conditions daily. Sulfur dioxide emissions continued to be high, averaging 4,853-5,188 tonnes/day (t/d) during 26-27 October. A special notice issued on 28 October noted that summit emissions of sulfur dioxide measured with a Flyspec instrument averaged 10,074 tonnes/day (t/d), the fifth highest ever recorded at the volcano. Sulfur odors were reported in Masulog and Canlaon City (8 km ESE) proper and, to a lesser degree, in the neighborhoods of Panubigan and Binalbagan, Canlaon City. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 16-22 October, characterized by elevated seismicity and sulfur dioxide emissions. Visual monitors recorded continuous degassing, with brief episodes when gray ash was entrained in the plume. Three “ashing” events, at 0641, 0701, and 0801 on 19 October, lasted two to six minutes long, based on visual observations; no detectable seismic or infrasound signals were recorded. The events generated light-gray plumes that rose 500 m above the crater and drifted SW. Traces of ash deposits were reported in the barangays of Yubo and Ara-al, La Carlota City (14 km W), and Sag-ang, La Castellana (16 km SW). A sulfur dioxide odor was also reported in Yubo.
The seismic network recorded 6-19 daily volcanic earthquakes. Daily gas-and-steam emissions that were sometimes voluminous rose 200-900 m above the summit and drifted W, SW, S, and SE. Sulfur dioxide emissions were recorded during 16-20 October and continued to be high, averaging 2,679-6,477 tonnes/day. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 8-15 October, characterized by elevated seismicity and sulfur dioxide emissions. The seismic network recorded 1-19 daily volcanic earthquakes. Daily gas-and-steam emissions that were often voluminous rose 400-750 m above the summit and drifted NE, SE, SW, and W. Sulfur dioxide emissions were recorded daily and continued to be high, averaging 1,919-6,011 tonnes/day. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 2-8 October, characterized by increased seismicity and sulfur dioxide emissions. The seismic network recorded 5-15 daily volcanic earthquakes. Daily gas-and-steam emissions that were often voluminous rose 100-650 m above the summit and drifted NE, W, SW, and S. Sulfur dioxide emissions were recorded daily and continued to be high, averaging 2,606-9,042 tonnes/day. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 25 September-1 October, characterized by increased seismicity and sulfur dioxide emissions. The seismic network recorded 7-16 daily volcanic earthquakes. Daily gas-and-steam emissions that were voluminous mid-week rose 100-850 m above the summit and drifted in multiple directions. Sulfur dioxide emissions were recorded daily and continued to be high, averaging 4,992-8,973 tonnes/day. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported continuing unrest at Kanlaon during 17-24 September, characterized by increased seismicity and sulfur dioxide emissions. The seismic network recorded five volcanic earthquakes during 17-18 September and 15-55 daily volcanic earthquakes during the rest of the week. Weather clouds obscured views of the summit during 17-19 September. Voluminous gas-and-steam emissions rose 300-800 m above the summit and drifted in multiple directions during 20-23 September. Sulfur dioxide emissions were recorded daily and continued to be high, averaging 5,362-10,449 tonnes/day. According to a Disaster Response Operations Monitoring and Information Center (DROMIC) report there were a total of 3,905 people in evacuation centers as of 22 September. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Disaster Response Operations Monitoring and Information Center (DROMIC)
PHIVOLCS reported continuing unrest at Kanlaon during 11-17 September, characterized by increased seismicity and sulfur dioxide emissions. Sulfur dioxide emissions reached a record high on 11 September, averaging 11,556 tonnes/day (t/d), before decreasing slightly to 10,880 t/d on 12 September; emissions were not reported the rest of the week. The number of volcanic earthquakes detected by the seismic network was 337 during 10-11 September and 79 recorded during 11-12 September. The daily number fluctuated from 2 to 32 on the other days. Weather clouds obscured views of the summit during the second half of the week. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano. According to a Disaster Response Operations Monitoring and Information Center (DROMIC) report there were a total of 2,298 people in evacuation centers as of 16 September.
Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Disaster Response Operations Monitoring and Information Center (DROMIC)
PHIVOLCS issued special notices for Kanlaon noting periods of increased seismicity and continuing high levels sulfur dioxide gas emissions. The seismic network detected 288 volcano-tectonic earthquakes from 2030 on 9 September to 1100 on 10 September that were located at depths of 0-9 km beneath the NE flank. The strongest events were classified at Intensity II and felt in some barangays (neighborhoods) of Canlaon City, 8 km SSE, Negros Oriental. Rumbling sounds were reported by residents of Bago City and a strong sulfur odor was reported in a few barangays in the cities of Bago (30 km NW), La Carlota (14 km W), and Canlaon. According to a news article the intense seismicity prompted the local Canlaon City government to order a mandatory evacuation of the Permanent Danger Zone, defined as a 4 km radius from the summit, as a precautionary measure. About 91 families (301 people) moved to evacuation centers.
Summit emissions of sulfur dioxide measured with a Flyspec instrument averaged 9,985 tonnes/day (t/d) on 10 September, the highest ever recorded at the volcano. Sulfur odors were reported in the barangays of Ilijan (Bago), Ara-al and San Miguel (La Carlota), and in Masulog, Linothangan, and Pula (Canlaon). A steam-and-gas plume rose 1 km above the summit and drifted SE. Another record high for sulfur dioxide emissions was recorded on 11 September with an average of 11,556 t/d. Residents reported sulfur odors in areas downwind including San Miguel, Masulog, Pula, Codcod (San Carlos City), and Inolingan (Moises Padilla). A news report noted that both public and private schools suspended classes in four barangays.
Elevated sulfur dioxide gas fluxes had been recorded in 2024 with an average of 1,273 t/d prior to the 3 June eruption; afterward the eruption emissions were averaging 3,468 t/d. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone and warned pilots not to fly close to the volcano.
Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Philippine News Agency (PNA); Philippine News Agency (PNA)
PHIVOLCS reported that unrest at Kanlaon continued during 27 August-3 September. There were 3-12 daily volcanic earthquakes recorded by the seismic network. Steam-and-gas emissions rose 100-500 m above the summit and drifted ENE, E, SW, and W on most days. Sulfur dioxide emissions declined during the week, averaging 4,585 (27 August), 4,418 (28 August), 3,189 (29 August), and 2,669 (31 August) tonnes per day. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued special notices for Kanlaon noting continuing high levels sulfur dioxide gas emissions. Summit emissions measured with a Flyspec instrument averaged 6,720 tonnes/day (t/d), 6,367 t/d, and 7,172 t/d on 21, 24, and 25 August, respectively. Sulfur odors were reported in several barangays (neighborhoods) in La Carlota City (14 km W) and La Castellana (16 km SW), Negros Occidental, on 21 August and in Murcia (17 km NNW), Negros Occidental, on 24 August. Voluminous steam-rich plumes were observed on 24 August rising as high as 700 m above the crater rim and drifting N. The 25 August measurement was the second highest emission average ever recorded at the volcano. Sulfur dioxide emissions decreased to 3,447 t/d on 26 August.
Higher sulfur dioxide gas fluxes had been recorded in 2024 with an average of 1,273 t/d prior to the 3 June eruption; afterward the eruption emissions were elevated, averaging 3,351 t/d. An average of nine volcanic earthquakes per day also persisted after the 3 June eruption. Ground deformation data from continuous GPS and electronic tilt data indicated slow inflation of the volcano since March 2022; the rate of inflation at the E flank increased in 2023 and at the SE flank beginning in July 2024. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon at 2330 on 10 August noting increased sulfur dioxide emissions. Earlier in the day a Flyspec instrument measured an average of 4,839 tonnes per day (t/d) of sulfur dioxide emissions at the summit crater, the third highest value recorded in 2024. Gas emissions rose 400-600 m above the carter rim and drifted SE and NE during 10-13 August. Another special notice was issued at 1830 on 13 August noting that the Flyspec instrument measured an average of 7,307 t/d, the highest sulfur dioxide emissions ever recorded at the volcano. Higher sulfur dioxide gas fluxes had been recorded in 2024 with an average of 1,273 t/d prior to the 3 June eruption; afterward the eruption emissions were elevated, averaging 3,102 t/d. An average of nine volcanic earthquakes per day also persisted after the 3 June eruption. Ground deformation data from continuous GPS and electronic tilt data indicated inflation of the volcano since March 2022 and specifically at the E flank starting in 2023. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported that moderate emissions at Kanlaon rose 100-400 m and drifted in several directions during 11-16 July. Sulfur dioxide emissions were as high as 2,556 tonnes per day measured on 13 July. There were 2-19 daily volcanic earthquakes recorded by the seismic network. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that daily diffuse gas-and-steam emissions at Kanlaon rose 100-150 m and drifted mainly NW, W, and SW during 25 June-2 July. Sulfur dioxide emissions averaged 2,774 tonnes/day (t/d) on 25 June, 3,299 t/d on 27 June, and peaked at 5,397 t/d on 28 June, the highest value recorded since instrumental gas monitoring began. Emissions averaged 3,007 t/d on 30 June and then peaked again at 5,083 t/d on 2 July, the second highest recorded value in 2024 and the third highest since monitoring began. PHIVOLCS noted that increased sulfur dioxide emissions had been recorded in 2024, averaging 1,897 t/d, though emission since the 3 June eruption were particularly elevated with a current average of 3,254 t/d. There were 1-14 daily volcanic earthquakes recorded by the seismic network; volcanic earthquake activity persisted at an average of 10 events/day since the 3 June eruption. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that intense rain on 6 June mobilized ash deposited during the 3 June eruption at Kanlaon causing lahars to descend the S flank and impact local communities. The lahars began at around 1300 and lasted 25 minutes based on seismic data. They deposited cohesive gray mud, plant debris, and gravel in at least four stream channels including Tamburong Creek, which courses through Biak-na-bato and Calapnagan, La Castellana; Intiguiwan River in Guinpanaan and upstream Baji-Baji Falls in Cabacungan, La Castellana; Padudusan Falls, Masulog, Canlaon City; and the Binalbagan River, which drains the S flank of the volcano. Lahars overflowed parts of Tamburong Creek and deposited material a few centimeters thick along a section of the main road in Biak-na-Bato, making it impassable to motorists. Thunderstorms continued and channel-confined lahars on the S and W flank were detected the next day. The lahars began at around 1450 on 7 June and lasted 80 minutes based on seismic data. They were described as cohesive and cement-like and carried tree debris along the Baji-Baji Falls and Ibid Creek, in Cabacungan, La Castellana. Lahars also descended the Santo Guintubdan, Ara-al, La Carlota City and muddy waters were observed in the Buslugan, Busay Oro, Busay Abaga, Busay Mayor, Busay Kapid, Kabkaban, Ezzy, Busay Ambon, and Labi Labi falls. Voluminous gas-and-steam emissions rose 1.5-2 km above the summit and drifted NE and SW during 6-8 June.
A special notice was issued on 8 June due to elevated sulfur dioxide levels. During a field survey sulfur dioxide flux averaged of 4,397 tonnes per day (t/d) which was the highest level recorded so far this year and the second highest land-based measurement for Kanlaon. Sulfur dioxide emissions were elevated in 2024, averaging 1,458 t/d, though after the 3 June eruption the daily average increased to 3,347 t/d. Emisisons had decreased on 9 June, averaging 3,304 t/d. The rate of volcanic earthquakes persisted at above-background levels with an average of 33 events per day. Moderate steam-and-gas emissions rose 300-500 m above the summit and drifted NE and SW during 9-11 June. At least 1,237 families or 4,190 residents of five barangays remained in evacuation shelters according to a 12 June news article; many had health problems from exposure to sulfur dioxide gas and ash. The Alert Level remained at 2 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); The Philippine Star
PHIVOLCS reported that at 1851 on 3 June an explosive eruption at Kanlaon ejected incandescent material and produced a voluminous ash plume that rapidly rose 5 km above the vent and drifted W. Pyroclastic density currents generated from column collapses traveled 2-3 km down the S and SE flanks based on webcam views. The eruption was recorded by all 10 seismic stations, three infrasound stations, and webcams, and lasted six minutes based on the seismic data. Rumbling was heard in a La Castellana, La Carlota City, and Canlaon City. Coarse ashfall was reported in those same areas and additionally in Bago City. A sulfur odor was also reported in many neighborhoods in the cities of Bago, Bacolod, La Carlota, La Castellana, Murcia, and Canloan City. The Alert Level was raised to 2 (on a scale of 0-5) at 2000 and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone. The eruption was preceded by a M 3.5 volcano-tectonic earthquake at 1847. The gas (sulfur dioxide) portion of the plume rose 8-17 km, reaching the upper troposphere based on satellite data.
Abundant gas emissions followed the eruption and then waned by 0820 on 4 June. The emissions likely entrained ash that fell in minor amounts SW of the volcano. Sulfur dioxide emissions averaged 4,113 t/d, the highest gas flux recorded in 2024 and the second highest ever recorded at Kanlaon. According to the National Disaster Risk Reduction and Management Council (NDRRMC), a total of 1,888 people had evacuated to 11 evacuation shelters and a total of eight domestic flights and one international flight were cancelled.
Periodic swarms of volcano-tectonic earthquakes had been recorded since March 2020 and seismicity had been above background levels during the previous month. The report noted that sulfur dioxide emissions had been variable but increasing overall since May 2023 and anomalously high during the 2024, averaging 1,273 tonnes per day (t/d); background levels averaged less than 300 t/d.
Sources: The National Disaster Risk Reduction and Management Council (NDRRMC); Philippine Institute of Volcanology and Seismology (PHIVOLCS); Simon Carn
In a special notice for Kanlaon, PHIVOLCS stated that the seismic network detected 24 volcano-tectonic earthquakes during 1335-1630 on 26 May with local magnitudes of 0.8-2.3 and depths of 0-6 km beneath the W flank. Sulfur dioxide gas emissions from the summit crater had been elevated since 1 January, averaging 1,291 tonnes/day (t/d); the most recent measurement was 2,003 t/d, recorded on 26 May. Ground deformation data from continuous GPS and electronic tilt data had been recording inflation at the volcano since March 2022. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon at 1530 on 30 April noting increased sulfur dioxide emissions. On 30 April a Flyspec instrument measured an average of 2,707 tonnes per day (t/d) of sulfur dioxide emissions at the summit crater, the second highest value recorded in 2024; sulfur dioxide emissions average 3,098 t/d on 19 January. The report noted that higher sulfur dioxide gas fluxes had been recorded for a year with an overall average of 1,300 t/d. The rate of volcanic earthquakes remained at baseline levels of three events per day, though episodes of increased activity had occurred several times during the previous year. Ground deformation data from continuous GPS and electronic tilt data indicated inflation of the volcano since March 2022 and specifically at the E flank starting in 2023. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
In a special notice for Kanlaon, PHIVOLCS stated that the seismic network detected 15 volcano-tectonic earthquakes during 0358-0500 on 22 November with local magnitudes of 1.4-4.2 and depths of 0-2 km beneath the N flank. Sulfur dioxide gas emissions from the summit crater were elevated since 1 May, averaging 570 tonnes/day (t/d); the most recent measurement was 1,017 t/d, recorded on 14 November. Ground deformation data from continuous GPS and electronic tilt data had been recording inflation at the volcano since March 2022, and inflation of the mid-SW flank since October. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon at 0900 on 6 September, noting increased seismicity. The seismic network detected 36 volcanic earthquakes including 34 volcano-tectonic earthquakes between 0500 on 4 September and 0750 on 6 September at depths of 0-9 km beneath the NE flank. The earthquakes had local magnitudes of 0.8-3.4. Ground deformation data from continuous GPS and electronic tilt data had been recording inflation at the mid-flanks of the volcano since March. Sulfur dioxide emissions at the summit crater averaged 788 and 301 tonnes per day (t/d) on 7 and 11 September, respectively. The number of volcano-tectonic earthquakes decreased during the rest of the week; there were 23 recorded during 6-7 September and 2-9 daily earthquakes during 8-12 September. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon at 1000 on 21 July, noting increased seismicity. The seismic network detected 35 volcano-tectonic earthquakes between 2200 on 20 July and 0906 on 21 July at depths of 12-15 km beneath the summit crater. The earthquakes had local magnitudes of 0.9-2.3. Ground deformation data from continuous GPS and electronic tilt data had been recording inflation at the mid-flanks of the volcano since March. Sulfur dioxide emissions at the summit crater averaged 786 tonnes per day (t/d) on 18 July and 230 t/d on 21 July, slightly higher than the average of 566 t/d measured in March. The number of volcano-tectonic earthquakes decreased during the rest of the week; there were 16 recorded during 21-22 July and 1-2 daily earthquakes during 23-25 July. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon at 2030 on 4 May, noting increased seismicity and ground deformation, and ongoing elevated sulfur dioxide emissions. Ground deformation data from continuous GPS and electronic tilt data indicated short-term inflation of the lower and mid-flanks of the volcano since March, though during the second week of April inflation was pronounced at the SE mid-flank. Real-time, continuous gas monitoring of thermal springs on the N flank detected sulfur dioxide for the first time beginning in April. Sulfur dioxide emissions at the summit crater averaged 632 tonnes per day on 1 May, lower than the average of 1,099 tonnes per day measured the day before, but higher than the average of 124 tonnes per day emitted since March. The seismic network detected 20 shallow volcanic earthquakes (M 1.2-2.4) beneath the summit crater between 2225 on 3 May until 1600 on 4 May. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon at 0700 on 1 May, noting increased sulfur dioxide emissions. Real-time, continuous volcanic gas monitoring of thermal springs on the N flank detected sulfur dioxide for the first time beginning in April. On 30 April a Flyspec instrument measured an average of 1,099 tonnes per day of sulfur dioxide emissions at the summit crater, a value which was significantly higher than the average of 124 tonnes per day measured since March. During the month of April, the seismic network recorded 141 volcanic earthquakes, an average of five per day, at shallow depths less than 10 km in the N and W parts of the volcano. Ground deformation data from continuous GPS and electronic tilt data indicated short-term inflation of the lower and mid-flanks of the volcano since March. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon at 1400 on 3 July, noting increased earthquake activity beneath the summit. A total of 41 volcanic earthquakes were recorded by the seismic network beginning at 0500 on 30 June, including seven shallow tornillo signals indicating gas movement through fractures in the upper flanks. Ground deformation data from continuous GPS indicated minor, short-term inflation of the lower and mid-flanks of the volcano since January 2022, consistent with continuous electronic tilt data that had recorded inflation on the SE flanks since mid-March 2022. The seismicity and inflation likely reflected shallow hydrothermal processes. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon on 9 February, noting localized earthquake activity on the lower NW flank. There were 11 very shallow earthquakes, with local magnitudes of M 0.9-2.1, recorded by the seismic network between 2012 on 8 February and 0900 on 9 February. Ground deformation data from continuous GPS and tilt measurements indicated slight inflation of the middle and upper flanks of the volcano since mid-October 2021; EDM and electronic tilt data reflected short-term deflation on the SE flank since December 2021 and January 2022, respectively. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS issued a special notice for Kanlaon on 21 January, noting that a total of 18 volcanic earthquakes were recorded in the past day. Four of those events were classified as shallow “tornillo” signals indicating gas movement along shallow fractures in the upper part of the volcano. Ground deformation data from continuous GPS and tilt measurements indicated slight inflation of the volcano since mid-October 2021. The seismic activity and ground deformation was likely caused by shallow hydrothermal processes and could generate phreatic events. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported slightly increased seismic activity and volcanic gas flux at Kanlaon. The seismic network recorded 28 volcanic earthquakes during 11-13 February with local magnitudes between 0.7 and 2.2. They were located at shallow depths around 10 km across the N to E portions of the edifice. The sulfur dioxide emission rate on 13 February was 1,130 tonnes per day, the highest value recorded this year; sulfur dioxide emissions had been higher than background levels of 300 tonnes/day since June 2020. Ground deformation data from continuous GPS and tilt measurements indicated slight inflation of the lower and middle flanks since June 2020. Increased seismic activity continued through 16 February; from 0800 on 14 February to 0800 on 16 February there were a total of 59 earthquakes. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that the seismic network recorded 6-44 volcano-tectonic earthquakes per day at Kanloan during 23-30 June and 1-4 volcanic earthquakes during 27-29 June. Steam plumes rose 100-300 m above the summit and drifted NE, NW, and SW. A M 3.6 earthquake was recorded at 1900 on 23 June and was felt at Intensity III in La Carlota City and at Intensity II in Bago City, Negros Occidental. Sulfur dioxide emissions were 438, 237, and 116 tonnes per day on 13, 24, and 27 June, respectively. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that ground deformation data from continuous GPS measurements at Kanlaon indicated slight deflation of the lower and middle flanks since January. Tilt data from instruments on the SE flank recorded continuing deflation on the lower flanks and inflation of the mid-flank since April 2020. White steam plumes rose 100-200 m above the summit and drifted NW and SW.
The seismic network recorded as many as 10 volcanic earthquakes per day during 17-21 June. A series of earthquakes beneath the lower W flank began at 1603 on 21 June, and by 0800 the next morning there were a total of 136 events recorded. Five of the earthquakes (recorded at 0101, 0104, 0134, 0206, and 0507 on 22 June) were M 3-4.7, and were felt at Intensities II to IV in La Carlota City and Bago City, Negros Occidental, and Canlaon City, Negros Oriental. During 22-23 June there were a total of 104 volcano-tectonic earthquakes beneath the W flank. The Alert Level remained at 1 (on a scale of 0-5) and PHIVOLCS reminded the public to remain outside of the 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that ground-deformation data at Kanlaon indicated long-term slow inflation of the volcano since 2017, slow inflation of the lower flanks since May 2019, and notable inflation of the upper flanks beginning near the end of January 2020. The seismic network recorded a total of 80 volcanic earthquakes since 9 March; 77 of them were low-frequency events associated with magmatic fluids. The deformation and seismic data both indicated unrest; PHIVOLCS raised the Alert Level to 1 (on a scale of 0-5) on 11 March and reminded the public to remain outside of the 4-km-radius Permanent Danger Zone. During 12-17 March there were between two and eight volcanic earthquakes recorded daily.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
On 25 October PHIVOLCS lowered the Alert Level for Kanlaon to 0 (on a scale of 0-5) noting that volcanic activity had declined to baseline levels in June and had continued to be low.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that during 17-19 April dirty-white steam plumes from Kanlaon rose as high as 1.2 km above the crater rim and drifted SW, NW, and NE. White steam plumes rose 300-600 m and drifted SW and NW during 20-24 April. The Alert Level remained at 2 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that there were three or fewer volcanic earthquakes detected at Kanlaon each day during 27 December 2017-2 January 2018. Dense weather clouds prevented visual observations, though on 30 December a steam plume was seen rising 500 m above the crater rim and drifting SW. The Alert Level remained at 2 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that during 19-20 December there were 412 volcanic earthquakes detected at Kanlaon. A low-energy, explosion-type earthquake was detected at 0233 on 21 December associated with gas emissions from the summit area. Later in the day steam plumes rose 400 m and drifted NE. The number of daily volcanic earthquakes increased to 957 the next day and then decreased to less than 20 per day during 22-23 December; the daily count increased to 382 and 776 events on 24 and 25 December, respectively, and then decreased to 82 on 26 December. White plumes rose 300 m and drifted NE, NW, and SW on 21 December, and 700 m on 26 December; weather clouds prevented views on the other days. The Alert Level remained at 2 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported between 1 and 7 volcanic earthquakes at Kanlaon were recorded each day during 2-8 December, prior to the phreatic eruption on 9 December. Only three events were detected on 10 December, and then the number increased to 155 the next day. The number of daily volcanic earthquakes increased to 578 on 13 December, rising to 1,007 the next day, and peaking at 1,217 on the 15th. The earthquake count dropped to 149 on 16 December before returning to six or less through 19 December. White steam plumes rose 800 and 300 m above the crater on 13 and 14 December, respectively. White plumes were diffuse on 15 December; weather clouds prevented views of the summit area during 16-18 December. Sulfur dioxide emissions were 603-687 tons per day during 13-14 December. The Alert Level remained at 2 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that an approximately 10-minute-long, low-energy phreatic eruption at Kanlaon began at 0947 on 9 December. A plume of voluminous steam and dark ash rose 3-4 km above the summit vent. The event was heard as far away as La Castellana, Negros Occidental. Minor amounts of ash fell in Sitio Guintubdan, and barangays Ara-al, Sag-ang, and Ilihan. The eruption was preceded by the resumption of degassing at the summit crater at 0634, detectable as continuous low-energy tremor during periods when the summit was not visible; degassing was last observed September 2016. The Alert Level remained at 2 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that between 24 June and 18 August the seismic network at Kanlaon detected 244 volcanic earthquakes. The report stated that the increased seismic activity could be followed by phreatic explosions at the summit crater, despite the absence of visible degassing or steaming from the active vent during 2017. The Alert Level was raised to 1 (on a scale of 0-5), and the public was warned to not enter the 4-km-radius Permanent Danger Zone (PDZ).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
On 5 May PHIVOLCS reported that since the last phreatic eruption at Kanlaon, which occurred on 15 June 2016, there has been a general decline in activity: seismicity was at baseline levels, no significant deformation had been detected since August 2016, sulfur dioxide emissions were low, and no steaming had been observed since 29 September 2016. The Alert Level was lowered to 0 (on a scale of 0-5), though the public was warned to not enter the 4-km-radius Permanent Danger Zone (PDZ).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that during 20-25 July diffuse white plumes rose above Kanlaon; On 20 July plumes were a dirty-white color, and on 25 July they rose 200 m and drifted NW and SW. The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that during 22-23 and 25-26 June white steam plumes from Kanlaon rose as high as 800 m and drifted NW and SW; wispy steam plumes were observed on 27 June. Starting at 1640 on 23 June the seismic network recorded a 4-minute-long, explosion-type signal; weather clouds prevented visual observations of the summit area. The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Based on visual observations, PHIVOLCS reported that a series of three eruptive events occurred at Kanlaon on 18 June, beginning at 0919 and lasting 27 minutes. These events were recorded by the seismic monitoring network as consecutive explosion-type earthquakes that lasted 30, 42, and 29 seconds, respectively. The first event, a steam-and-gas explosion, generated a light gray-to-white ash plume that rose 1.5 km above the crater and then later to 3 km. The second event, an ash eruption immediately following the first event, produced a dense black ash plume that rose 500 m. Lastly, a grayish ash plume rose 500 m. Minor ashfall was reported to the W in the barangays of Ara-al, San Miguel, and Yubo in La Carlota City (14 km W), Sag-ang in La Castellana (16 km SW), and Ilijan in Bago City (30 km NW). A diffuse sulfur odor was detected in Ara-al. The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that long-duration tremor began at Kanlaon at 0130 on 30 March. The tremor was accompanied by gas-and-steam plumes that rose 600-700 m and drifted SW and SSW during 30 March-1 April. On 31 March minor ashfall was reported in areas downwind including in parts of La Carlota City (14 km W), La Castellana, and Bago City in Negros Occidental. The tremor continued during 2-4 April, though the energy decreased, and steam plumes rose 400-500 m. On 5 April steam plumes rose 800 m and drifted SW. The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that at 1820 on 29 March the seismic network at Kanlaon detected an explosion that lasted about 12 minutes. The event was accompanied by a booming sound heard in communities to the W, including Ara-al, Yubo, La Carlota City (14 km W), and Canlaon City (8 km ESE) in Negros Occidental. Observers to the SE reported an ash plume that rose 1.5 km above the crater; minor amounts of ash fell in areas downwind. Incandescent ejecta caused a small bushfire on the upper flank. A 25-second-long explosion was detected at 1918. The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that at around 1230 on 30 Decemeber a low-energy explosion at Kanlaon, observed by residents in barangays Cabagnaan and Sag-ang in La Castellana (16 km SW), produced an ash plume that rose 100 m above the crater and slowly drifted SW. The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that at 1457 on 23 December the seismic network at Kanlaon detected an explosion. The event was not visually observed due to dense weather clouds around the summit area but rumbling was heard in nearby barangays including Cabagnaan, La Castellana (16 km SW), and Ara-al and Yubo, La Carlota City (14 km W). Minor amounts of ash fell in Ara-al, Haguimit, and La Granja, La Carlota City, and a sulfur odor was noted in barangay Tres Elis, La Castellana. An explosive event detected by the seismic network at 2109 on 24 December was again not visually observed. Trace amounts of ash fell in Ara-al, Haguimit, and La Granja, and a sulfur odor was reported in Tres Elis. White steam plumes rose 100 m above the crater and drifted SW on 26 December. A five-minute long ash event that began at 1329 on 27 December was accompanied by rumbling heard in a few local barangays. An eruption plume, viewed from the SE flank, rose 1 km above the crater, and may have risen as high as 4.5 km based on pilot observations. Minor ashfall was noted in Ara-al, Yubo, and La Granja, Cabagnaan, Sag-ang (La Castellana), barangay Miranda, Hinigaran (Negros Occidental), Municipality of Pontevedra (Negros Occidental), and reached as far as Nueva Valencia, Guimaras (58 km WNW). The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that at 2138 on 15 December a low-frequency earthquake at Kanlaon that lasted 45-47 seconds possibly corresponded to an ash emission, though inclement weather prevented visual observations of the crater. Rumbling was heard in neighborhoods on the SE flank. On 17 December white steam plumes rose 50 m above the crater. Poor weather conditions prevented views of the crater through 22 December.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that two volcanic earthquakes at Kanlaon were accompanied by a one-minute, low-energy, gray ash emission at 0513 on 11 December. Observers noted ash emissions at 0951, 1008, 1140, and 0101 on 13 December which rose 200-300 m and drifted SW. The emissions were not detected by the seismic network, indicating a shallow source. Trace amounts of ashfall were reported in Sitio Bais, Brgy Yubo, and La Carlota City on the W flank and Brgy Sag-ang and La Castellana on the SW flank. The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that the seismic network for Kanlaon detected 11 volcanic earthquakes during 24-25 November. Emissions of gas and ash rose 150 m above the crater and drifted SW on 25 November. The Alert Level remained at 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
PHIVOLCS reported that the seismic network for Kanlaon detected an explosion-type signal beginning at 0930 on 23 November, culminating with an 8-minute-long steam explosion. Observers reported that a white plume rose 1-1.5 km above the crater and drifted SW, and rumbling was heard in local areas. Only four volcanic earthquakes had been recorded during the previous week, but after the explosion, the network detected volcanic tremor that lasted for five hours. The Alert Level was raised to 1 (on a scale of 0-5). Continuous steam emissions with minor ash content were observed the next morning.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Based on a pilot observation, the Tokyo VAAC reported that on 15 May an ash plume from Kanlaon rose to an altitude of 2.4 km (8,000 ft) a.s.l. and drifted W. Ash was not identified in satellite imagery. [PHIVOLCS later confirmed that the plume originated from a fire and not an eruption. Monitored parameters for Kanlaon indicated normal levels and the Alert Level remained at 0 (on a scale of 0-5).]
Source: Tokyo Volcanic Ash Advisory Center (VAAC)
PHIVOLCS reported that during 23 August-1 September the seismic network for Kanlaon detected a significant rise in the number of earthquakes. A few of the earthquakes were felt as far away as Bago City, 30 km NW. The epicenters clustered on the NW flank.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
According to news articles, PHIVOLCS lowered the Alert Level for Kanlaon to 0 on 25 April. Seismic activity was at background levels during 5 March-25 April, with 0-3 earthquakes per day. Mt. Kanlaon Natural Park opened for mountaineering activities; however visitors were warned that the risk of entering the 4-km permanent danger zone remained high.
Source: Sun Star News
PHIVOLCS reported that during 7-10 February the seismic network for Kanlaon detected a significant rise in earthquakes. On 10 February the Alert Level was raised from 0 to 1 (out of 5). Cloud cover prohibited visual observations of the summit. The public was strongly advised not to enter the 4-km Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
On 2 November, PHIVOLCS reported the lowering of the Alert Level for Canlaon from 1 to 0. During 26 July-2 November, no ash explosions occurred and steam emissions and seismicity were low.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Based on interpretations of seismic data, an explosion at Canlaon that lasted more than 10 minutes occurred on 23 July. An ash column was not observed due to cloud cover. Trace deposits of ash fell up to 9 km ENE of the crater in the neighborhoods of Pula, Malaiba, and Lumapao. On 24 July, PHIVOLCS reported a total of 16 volcanic earthquakes, 3 short-duration tremors, and 2 earthquakes indicating small explosions. Ash was not observed.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Minor steam-and-ash emissions that were observed from Canlaon during 21-24 June reached a maximum height of 1.5 km above the summit (12,900 ft a.s.l.) and drifted NW and SW. Light ash fall was observed approximately 25 km SW in the municipality of La Castellana. The alert status remained at Level 1, which restricts activity within 4 km of the summit.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Minor steam-and-ash emissions that were observed from Canlaon during 13-15 June reached heights of 2 km above the summit (14,600 ft a.s.l.) and drifted primarily NE and NW. Light ashfall was observed on the volcano's upper N flanks and reached approximately 10 km E in Canlaon City. The alert status remained at Level 1, which restricted activity within 4 km of the summit.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Small explosions on 3, 10-11, and 12 June generated steam-and-ash emissions from Canlaon that reached maximum heights of 1 km above the summit (11,300 ft a.s.l.) and drifted NW and SW. Ash fell on the upper SW slopes during 10-12 June. The alert status was raised on 12 June to Alert Level 1 (scale 0 to 5), which restricts activity within 4 km of the summit.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Steam emissions continued at Canlaon during 25-26 May, rising to a maximum height of 1 km above the volcano's crater (11,300 ft a.s.l.). Seismic activity remained at low levels. The sulfur-dioxide flux was at ~1,400 metric tons on 26 May, above the usual flux of 500 metric tons per day.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Phreatic activity continued at Canlaon during 18-23 May, with ash-and-steam plumes rising to ~1 km above the volcano (~11,300 ft a.s.l.). This activity was not recorded in seismic data. The sulfur-dioxide flux on 22 May was at ~2,080 metric tons per day, much higher than the normal flux of 500 metric tons per day. Canlaon remained at Alert Level 1, with a 4-km Permanent Danger Zone around the summit off limits to visitors.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Multiple episodes of mild ash and steam ejections were observed at Canlaon during 10-11 May that sent clouds to heights of up to 500 m above the vent before being blown NW. These episodes were not seen in the seismic record. The hazard status remained at Alert Level 1.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Contingency plans formulated earlier this year by local governments in consultation with PHIVOLCS in the event of a major eruption were misinterpreted in press reports indicating that evacuations were being recommended. The current level of activity does not require any evacuation or facility closures. Ongoing ash emissions are only a concern on the upper slopes of the volcano within 4 km of the summit crater. Regular mild ash-and-steam clouds rising less than 800 m above the crater did not cause ashfall in local communities during 3-10 May.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
During 27 April to 2 May, mild ash-and-steam emissions from Canlaon produced plumes to a maximum height of 1 km above the volcano (11,300 ft a.s.l.). The sulfur-dioxide flux began to increase on 28 April, reaching 2,700 tons on 1 May. According to news reports, flights to and from nearby Kalibo airport were suspended on 3 May due to reduced visibility.
Sources: Inquirer.net; Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Mild ash eruptions continued at Canlaon during 21-26 April, producing plumes as high as 1 km above the volcano (11,300 ft a.s.l.). Emissions on 21 April drifted SW and deposited small amounts of ash in the villages of Sagang, Mansalanao, Old Fabrica, Biak-na-Bato, Kamandag, Tinago, and Cabagnaan of the town La Castillana. Emissions on 22 April deposited ash in Manghanoy and Cabagnaan. Emissions on 25 April deposited traces of ash in Canlaon City. Canlaon remained at Alert Level 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
During 13-14 April, mild ash emissions at Canlaon produced plumes to a height of ~700 m above the crater (~10,300 ft a.s.l.). During 15-17 April, moderate-to-strong emissions produced ash plumes to ~2 km above the crater (~14,600 ft a.s.l.) and deposited ash in villages as far as La Castellana (16 km SW of the crater). Canlaon remained at Alert Level 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
A low-energy ash emission from Canlaon on 7 April at 1429 generated a cloud to a height of ~100 m above the crater (~8,300 ft a.s.l.). The cloud slowly drifted SW. Only the crater and upper SW slopes of the volcano were affected by the emission. According to PHIVOLCS, the seismic monitoring network around the volcano did not record any earthquakes during the event. Canlaon remained at Alert Level 1.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Ash emissions began from Canlaon on 20 March around 1300. Small amounts of ash fell in the town of Guintubdan 5 km W of the volcano. During 24 March to 4 April, sporadic ash emissions rose to a maximum height of 1 km above the volcano (11,300 ft a.s.l.). During this time ash fell in the towns of La Castellana (16 km SW of the crater), Upper Sag-ang, Yubo (5-6 km SW), and Guintubdan (5-6 km WNW). Due to this low-level episode of unrest, PHIVOLCS raised the Alert Level at Canlaon from 0 to 1 on 30 March. There was also a 4-km-radius Permanent Danger Zone around the volcano's summit. According to a news article, pilots were advised to avoid flying near Canlaon.
Sources: The Philippine Star; Inquirer.net; Philippine Institute of Volcanology and Seismology (PHIVOLCS)
A brief ash emission began at Canlaon around 0930 on 21 January. The cloud produced from the emission rose to an approximate height of 500 m above the active crater and drifted WNW and SW. No coincident volcanic earthquakes were recorded. There were fine ash deposits in the city of Cabagnaan, ~5.5 km SW of the crater. PHIVOLCS advised the public to avoid entering the 4-km-radius Permanent Danger Zone around the volcano.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
On 1 March PHIVOLCS reduced the Alert Level at Canlaon from 1 to 0, due to low seismicity and volcanism. After September 2003, either no activity or weak steam emissions were observed at the summit crater and seismicity was at normal levels. The public was advised that there was still a risk of sudden phreatic explosions occurring in the 4-km Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
An emission from Canlaon on 10 July at 1735 sent an ash-and-steam cloud to a height of ~1 km above the summit. The cloud was visible from Canlaon City and drifted NW, SW, and NE, depositing ash in an area within a 4 km radius around the crater. Emissions also occurred on 11 July during 0620-0624 and 0658-0705 that rose to ~1.3 km above the crater and drifted SE. Canlaon remained at Alert Level 1, with a 4-km-radius Permanent Danger Zone.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
As of 4 July, moderate steam-and-ash emissions continued at Canlaon, with ash columns reaching ~900 m above the summit. Low-frequency volcanic earthquakes and low-frequency short duration harmonic tremor were recorded. According to PHIVOLCS, based on Canlaon's historical behavior the mild phreatic activity that is occurring is probably related to hydrothermal disturbances at shallow depths. The absence of longer duration harmonic tremors suggested no active magma movement or intrusion. However, sudden ash emissions and explosions are still expected to occur anytime without warning. Canlaon remained at Alert Level 1 (on a scale of 0-5).
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
On 17 and 18 June multiple small emissions occurred at Canlaon. On the 17th and on the morning of the18th ash-and-steam plumes rose to a maximum height of ~400 m above the volcano and drifted NE. On the afternoon of the 18th plumes drifted SE. Low-frequency volcanic earthquakes were recorded prior to the eruptions. Canlaon remained at Alert Level 1 (on a scale of 0-5), with a 4-km-radius Permanent Danger Zone.
Sources: ABS-CBN News; SunStar News; Philippine Institute of Volcanology and Seismology (PHIVOLCS)
According to a news article, an ash emission occurred from Canlaon on 8 June during 0645-0700. Small amounts of ash fell in Canlaon City, Barangay Masulog, and Barangay Linutangan. In addition, PHIVOLCS recorded several low-frequency volcanic earthquakes and short-duration harmonic tremor. Moderate steaming occurred, which was above normal levels. The Alert Level at Canlaon remained at 1 (on a scale of 0-5), with a 4-km-radius Permanent Danger Zone.
Source: Sun Star News
A small ash puff was released from Canlaon on 28 November at 0721. The puff rose to a height of ~100 m above the active crater and drifted SW. Associated volcanic tremor was recorded at Cabagnaan and Guintubdan stations. Traces of ash fell at Cabagnaan station, SSW of the active crater. Moderate steam emissions were observed immediately after the ash puff and a few discrete tremors were recorded. PHIVOLCS advised the public to remain outside of the 4-km-radius Permanent Danger Zone.
Sources: ABS-CBN News; Philippine Institute of Volcanology and Seismology (PHIVOLCS)
During early February, high-frequency earthquakes were recorded at Canlaon at depths of 1-5.5 km. In the previous week, several low-frequency earthquakes were recorded. According to a news report, PHIVOLCS stated that the occurrence of low-frequency earthquakes supports the idea that some fluid migration, possibly magma ascent, is occurring. The Alert Level remained at 1 ("Low-level unrest"), and a 4-km-radius Permanent Danger Zone was in effect.
Source: Sun Star News
PHIVOLCS noted in a 21 March report that since January 2001 earthquake clusters or occurrences have been recorded by the seismic monitoring network around the volcano. These earthquakes may signify a reactivation of the volcanic system at depth and could be a precursor to more vigorous activity, such as ash explosions. This interpretation is based on similar earthquake clusters manifested prior to the 10 August 1996 phreatic explosion from the active summit crater of the volcano. In view of the possibility of a sudden ash ejection, PHIVOLCS recommends the immediate suspension of all treks to the summit crater until further notice. As an additional precaution, the pre-defined 4-km-radius Permanent Danger Zone (PDZ) should be avoided at all times.
Source: Philippine Institute of Volcanology and Seismology (PHIVOLCS)
Reports are organized chronologically and indexed below by Month/Year (Publication Volume:Number), and include a one-line summary. Click on the index link or scroll down to read the reports.
Ash eruptions cause mudflow hazards
Card 0792 (14 October 1969) Ash eruption on 11 October
The following cable was received from the American Embassy in Manila. "Canlaon Volcano on Negros Island erupted 2200 on 11 October (local time). Activity was ash eruption only. Present activity slight emission of white steam. No lava flow observed. Eruption consisted of ash laden clouds, air shock manifested during eruption. Ash deposited on W slope of volcano."
The following report is from Father Hennessey. "Canlaon . . . erupted at 2205 local time, 11 October 1969. An earthquake was felt in the vicinity. A mild ejection of ashes on the western slope; eruption cloud of white smoke for 25 minutes; no report of molten lava; very little change in physical and biological environment. Present activity is quiet."
Card 0798 (21 October 1969) Strong ash eruption on 14 October; ashfall and mudflow hazard
The following is from the "Manila Bulletin" on 15 October 1969. "Canlaon volcano emitted yesterday afternoon ashes that soared up to 15,000 feet after showing signs of cooling off the past few days. The new ash emission, according to the commisssion on volcanology, was accompanied by booming sounds like distant cannon blasts. COMVOL said the ash emission started at 1722 and lasted up to 1800. After that, the volcano ejected white steam. The ashes rising above the volcano's summit drifted southwest, according to Comvol. This development confirmed COMVOL's earlier evaluation that the volcano would be puffing ash at varying degrees for some time.'
The following is from the "Manila Times" on 16 October 1969. "A 35-hectare area caved in last night in barrio Malawig at the foot of the Canlaon Volcano after it erupted at 1725 yesterday. Red Cross Director Dr. Mariano Beltran reported that an accumulation of sulfuric sands blocked a road in barrio Biak-na-bato of this town which links Negros Occidental to Negros Oriental. The mudflow menace persisted yesterday over Canlaon Volcano in Negros as heavy rains turned heay deposits of ashes on its upper slopes into new rivers of mud. Rogelio Datuin, supervising volcanologist, said that the volcano's activity has returned with no seismic disturbance recorded during the past 24 hours."
The following is from the "Manila Times" on 11 October 1969. "Canlaon Volcano is an andesitic volcano and no violent eruptions are recorded, but ash has been ejected from time to time, and characterized further by continuous emission of vapor of sulfur dioxide under high temperature."
Information Contacts: Card 0792 (14 October 1969)Mr. Bryoade, American Embassy, Manila, Philippines; Father Hennessey, Manila Observatory, Manila, Philippines.
Card 0798 (21 October 1969)The Manila Bulletin, Manila, Philippines; The Manila Times, Manila, Philippines; J.J. Hennessey, Manila Observatory, Manila, Philippines.
Twenty-minute ash eruption
A brief ash eruption began at [0610] on 27 June. A grayish eruption column rose [~1,500 m] above the summit before being blown S by strong prevailing winds. Ash fell on S-flank villages within 8 km of the summit. The eruption ended after about 20 minutes, and was succeeded by voluminous but low-pressure emission of white vapor.
Information Contacts: G. Andal, Commission on Volcanology (COMVOL), Quezon City.
Intermittent ash emission continues
Intermittent ash emission continued through July. The most recent ash emission occurred at 1253 on 31 July when a brownish column rose 700 m above the crater, accompanied by volcanic tremor.
Information Contacts: G. Andal, COMVOL, Quezon City.
Intermittent ash emission continues
Canlaon ejected steam and a little ash for 4.5 hours on 2 August. The cloud rose 800-1,400 m above the crater rim. Seismographs recorded local activity. A smaller eruption occurred at 0610 on 9 August, producing a 250-m cloud. [A smaller eruption ended with small explosions on 14 August at 0615 and 2 September at 1600.]
Further Reference. Oanes, A., 1978, 1978 Canlaon volcano eruption: COMVOL report (unpub.).
Information Contacts: G. Andal, COMVOL, Quezon City.
Earthquake swarm
COMVOL reported that an average of 60 earthquakes/day were recorded near Canlaon in mid-May, reaching a maximum of 160 on 17 May [but see 5:6]. COMVOL installed three additional seismic stations around the volcano and extended the danger zone from 4 to 10 km. A similar earthquake swarm preceded the 1978 eruption.
Information Contacts: AFP.
Seismicity declines
An earthquake swarm began 6 May in the vicinity of Canlaon. The number of earthquakes recorded per day on nearby seismographs reached a peak of 108 on 19 May, then seismicity began a gradual decline. In late June, volcanic shocks continued to occur at a rate of about 40/day. As of 27 June, a total of 2,652 events had been recorded. No surface volcanism has been reported with this earthquake swarm.
Information Contacts: O. Peña, COMVOL, Quezon City.
Seismicity still above normal in late November
Seismic activity has lessened considerably, but remained above normal as of late November.
Information Contacts: O. Peña, COMVOL, Quezon City.
Steam and ash eruption follows local seismicity
A small steam and ash eruption 13-14 March was preceded by local seismic activity. Three high-frequency volcanic tremors were recorded on 9 March and one each on 10, 11, and 12 March by a PHIVOLCS seismograph 9 km from the vent. Sustained seismic activity started suddenly on 13 March at 1312, 4.5 hours before the onset of the eruption, and totaled 139 recorded events, 60 of which were high-frequency and 79 low-frequency types. At the beginning of the seismic crisis, only high-frequency tremors were recorded, then low-frequency types predominated between 1400 and 1600. The number of events per minute declined before the eruption began.
Mild ejection of steam with a minimal amount of ash started 13 March at 1745, producing a plume that reached 300-500 m height. At 1515 the next day, the summit was steaming voluminously, and the vapor column rose 500-700 m. On 15 March at 1700, "moderate" steaming was reported. The volcano was cloud-covered and only occasionally visible. During the eruption's first 24 hours (until 14 March at 1759) 51 high-frequency and 9 low-frequency tremors were recorded.
Information Contacts: PHIVOLCS, Quezon City.
Small ash eruption with seismicity
On 5 October a small eruption produced an 800-m eruptive cloud, depositing ash on four nearby villages. A strong booming sound was reported to have preceded the eruption and earthquakes were felt during the eruption. Activity had declined to voluminous emission of white vapor on 8 October and weakened further the next day, but seismographs continued to record low-frequency events. PHIVOLCS declared a 4-km-diameter danger zone two weeks before the eruption, and residents of the zone were ordered to evacuate when the eruption began.
Information Contacts: AFP.
Minor ash ejection
Without any preceding seismic activity, Canlaon weakly ejected ash on 3 June at 0139. Ash reached a height of ~ 300 m above the crater rim before drifting NE. The ejection was accompanied by audible rumbling and an explosion earthquake felt at intensity I, 5.5 km SE of the crater (at Barangay Pula). The event lasted 15 minutes, 45 seconds.
Another explosion earthquake, with 18 mm amplitude, occurred at 0435; it lasted 55 seconds. From 0436 to 0500 there was moderate to voluminous emission of dirty white steam, reaching a height of 300 m and drifting NW. Ash deposits were confined to 200 m from the crater on the SE and NE slopes.
Information Contacts: PHIVOLCS, Quezon City.
Renewed explosions and seismicity
Canlaon again erupted on 21 June, almost 19 days after the previous ash ejection. The event started at 1907 and was characterized by a cauliflower-shaped ash-steam cloud that rose to 4,000 m above the volcano's 2,465-m summit. The event was initiated by an explosion-type earthquake felt with intensities III and II at seismic stations 6 and 8.7 km from the summit respectively (Cabagnaan and Canlaon). Booming and hissing sounds accompanied the ash ejection. A strong sulfurous odor was detected at Canlaon station a few minutes after the event. Field investigation the next morning showed that light ashfall had occurred on several villages SE of the summit. The maximum thickness of the wet, rainsoaked ash deposit 4.5 km from the summit was 2 mm. The maximum volume of ejected material was 136,600 m3.
The eruption was anticipated because of the marked increase in steam volume 10 days prior to the eruption. The number of low-frequency volcanic earthquakes had remained at a high level after the ash ejection of 3 June and decreased slightly 9-13 June. Seismicity increased again on 14 June, 8 days earlier.
As of 1 July, seismicity and steaming had decreased slightly. PHIVOLCS noted that other ash ejections are still to be expected based on the eruptive patterns of 1969, 1978, and 1985. Furthermore, PHIVOLCS noted that the continued presence of low-frequency harmonic tremor, not recorded in the past at this volcano, heightens the possibility of magmatic eruption.
Information Contacts: R.S. Punongbayan, PHIVOLCS.
Ash eruption follows increased seismicity
Increased seismicity and thermal activity were followed by a small ash eruption.
On 30 March the number of volcanic earthquakes reached 9/day, an increase from the previous level of 1-3/day. Seismicity continued at moderate to low levels until 22 April when 74 low-frequency volcanic events were recorded and steam emission increased. Steam plume height increased to 150-200 m from a normal of 50-100 m, and 40-50% of the vent opening was filled with steam. PHIVOLCS officially informed the Secretary of Science, Department of Science and Technology that the condition of the volcano was unstable but since no harmonic tremor was being recorded, only a mild ash ejection was expected if activity increased.
On the morning of 24 April a fresh ash deposit ~1-2 km wide and 6.5 km long extended down the SW flank. No eruption signals were recorded by seismometers and no sounds were heard by nearby residents. A sulfur smell was reported from the Cabagnaan Observatory (approximately 6 km SW of the crater) on the same day.
Geochemical studies of the Mambucal aquapool, mudpool, and sulfur spring (9.5 km NNW of the summit) showed increasing sulfate and chloride concentrations starting 19 February.
Information Contacts: PHIVOLCS.
Sulfate increased in thermal area before ash eruption
The ash eruption that occurred 23 or 24 April was preceded by a steady increase in sulfate concentration in the Mambucal aquapool, mudpool, and sulfur spring. The increase began on 19 February when the average sulfate concentration rose from 40 ppm to 89-106 ppm in the aquapool, from 200-364 ppm to 490-708 ppm in the mudpool, and from 100-149 to 356-436 ppm in the sulfur spring (figure 1). Chloride concentration in the aquapool had ranged from 1,682-1,826 ppm but values began fluctuating between 1,870-2,130 ppm on 15 March. No corresponding change in chloride concentration was noted in the mudpool or sulfur spring. Thermal measurements in the Mambucal probe hole, aquapool, and sulfur spring yielded anomalous results but increases of 1.0°, 3.0°, and 5.0° C respectively (compared to the readings of the last quarter of 1986) were noted.
Figure 1. Sulfate concentration at Mambucal Aquapool, Mudpool, and Sulfur Spring, 9.75 km NNW of Canlaon's summit, 1 January-4 April 1987. Courtesy of PHIVOLCS. |
Geodetic measurements on 28-29 April revealed a slight inflation of 2.61 mm along a 400-m levelling line on the SE flank. Seismicity began increasing on 30 March 1987 and reached 74 low-frequency events on 22 April (see figure 2 and 12:4).
Figure 2. Number of low-frequency volcanic earthquakes at Canlaon, 1 January 1986-29 April 1987. Courtesy of PHIVOLCS. |
Further Reference. Bautista, L.P., 1987, Volcano Update - Canlaon Volcano; Phivolcs Observer, v. 3, no. 2, p. 5.
Information Contacts: PHIVOLCS.
Series of ash ejection
A series of ash ejections began on 21 June. During the initial outburst from 1725 to 1740, light-grayish steam clouds rose to a maximum height of 300 m above the crater. Traces of ash were noted at the village of Mananawin on the SE slope at 980 m elevation. This event was not recorded by the flank seismic network. Previous ash ejections in April 1987 were similarly not recorded (12:4-5).
Ash ejections ocurred again the next day at 1230 and 1418 and were recorded as small-amplitude (0.5 mm) harmonic tremors with durations not exceeding 2 minutes. The maximum ash cloud height was 600 m above the crater. Sulfur stench was noted by SE flank residents. On 24 June, ash ejections occurred at 1155 and 1455, accompanied by faint rumbling sounds. Ash from the 400-m-high eruption clouds was deposited on the upper SE slopes. No eruption signal was recorded by PHIVOLCS seismic stations.
Another ash ejection occurred at 1105 on 27 June, accompanied by an explosion-type earthquake that had a maximum double amplitude of 4.0 mm and lasted for 1 minute. As observed from the Canlaon Volcano Observatory (8.7 km SE of the crater), the cloud rose 500 m above the crater and deposited ash along the SW upper slopes. Background seismicity varied from 5 to 18 events/day following the first outburst. Steam emission between ash ejections covered 20-50% of the crater's area.
Since the ash eruption of April 1987, slight inflation of the SE flank and moderate seismicity have occurred (12:4-5).
Further Reference. Sincioco, J., 1988, The 1988 Eruptive Activity of Canlaon Volcano; Phivolcs Observer, v. 4, no. 3, p. 3.
Information Contacts: PHIVOLCS.
Mild ash ejections to 1,200 m
Since 25 October, mildly explosive ash ejections, to as much as 1,200 m above the summit, have occurred almost daily. As of 3 November, 29 voluminous gray plumes had deposited ash over the entire crater area and the upper SW and S slopes. No significant seismicity preceded emissions, which were accompanied by small-amplitude explosion earthquakes and tremor episodes. Iseismicity;explosion earthquake Total sulfate concentrations of hot springs NW of the crater have increased since March, from 90 to 135 ppm in the aquapool, 300 to 365 ppm in the mudpool, and 180 to 250 ppm in the sulfur spring.
Information Contacts: PHIVOLCS.
Ash ejections decline
Mild ash ejections occurred almost daily at Canlaon in the 5 weeks since eruptive activity began on 25 October at 1230. A total of 79 ash ejection episodes have been documented, the most recent on 1 December from 0515 to 0737. Plumes generally reached 200-1200 m above the summit (the highest on 3 November) and were dispersed as far as 8-10 km S. The ash plumes emitted during activity 15-17 November and 1 December covered ~80% of the crater area, compared to 100% for the larger eruptive episodes. Ground deformation measurements showed slight inflation of the edifice a few hours before ash ejections, most of which were accompanied by small-amplitude explosion earthquakes and short-duration harmonic tremor. Between eruptive episodes, moderate amounts of white steam covered ~20-40% of the crater, and seismic levels fell to 5-10 volcanic events/day. Activity remained weak and PHIVOLCS did not recommend evacuation.
As of 13 December, ash plume heights and steam volume had decreased, but not to pre-eruptive levels. Average plume dispersals had also decreased from 0.5-1 km to 50-100 m from the summit. PHIVOLCS noted that although activity appeared to be waning, the volcano's status remained abnormal.
Information Contacts: PHIVOLCS.
Small ash emission
Mild ash emission occurred from Canlaon on 8 January [1992] from 1405 to 1426. The light-gray ash clouds rose 600-800 m above the crater before drifting SW. Ashfall was confined to the upper flanks. During the ash emission, the seismograph at Canalon City Observatory recorded short-duration harmonic tremor with a maximum double amplitude of 10 mm, and 15 volcanic earthquakes. Seismic activity then gradually decreased; 8 volcanic earthquakes were recorded shortly after the eruption, but only two small volcanic events were detected between 1600 and 0600 the next morning. Steam emission also gradually decreased from voluminous (filling 80% of the crater) to moderate (40% of the crater filled). As of 12 January, activity was characterized by weak to moderate white vapor emission, with plume heights of 50->100 m and vapor filling 20-40% of the crater. Prevailing winds carried the plume SW and SSW.
Seismic activity had remained at background levels (<5 events/day) from 15 February 1991 through the day before the eruption, and pre-eruption steam emission varied from wispy to weak. Geologists believe that the eruption was triggered by ground water suddenly contacting hot rock beneath the summit crater.
A PHIVOLCS quick-response team left for Canlaon on 9 January. They issued no recommendation for evacuation, but advised residents of the area not to venture within the previously delineated danger zone (5 km radius) and to heed precautionary and safety measures.
Information Contacts: PHIVOLCS.
Small ash emission
Newspapers reported a 1-km-high ash emission and ashfall at flank towns on 10 June, coinciding with a minor earthquake. There were no reports of injuries.
Information Contacts: Reuters.
Phreatic explosions produce gray steam clouds that rise 800-1,000 m
People living in the vicinity of the volcano were advised to not enter the 4-km-radius permanent danger zone following a mild phreatic explosion at 0519 on 25 August that produced a voluminous gray steam cloud to 800 m height before drifting NNE. Steaming from the summit area increased following the explosion, and later that morning (0600-1045) a dirty white steam plume rose to heights that varied from 200 to 500 m. Moderate steam emission to 100-200 m was observed in the afternoon and evening. Radio reports stated that ash fell as far away as Panay Island, about 65 km W. Harmonic tremor was detected for 20 minutes during the eruption by a seismometer at Cabagnaan Station, 5.5 km SW of the summit, and an earthquake accompanied by rumbling sounds was felt at the station at 0526. The seismometer also recorded 21 low-frequency volcanic earthquakes within 3 hours after the explosion. Seismicity then rapidly declined, with only two high-frequency and three low-frequency events recorded from 1200 on 25 August through 0500 the next day. Seismicity prior to the explosion was at normal background levels of 0-2 events/day.
Canlaon had another mild phreatic explosion at 2329 on 3 September, which lasted for 8 minutes and produced a grayish steam-and-ash column that rose 1,000 m above the summit before drifting SSW and SSE. Traces of ash fell at the Canlaon Volcano Observatory, 8 km SSE of the summit. The phreatic explosion was accompanied by an earthquake felt at the Cabagnaan Station. Moderate-to-strong emission of dirty white steam was observed for 6 hours after the explosion; steaming activity then declined and the steam became white. Increased seismicity was noted during the explosion along with strong steaming, similar to previous phreatic activity at the volcano. Seismicity returned to background levels the next day. EDM surveys conducted after the 3 September event did not indicate significant inflation. Petrographic examination of the ash deposited by the 25 August and 3 September explosions indicated no juvenile component.
Information Contacts: R. Solidum, PHIVOLCS; AP.
Sudden phreatic explosion kills three people
On 10 August at 1431 an ash ejection killed three hikers and emitted a dirty-white steam-and-ash plume to 1,500 m above the central summit crater. The ash ejection lasted ~24 minutes, based on seismic records. A small associated explosion-type earthquake (22.8 mm of amplitude) was detected at the PHIVOLCS Cabagnaan seismic station, 5.5 km SW of the volcano. The ash drifted NE and was observed at altitudes of 7.6 and 11.3 km by Qantas aviators. The Bureau of Meteorology in Darwin issued a volcanic ash advisory describing the plume as extending 110 km SW. PHIVOLCS established a Level 1 alert (low level of hydrothermal disturbance, without any indication of magmatic activity), but no evacuation was advised. PHIVOLCS promptly warned the public to stay outside the 4-km-radius permanent-danger buffer zone. Based on previous Canlaon ash ejections, which were clustered in time, it was judged that there could be more explosions without any additional precursors. After the ash ejection, moderate emissions of white to dirty-white steam rose 100-150 m before drifting NE. On 11 August more white steam emissions were noted between 0353 and 0500. Another aviation notice reported the plume drifting SW.
The Cabagnaan seismograph recorded a total of 23 low-frequency volcanic earthquakes and four tectonic earthquakes from 0600 on 11 August through 0600 on 12 August. During 12 August, a quick response team from PHIVOLCS had installed four seismographs and was monitoring ground deformation. The team was also planning to determine the extent of the ash deposit.
According to 11 August news reports, two mountaineering groups were present on the summit at the moment of the explosion: a group of ten students from a Belgian University and their seven Filipino guides, and two British visitors accompanied by two local guides. Three people, one British and two Filipino, were killed. Seven Belgians and four Filipinos were evacuated or managed to make it off the mountain before darkness halted rescue efforts, but the other survivors were not rescued until the next morning.
Some of the 18 survivors were hospitalized because of injuries caused mainly by falling ejecta. Belgian Caroline Verlinde told reporters that she was descending from the crater rim when the eruption began without warning. She said she had seen a plume of smoke but her guide reassured her that it was normal. "Suddenly it spewed ash and stones. I hid behind a tree but my friends had nothing to protect them. I saw stones falling on them," she told the reporters.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, 5th & 6th Floors, Hizon building, 29 Quezon Avenue, Quezon City, Philippines; Bureau of Meteorology, Northern Territory Regional Office, P.O. Box 735, Darwin, NT 0801, Australia; Agence France Presse (AFP); Reuters Limited.
Earthquakes increase during early 2001 and begin to decrease 28 March
During January through March 2001, earthquake clusters were recorded by the seismic monitoring network around Canlaon. Similar activity occurred prior to the 10 August 1996 phreatic explosion from the active summit crater of the volcano (BGVN 21:07), leading the Philippine Institute of Volcanology and Seismology (PHIVOLCS) to believe that the earthquakes could signify a reactivation of the volcanic system at depth, a precursor to more vigorous activity such as ash explosions. On 21 March, a PHIVOLCS advisory of possible forthcoming activity recommended the immediate suspension of all treks to the summit crater. In addition, the 4-km-radius Permanent Danger Zone (PDZ) became off-limits at all times.
Beginning 28 March through at least 31 May, earthquakes averaged only about 1-2 events per day, a low level of seismicity. Accordingly, PHIVOLCS relaxed its no-entry advisory but urged visitors to avoid entering the crater because explosions could still occur without warning. For the same reason, the public was reminded that no permanent human activity is permitted within 4 km of the crater. No further reports were issued through at least October.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, 5th & 6th Floors, Hizon building, 29 Quezon Avenue, Quezon City, Philippines; Bureau of Meteorology, Northern Territory Regional Office, P.O. Box 40050, Casuarina, NT 0811, Australia.
Increased seismicity during January 2002 may be precursor to eruption
As of late May 2001, seismicity at Canlaon was low, and the Philippine Institute of Volcanology and Seismology (PHIVOLCS) relaxed its no-entry advisory into the crater (BGVN 26:10). No further reports were issued through 2001.
On 30 January 2002 PHIVOLCS reported that during the previous month, the seismic network around the volcano detected a higher number of earthquakes, observations that may indicate a reactivation of the volcano. Seismicity was dominated by high-frequency earthquakes located around the crater, from shallow depth to 8.5 km deep. These earthquakes may represent episodes of subsurface fracturing due to magma intrusion. During mid-January, PHIVOLCS further noted the occurrence of several low-frequency earthquakes, which supports the idea that some fluid migration, possibly magma ascent, was occurring. PHIVOLCS noted that if this idea was confirmed by forthcoming surveys, then the Alert Level may be raised.
Increased activity at Canlaon was recognized as early as January 2001 with occurrences of earthquake clusters. At the time PHIVOLCS issued a similar notice but activity quieted down. This year's reactivation seems more intense in terms of the number of earthquakes. They could foretell of impending phreatic eruptions. Several teams were sent to augment the Canlaon Volcano Observatory with additional seismometers and deployment of a GPS-based ground-deformation monitoring network. Because sudden phreatic or steam-driven explosions may occur at any time, PHIVOLCS urged the public to strictly observe the 4-km-radius Permanent Danger Zone (PDZ) around the volcano and recommended the suspension of all treks within this zone until further notice. As of 30 January, PHIVOLCS reported that volcanic activity did not require any kind of evacuation except for areas within the PDZ.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, 5th & 6th Floors, Hizon Building, 29 Quezon Avenue, Quezon City, Philippines.
Increased seismicity during March-April 2002
In February 2002, the Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported sustained seismic activity that might lead to an explosion at Canlaon. PHIVOLCS noted an increase in seismic activity in Canlaon after five weeks of continuous and sustained earthquakes. During 27-28 February the Guintubdan seismic station detected at least 67 earthquakes, which was above the background seismic level of a few earthquakes per day. PHIVOLCS monitored both high- and low-frequency volcanic earthquakes at Canlaon; high-frequency events dominated, indicating that the volcano was undergoing possible magma intrusion. PHIVOLCS noted that such intrusions result in many high-frequency events intermixed with a few low-frequency earthquakes. The epicenters were detected over a large area, which could mean that a large body of magma was developing beneath the volcano. At this stage of activity, a major eruption was not anticipated because the earthquakes could also have been caused by rockslides along the volcano's faults.
On 27 February trekking was banned within the 4-km danger zone after PHIVOLCS declared Alert Level 1 (the volcano is in a restive state, but trekking or any human activity could be dangerous within the danger zone). PHIVOLCS issued a statement that the area near the volcano should be avoided because of "possible sudden phreatic or steam-driven explosions." In the meantime, monitoring instruments were to be installed at the Guintubdan seismic station, located near the crater, to monitor the volcano's seismic activities.
On 15 April PHIVOLCS concluded that the episodes of apparent seismic unrest at Canlaon could be traced to the Guintubdan and Mambucal areas. The Guintubdan area has been the site of earthquake swarms in the past, and these high-frequency events may be related to local fault movement and/or intrusions. On the other hand, earthquakes in the Mambucal area occurred when the Philippine National Oil Company (PNOC) pumped water into its geothermal wells and induced micro-earthquake fracturing at depth. In both instances, PHIVOLCS noted that significant earthquakes only occurred over a broad area N of the active crater of Canlaon, without distinct clustering or migration towards the crater. These observations suggest that earthquake activity, for now, is not related to a reactivation of the Canlaon magma system. With the return of seismic activity to baseline levels and having identified non-volcanic seismic sources in this area, PHIVOLCS lowered the alert status of Canlaon from Alert Level 1 to Alert level 0. However, visitors to the summit area were strongly urged to avoid entering the crater because sudden explosions may occur without warning. For the same reason, PHIVOLCS reminded the public that no permanent human activity is permitted within 4 km of the crater.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, 5th & 6th Floors, Hizon building, 29 Quezon Avenue, Quezon City, Philippines.
Steam emission in June 2002; ash emissions in November 2002 and March 2003
The Philippine Institute for Volcanology and Seismology (PHIVOLCS) reported a sudden increase in steaming activity at Canlaon (also spelled Kanlaon) on 28 June 2002. At about 0436, "dirty white steam" was observed rising up to 200 m above the active crater and drifting SW and SSW. However, there was no corresponding significant earthquake activity; the seismic network detected only two high-frequency volcanic earthquakes in the 24-hour window around the event. A small ash puff on 28 November 2002 at 0721 rose ~100 m above the active crater and drifted SW. The event was recorded as a volcanic tremor at the Cabagnaan and Guintubdan seismic stations. Traces of ash deposits were observed at Cabagnaan Station, located SSW of the active crater. Moderate emission of white to dirty white steam was observed immediately after the ash puff. As of 1100 on 28 November, activity had decreased to only minor white steaming from the summit with a few discrete tremors.
A PHIVOLCS report on 17 March indicated that the hazard status of Canlaon had been raised to Alert Level 1 following an ash emission on that day and one the previous week. At about 0530 on 17 March observatory personnel noted the emission of a grayish volcanic plume. The dirty white steam clouds rose 50 m above the active crater and drifted SW and SSW. No corresponding significant earthquake activity accompanied the event; the seismic network detected only two small low-frequency volcanic earthquakes in the preceding 24 hours. PHIVOLCS interpreted the activity as being hydrothermal in nature at shallow levels in the crater, with no indication of active magma intrusion. Details of the ash emission that occurred "last week" were not provided.
Alert Level 1 signifies that there could be possible ash explosions in the coming days or weeks. For this reason, PHIVOLCS reiterated that the public should avoid entering the 4-km-radius Permanent Danger Zone.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, University of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs. dost.gov.ph/).
Ash-and-steam explosions between 23 May and 4 July; minor ashfall on 8 June
Following an ash emission from Canlaon on 17 March 2003 (BGVN 28:03), the Philippine Institute of Volcanology and Seismology (PHIVOLCS) raised the hazard status to Alert Level 1 (on a scale of 0-5), which signified possible ash explosions in the coming days or weeks. There was another ash emission on 23 May.
Beginning on 1 June, the seismic network detected an average of five low-frequency volcanic earthquakes per day. Moderate steaming was noted, which is unusual for Canlaon because steam is typically wispy or nonexistent during normal and quiet conditions.
Brief bursts of ash and steam reaching 100 m above the active crater were observed on 1, 3, 4, 5, 6, 7, and 8 June. An ash emission during 0645-0700 on 8 June deposited traces of ash at Canlaon City proper and in the barangays of Masulog and Linutangan. Eight low-frequency volcanic earthquakes and four low-frequency short-duration harmonic tremors were recorded in the 24-hour period prior to the event. In addition, PHIVOLCS seismographs in Cabagnaan (6 km SW of the active crater) and Canlaon City (8.7 km SE) detected episodes of low-frequency tremor.
Small ash ejections continued after 8 June. Ash-and-steam columns rose to 1,000 m before drifting SSE and SE. Ash explosions on 13 June between 0647 and 0756 were recorded at Cabagnaan as low-frequency short-duration harmonic tremors. The explosions produced voluminous dirty-white steam which rose to ~500 m and drifted SSE and ESE. Six low-frequency volcanic earthquakes and three low-frequency short-duration harmonic tremors were detected the 24 hours prior to the event.
Two small steam-driven explosions occurred during 0820-0835 and 1020-1030 on 17 June. The ejected ash-and-steam columns rose to ~400 m above the summit crater and drifted NNE. In the 24-hour period prior to the explosions, the volcano's seismic network detected eight low-frequency volcanic earthquakes, two high-frequency volcanic earthquakes, and one low-frequency short-duration harmonic tremor.
A mild ash ejection at 1422 on 18 June was recorded as a low-frequency volcanic earthquake. A grayish ash-and-steam cloud rose ~ 400 m above the summit crater before drifting SE. Only two low-frequency volcanic earthquakes and one short-duration harmonic tremor preceded the explosion. Mild ash explosions occurred during 0701-0707, 0743-0750, and 1420-1430. These explosions produced voluminous ash-and-steam clouds that rose 400 m above the summit crater before drifting NW. The events were reflected in seismic records as low-frequency volcanic earthquakes. In the 24-hour period prior to the events, two low-frequency earthquakes, one high-frequency volcanic earthquake, and one short-duration harmonic tremor were recorded by the seismic network.
The volcano continued to manifest moderate steaming and ash emission activity with an ash column rising ~900 m above the summit crater at 0515 on 4 July. In the 24-hour period prior to the event the seismic network recorded five low-frequency volcanic earthquakes and two low-frequency short-duration harmonic tremors.
The hazard status during June and July remained at Alert Level 1, and PHIVOLCS reminded the public to avoid entering the 4-km-radius Permanent Danger Zone. The absence of longer duration harmonic tremor suggested to PHIVOLCS that there was no magma movement or intrusion, indicating that the explosions were possibly a result of reactivation of a shallow hydrothermal system.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, University of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs. dost.gov.ph/).
1-km-high plume of ash-laden steam on 10-11 July 2003
Ash ejections were reported at Canlaon (also spelled Kanlaon) on 10 and 11 July 2003. At 1735 on 10 July a column of ash-laden steam, described as a moderate to strong dirty white color, was seen rising from the volcano to a height of 1 km by observers in Kanlaon City. The cloud drifted to the NW, SW, and NE, with an area within a 4-km radius from the crater affected by ashfall. The explosion registered as a low-frequency volcanic earthquake. Prior to this activity, two low-frequency volcanic earthquakes and two low-frequency short-duration harmonic tremors were recorded by the seismograph at Kanlaon Volcano Station. The phreatic activity continued as of 2000 that night.
Two ash ejections were reported on 11 July, from 0620 to 0624 and 0658 to 0705. Dirty white steam rose up to 1.3 km above the crater and drifted to the SW. The seismic network recorded six low-frequency volcanic earthquakes and three low-frequency short-duration harmonic tremors.
The alert status remained at Level 1 and PHIVOLCS reiterated its warning to the public not to venture within the 4 km radius Permanent Danger Zone.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, Univ. of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/).
Frequent ash explosions from 7 March until 23 July 2003
A report on 19 September 2003 from the Philippine Institute of Volcanology and Seismology (PHIVOLCS) summarized activity at Canlaon from 7 March to 23 July 2003. This included the ash ejections of 10 and 11 July (BGVN 28:07). There were 46 ash explosions recorded since March, characterized by emission of steam clouds with small amounts of ash rising 100-1,500 m above the active crater. Prevailing winds dispersed the ash mainly SW and SE, which settled predominantly over the mid-upper slopes of the volcano.
Seismic activity remained elevated through this period, with epicenters of some high-frequency events located near the active crater, focal depths ranged from near-surface down to 18 km. From June to July, the numbers of recorded low-frequency volcanic earthquakes and low-frequency short-duration harmonic tremor events increased. This coincided with phreatic episodes between 8 June and 23 July 2003.
On 23 July an ash explosion was observed from Kanlaon Volcano Observatory, 8.5 km ESE of the crater. Ash-laden steam clouds were ejected to heights of ~800 m above the active crater. After 23 July only weak steam emission was noted, and seismic activity returned to low levels.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, Univ. of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/).
Alert level lowered after seismic decrease; January 2005 phreatic ash emission
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) noted in a March 2004 report that the most recent eruptive episode of Canlaon had begun on 7 March 2003. Their 2003 Annual Report described a mild ash-and-steam emission on 7 March that rose 1 km above the summit and resulted in traces of ash deposited at Cabagnaan, 5.5 km S. On 17 March 2003 the hazard status had been raised to Alert Level 1 (BGVN 28:03, 28:06, 28:07, and 28:08). A total of 46 minor ash ejections were documented or observed, most from June to July 2003, characterized by steam clouds with minor ash that rose as high as 1,500 m. Prevailing winds dispersed the ash over the mid-upper slopes in the SW and SE sectors of the volcano.
Sporadic recordings of high-frequency volcanic earthquakes (HFVQ) and low-frequency volcanic earthquake swarms (LFVQ) starting in January 2003 prompted PHIVOLCS to issue a warning on the possibility of sudden phreatic explosions. In June 2003 daily occurrences of LFVQs increased dramatically and these heightened levels were sustained until July 2003. Low-frequency short-duration harmonic tremors (SDHLF) also appeared in June 2003 and increased like the LFVQs, indicating a continuous supply and transport of volcanic fluids towards the shallow levels of the crater area.
A general trend towards volcanic quiet was recognized during August 2003, but the status was maintained at Alert Level 1 because HFVQs, LFVQs, and SDHLFs persisted, though in diminishing numbers, until September 2003. After that time, steam emissions from the summit crater were only weak or absent, with normal levels of seismic activity. On 1 March 2004 PHIVOLCS lowered the hazard status to Alert Level 0, meaning the volcano has returned to a quiet state. The public was strongly advised, however, to consider the risk when entering the 4-km Permanent Danger Zone because sudden phreatic explosions may occur without warning. People planning to climb the volcano are advised to check with an observatory first.
Phreatic emission, January 2005. The value of continued warnings was shown on 21 January 2005, when Canlaon generated a sudden brief ash emission. The PHIVOLCS observatory at La Carlota City College reported moderate emission of a grayish volcanic plume at about 0930 that rose to ~ 500 m above the active crater and drifted WNW and SW, depositing light ash on the upper SW slopes. Traces of ash deposits were also observed at Cabagnaan, 5.5 km SW of the active crater. No coincident volcanic earthquakes were recorded, and Canlaon continued to be seismically quiet. These observations suggest the activity is hydrothermal in nature and occurring at very shallow levels near the crater floor.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, Univ. of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/).
Frequent ash emissions in March and April 2005; access remains restricted
Ash emissions and sporadic seismicity at Canlaon between March 2003 and March 2004 were reported in BGVN 29:12. A brief ash emission began at Canlaon around 0930 on 21 January 2005. The eruption cloud rose ~ 500 m above the active crater and drifted WNW and SW. No coincident volcanic earthquakes were recorded. Fine ash was deposited in the city of Cabagnaan, ~ 5.5 km SW of the crater. The Philippine Institute of Volcanology and Seismology (PHIVOLCS) advised the public to avoid entering the 4-km-radius Permanent Danger Zone around Canlaon.
Ash emissions began again on 20 March around 1300. Small amounts of ash fell in the town of Guintubdan 5 km W of the volcano. During 24 March to 4 April, sporadic ash emissions rose to a maximum of 1 km above the volcano. During this time ash fell in the towns of La Castellana (16 km SW of the crater), Upper Sag-ang, Yubo (5-6 km SW), and Guintubdan (5-6 km WNW). Due to this unrest, PHIVOLCS raised the Alert Level from 0 to 1 (on a scale of 0-5) on 30 March. According to a news article, pilots were advised to avoid flying near Canlaon.
On March 22 the Provincial Disaster Management Team (PDMT) warned it would apprehend trekkers and faith healers who ventured to Mount Canlaon during Holy Week. Trekking to Mount Canlaon has become a practice by some faith healers and mountaineers who believe that the volcano is a source of supernatural powers.
On 31 March at 0601 and 1715, two mild ash ejections reached heights of about 200-300 m above the summit before drifting NW and SW. Ash was deposited at Guintubdan, Upper Sag-ang, and Upper Mansalanao. A low-energy ash emission on 7 April at 1429 generated a cloud which rose to a height of ~ 100 m above the crater and drifted SW. According to PHIVOLCS, the seismic monitoring network around the volcano did not record any earthquakes during this event. During 13-14 April, mild ash emissions produced plumes to a height of ~ 700 m above the crater. During 15-17 April, moderate-to-strong emissions produced ash plumes to ~ 2 km above the crater and deposited ash in villages as far as La Castellana. None of these ash emissions was associated with seismicity, indicating that the activity is likely hydrothermal in nature, and taking place at shallow levels in the crater.
Throughout this period Canlaon remained at Alert Level 1. As of the end of April 2005, the 4-km-radius Permanent Danger Zone (PDZ) was restricted and all treks to the summit remained suspended.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, Univ. of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/); Chris Newhall, USGS, Box 351310, University of Washington, Seattle, WA 98195-1310, USA; Philippine Star (URL: http://www.philstar.com/).
May 2005 ash ejections ceasing after the 25th as monitored parameters declined
Throughout May 2005, PHIVOLCS noted that ash-and-steam emissions from Canlaon produced plumes to 500-1,000 m above the volcano. The hazard status remained at Alert Level 1. The SO2 flux remained above the 'normal' level of 500 metric tons/day (t/d) with values of 2,700 t/d on 1 May, 2,080 on 22 May, and 1,400 on 26 May. According to news reports, flights to and from nearby Kalibo airport were suspended on 3 May due to reduced visibility.
Although voluminous white steam continued to be discharged from the active vent early in June 2005, after 25 May ash ejections stopped and ash contents in the steam plume were significantly reduced. On [30 June] PHIVOLCS lowered the hazard status of Canlaon from Alert Level 1 to Alert Level Zero, listing a variety of reasons. For one, they noted the downtrend in the SO2 gas emission rate from a high of about 4,900 t/d, to the prevailing level of 1,500 t/d. For another, they noted the absence of significant seismic activity before, during, and after the ash emissions. And finally, they cited a lack of significant observations indicating near-surface hydrothermal activity. Since Canlaon has a history of sudden outbursts, the public was reminded to refrain from entering the 4-km-radius Permanent Danger Zone (PDZ) and to coordinate with PHIVOLCS and Disaster Management Councils in any attempt to climb the volcano.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, Univ. of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/); Chris Newhall, USGS, Box 351310, University of Washington, Seattle, WA 98195-1310, USA; Philippine Star (URL: http://www.philstar.com/).
Steam-and-ash explosions in June and July 2006
After a year of quiet following ash ejections from Canlaon in May 2005 (BGVN 30:06), the Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported that a new period of activity began on 3 June 2006. In total, twenty-three ash ejections occurred between 3 June and 25 July 2006. These outbursts were all water-driven in nature, characterized by emission of ash and steam that rose up to 2 km above the active crater. The prevailing winds dispersed ash in all directions. The seismic network, however, did not detect significant seismic activity before or after the ash emissions, supporting the idea that the explosions were very near-surface hydrothermal events.
Four explosive episodes that occurred over the days 3, 10, and 12 June ejected mainly steam with some ash, and affected only the summit crater and upper SW slopes. The event at 1430 on 3 June sent dirty white to grayish steam 800 m above the summit. The activity was observed until 1445 when thick clouds covered the summit. Another emission started at 2316 on 10 June and lasted until 0030 the next morning. The plume was estimated to attain heights of 700-1,000 m before drifting SW. After the ash emission, moderate to wispy steam plumes escaped, to maximum heights of 600 m above the summit. Another steam-and-ash episode during 0515-0535 on 12 June caused a plume to rise about 600 m before drifting SW. After the ash emission, generally weak to moderate steaming to a height of ~ 400 m returned. Plumes rose 600-1,000 m and drifted SW; ashfall was confined to the upper slopes. This new period of low-level unrest prompted PHIVOLCS to raise the hazard status to Alert Level 1 on 12 June, suspending all visits to within 4 km of the summit.
Three small steam-and-ash emissions without recorded seismicity occurred again between the afternoon of 13 June and the morning of the 14th. The grayish steam clouds rose ~ 900 m above the active crater and drifted NE and NW. Only traces of ash were observed over the N upper slope. An explosion from 0845 to 0924 on 14 June produced an ash and steam cloud, which rose up to 1.5 km above the summit and drifted N, affecting mainly the upper slopes. Voluminous grayish steam plumes were then seen rising up to 1.5 km above the summit crater after 1640 through the next morning. The seismic network detected only two low-frequency volcanic earthquakes. Kanlaon City proper experienced light ashfall starting at 1630 on 15 June after voluminous dirty white steam was observed rising 1.5-2 km above the summit crater a few hours earlier (from 1346 to 1520). As of 1800, ashfall was still wafting through the city.
The character of this episode changed on the afternoon of 19 June when two episodes of steam-and-ash emission sent clouds 600 m above the crater that drifted SW. Weak to moderate steaming was observed after the second explosion and during the morning observation on the 20th. The initial explosion was recorded by the Cabagnaan station's seismograph as low-frequency tremor with a duration of 13 minutes. One minute of tremor was recorded at the time of the second explosion. No precursor seismicity was detected. Traces of ashfall and sulfurous odors were reported at Barangay Cabagnaan proper in La Castellana. During the 24 hours before 0730 on 20 June, the seismic network detected two cases of low-frequency tremor and three small low-frequency volcanic earthquakes.
An additional six short steam-and-ash emissions took place during 21-25 June. The explosions produced grayish columns that rose 800-1,500 m above the crater and drifted NW, SW, and SSW. Volcanic seismicity was not associated with these events except for a single harmonic tremor before the emission on 25 June. Light ashfall was reported at Upper Cabagnaan in La Castellana. Weak to moderate steaming was observed after the explosions.
Steam-and-ash emissions were not reported again until the afternoon of 2 July. The grayish steam clouds then rose to heights of up to 1,000 m above the active crater and generally drifted NW. Another episode on the morning of 3 July produced a column to a height of 500 m above the crater. The seismograph at Cabagnaan recorded ten volcanic earthquakes while the seismograph at Sto. Bama near Guintubdan in La Carlota City recorded eight local seismic events during the 24 hour observation period that included these emissions.
An explosion-type earthquake with a 10 min, 25 sec duration was recorded at 0426 on 23 July, but cloud cover prevented observations. Traces of ash fell up to about 9 km ENE from the crater, affecting Barangays Pula, Malaiba, and Lumapao. When clouds cleared during 0630-0800 on 25 July, ash-laden steam clouds were seen rising up to 300 m above the crater drifting ENE and SE. Light ashfall was experienced at Gabok, Malaiba, and Lumapao of Kanlaon City, about 9 km from the crater. This emission was not reflected on the seismic record as only two small volcanic earthquakes were detected during the preceding 24 hours. Dirty white steam was observed on the morning of the 26th rising to a maximum of 100 m above the crater.
Explosions ceased after 25 July, and other activity, such as weak steaming and minor seismicity, showed a general trend towards quiescence. After three months with no further explosive emissions, on 2 November 2006 PHIVOLCS lowered the hazard status from Alert Level 1 to Alert Level 0, meaning the volcano has returned to normal conditions.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, Univ. of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/).
Sporadic ash explosions during November-December 2015 and March 2016
According to the Philippine Institute of Volcanology and Seismology (PHIVOLCS), after an ash explosion at Kanlaon on 23 July 2006 and a series of earthquakes the day after (BGVN 32:02), activity subsided. Only non-eruptive activity was reported between the 2006 explosion and 24 November 2015, when ash emission began following strong seismicity and steam explosions the day before; intermittent ash emissions continued through 30 December. Activity resumed briefly with explosions and ash plumes during 29-31 March 2016.
Reports during 2008-2010. During 26 July-2 November 2006, no ash explosions occurred, and both steam emissions and seismicity were low, prompting PHIVOLCS to lower the Alert Level from 1 to 0 (out of 5).
PHIVOLCS reported that during 7-10 February 2008, the seismic network detected a significant rise in earthquakes, prompting them to raise the Alert Level from 0 to 1 on 10 February. Cloud cover prohibited visual observations of the summit. According to a news account (Sun Star News), seismic activity returned to background levels during 5 March-25 April (0-3 earthquakes/day), persuading PHIVOLCS to lower the Alert Level to 0 on 25 April 2008.
During 23 August-1 September 2009 the PHIVOLCS seismic network detected a significant rise in the number of earthquakes. A few of the earthquakes were felt as far away as Bago City, 30 km NW. The epicenters clustered on the NW flank.
Based on a pilot observation, the Tokyo Volcanic Ash Advisory Center (VAAC) reported that on 15 May 2010 an ash plume rose to an altitude of 2.4 km and drifted W. Ash was not identified in satellite imagery. PHIVOLCS later confirmed that the plume originated from a fire and not an eruption. No further reports were issue by PHIVOLCS until November 2015.
Activity during November-December 2015. At 0930 on 23 November 2015 the seismic network detected an explosion-type signal, culminating with an 8-minute-long steam explosion. Observers reported that a white plume rose 1-1.5 km above the crater and drifted SW, and rumbling was heard in local areas. Only four volcanic earthquakes had been recorded during the previous week, but after the explosion, the network detected volcanic tremor that lasted for five hours. The Alert Level was raised to 1. Continuous steam emissions with minor ash content were observed the next morning. During 24-25 November, the seismic network detected 11 volcanic earthquakes; on 25 November, gas-and-ash emissions rose 150 m above the crater and drifted SW.
According to PHIVOLCS, two volcanic earthquakes accompanied by a one-minute, low-energy, gray ash emission occurred at 0513 on 11 December 2015. Observers also noted ash emissions at 0951, 1008, 1140, and 0101 on 13 December that rose 200-300 m and drifted SW. The emissions were not detected by the seismic network, indicating a shallow source. Trace amounts of ashfall were reported in nearby communities on the W and SW flanks. At 2138 on 15 December a low-frequency earthquake lasted 45-47 seconds. Inclement weather prevented visual observations of the crater. Rumbling was heard in neighborhoods on the SE flank. On 17 December white steam plumes rose 50 m above the crater. Poor weather conditions prevented further views of the crater through 22 December.
PHIVOLCS reported that at 1457 on 23 December 2015, the seismic network detected an explosion. The event was not visually observed due to dense weather clouds around the summit area, but rumbling was heard in nearby barangays (villages) including Cabagnaan, La Castellana (16 km SW), and Ara-al and Yubo, La Carlota City (14 km W). Minor amounts of ash fell in Ara-al, Haguimit, and La Granja, La Carlota City, and a sulfur odor was noted in barangay Tres Elis, La Castellana. Another explosive event was detected at 2109 on 24 December, but was again not visually observed. Trace amounts of ash fell in Ara-al, Haguimit, and La Granja, and a sulfur odor was reported in Tres Elis. On 26 December, white steam plumes rose 100 m above the crater and drifted SW. A five-minute long ash event that began at 1329 on 27 December was accompanied by rumbling heard in a few local barangays. An eruption plume, viewed from the SE flank, rose 1 km above the crater, and may have risen as high as 4.5 km based on pilot observations. Minor ashfall was noted in nearby communities as far as 58 km WNW. About 1230 on 30 December, a low-energy explosion produced an ash plume that rose 100 m above the crater and slowly drifted SW.
Activity during March-April 2016. According to PHIVOLCS, at 1820 on 29 March 2016, the seismic network detected a 12-minute explosion that was accompanied by a booming sound heard in nearby communities. Observers to the SE reported an ash plume that rose 1.5 km above the crater, and minor amounts of ash fell in areas downwind. Incandescent ejecta caused a small fire on the upper flank. A 25-second-long explosion was detected at 1918. On 30 March at 0130, a long-duration tremor began that was accompanied by gas-and-steam plumes that rose 600-700 m and drifted SW and SSW. On 31 March 2016, minor ashfall was reported in areas downwind, including in parts of La Carlota City (14 km W), La Castellana, and Bago City in Negros Occidental. The tremor continued during 2-4 April, though the energy decreased, and steam plumes rose 400-500 m. On 5 April steam plumes rose 800 m and drifted SW. The Alert Level remained at 1.
According to a 30 March 2016 news account (The Manila Times), PHIVOLCS said that GPS monitoring had detected slight inflation between December 2015 and 14 March 2016
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, Univ. of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/); Tokyo Volcanic Ash Advisory Center (VAAC), Tokyo, Japan (URL: http://ds.data.jma.go.jp/svd/vaac/data/); Sun Star News (URL: http://www.sunstar.com.ph/); The Manila Times (URL: http://www.manilatimes.net/).
Three ash explosions on 18 June 2016; steam plumes through July
An ash explosion from Kanlaon on 24 November 2015 was the start of activity that included intermittent ash emissions through December and during 29-31 March 2016 (BGVN: 4014). That activity was followed by decreasing tremor and steam plumes rising to as high as 800 during the first days of April 2016. A short series of explosions on 18 June 2016 were the last ash emissions through 2016, based on Philippine Institute of Volcanology and Seismology (PHIVOLCS) reports. The Alert Level remained at 1 (on a scale of 0-5) throughout the reporting period, indicating low level of volcanic unrest.
PHIVOLCS reported that ground deformation measurements from continuous GPS data as of 2 June 2016 indicated slight inflation of the edifice since December 2015. Weak to moderate emission of white steam plumes that rose 540 m during 15-17 June and drifted SW and NW.
A series of three eruptive events occurred on 18 June, beginning at 0919 and lasting 27 minutes. These events were recorded by the seismic monitoring network as consecutive explosion-type earthquakes that lasted 30, 42, and 29 seconds, respectively. The first event, a steam-and-gas explosion, generated a light gray-to-white ash plume that initially rose 1.5 km above the crater and then later to 3 km (figure 3). The second event, an ash eruption immediately following the first event, produced a dense black ash plume that rose 500 m. Lastly, a grayish ash plume rose 500 m. Minor ashfall was reported to the W in the barangays of Ara-al, San Miguel, and Yubo in La Carlota City (14 km W), Sag-ang in La Castellana (16 km SW), and Ilijan in Bago City (30 km NW). A diffuse sulfur odor was detected in Ara-al.
Figure 3. Photo sequence showing eruption plumes from Kanlaon at 0919 on 18 June 2016. Courtesy PHIVOLCS. |
PHIVOLCS reported that during 20, 22-23, and 25-26 June white steam plumes rose as high as 800 m and drifted WNW, NW and SW; wispy steam plumes were observed on 27 June. Starting at 1640 on 23 June the seismic network recorded a 4-minute-long, explosion-type signal; weather clouds prevented visual observations of the summit area.
White plumes were again seen during 20-25 July. On 20 July plumes were a dirty-white color; on 21-22 they were of white steam; and on 25 July they rose 200 m and drifted NW and SW. Sulfur dioxide (SO2) emitted at the active vent averaged 234 tonnes/day on 21 July.
Ground deformation data from continuous GPS measurements as of 3 September 2016 indicated no significant change of the edifice since August 2016.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, PHIVOLCS Building, C.P. Garcia Avenue, Univ. of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/).
Phreatic explosions on 9 December 2017 with ashfall and high seismicity
A series of three explosions at Kanlaon on 18 June 2016 sent ash plumes as high as 3 km above the crater and caused minor ashfall in neighborhoods W, SW, and NW of the volcano (BGVN 42:01). This was followed by steam plumes through 25 July 2016. The active Lugud crater (figure 4) has been the source of 21 reported eruptions since 1969; the latest eruption took place in December 2017. Information summarized here for activity from September 2016 through December 2017 was provided by the Philippine Institute of Volcanology and Seismology (PHIVOLCS).
PHIVOLCS reported on 5 May 2017 that since the last phreatic eruption in June 2016 there had been a general decline in activity: seismicity was at baseline levels, no significant deformation had been detected since August 2016, sulfur dioxide emissions were low, and no steaming had been observed since 29 September 2016. The Alert Level was lowered to 0 (on a scale of 0-5), though the public was warned to not enter the 4-km-radius Permanent Danger Zone (PDZ).
Between 24 June and 18 August 2017 the seismic network detected 244 volcanic earthquakes. The PHIVOLCS report noted that the increased seismic activity could be followed by phreatic explosions at the summit crater, despite the absence of visible degassing or steaming from the active vent. The Alert Level was raised to 1. The number of daily volcanic earthquakes increased after 18 August. In their 15 November report, PHIVOLCS indicated that during the previous 24 hours there had been 279 deep volcanic earthquakes recorded (compared to five the day before). This prompted them to raise the Alert Level to 2 (moderate level of unrest), where it remained for the rest of the year. The next day, the number recorded was 217. After that the daily number of volcanic events dropped considerably, especially after 21 November. Based on PHIVOLCS reports, the number of daily volcanic earthquakes during the first eight days of December 2017 varied from one to seven.
On 9 December an approximately 10-minute-long, low-energy phreatic explosion began at 0947 that was heard as far away as La Castellana, Negros Occidental (15 km SW). A plume of voluminous steam and dark ash rose 3-4 km above the summit vent (figure 5), and minor amounts of ash fell in Sitio Guintubdan (23 km W), and barangays W of the volcano (Ara-al, Sag-ang, and Ilihan). The eruption was preceded by the resumption of degassing at the summit crater at 0634, detectable as continuous low-energy tremor during periods when the summit was not visible; degassing was last observed September 2016.
Only three volcanic earthquakes were detected on 10 December, but then the number increased to 155 the next day. The number of daily events earthquakes increased again to 578 on 13 December, rose to 1,007 the next day, and peaked at 1,217 on the 15 December. The earthquake count dropped to 149 on 16 December before returning to six or fewer through 19 December. White steam plumes rose 800 and 300 m above the crater on 13 and 14 December, respectively. White plumes were diffuse on 15 December; weather clouds prevented views of the summit area during 16-18 December. Sulfur dioxide emissions were 603-687 tons per day during 13-14 December.
PHIVOLCS reported that during 19-20 December there were 412 volcanic earthquakes. A low-energy, explosion-type earthquake was detected at 0233 on 21 December associated with gas emissions from the summit area. Later in the day steam plumes rose 400 m and drifted NE. The number of daily volcanic earthquakes increased to 957 the next day and then decreased to less than 20 per day during 22-23 December. The daily earthquake count increased to 382 and 776 events on 24 and 25 December, respectively, decreased to 82 on 26 December, and the dropped to three or fewer over the last days of the year. Weather clouds often prevented observations , but white plumes rose 300 m and drifted NE, NW, and SW on 21 December, and 700 m on 26 December. A steam plume on 30 December was seen rising 500 m above the crater rim and drifting SW. On 30 December 2017, sulfur dioxide levels were measured at an average of 1,946 tonnes/day.
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS), Department of Science and Technology, University of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost.gov.ph/); Billy Lopue, flickr (URL: https://www.flickr.com/photos/21905294@N03/).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
Synonyms |
||||
Canlaon | Canalaon | Malaspina | Malespina | ||||
Craters |
||||
Feature Name | Feature Type | Elevation | Latitude | Longitude |
Lugad | Crater | |||
Southern Crater | Crater | |||
Thermal |
||||
Feature Name | Feature Type | Elevation | Latitude | Longitude |
Carabao Killer | Thermal | |||
Chicken Killer | Thermal | |||
Hog Killer | Thermal |
|
|
There is data available for 30 confirmed Holocene eruptive periods.
2024 Jun 3 - 2024 Jun 3 Confirmed Eruption VEI: 3
Episode 1 | Eruption | ||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2024 Jun 3 - 2024 Jun 3 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||||||||||||
At 1851 on 3 June an explosive eruption ejected incandescent material and produced a voluminous ash plume that rapidly rose 5 km above the vent and drifted W. Pyroclastic density currents generated from column collapses traveled 2-3 km down the S and SE flanks. | ||||||||||||||||||||||||||||||||||||||||
List of 6 Events for Episode 1
|
2017 Dec 9 - 2017 Dec 9 Confirmed Eruption VEI: 2
Episode 1 | Eruption | Lugud crater | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2017 Dec 9 - 2017 Dec 9 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
List of 13 Events for Episode 1 at Lugud crater
|
2015 Nov 24 - 2016 Jun 18 Confirmed Eruption VEI: 2
Episode 1 | Eruption | Lugud crater | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2015 Nov 24 - 2015 Dec 30 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
List of 23 Events for Episode 1 at Lugud crater
|
Episode 2 | Eruption | Lugud crater | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2016 Mar 29 - 2016 Mar 31 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
List of 10 Events for Episode 2 at Lugud crater
|
Episode 3 | Eruption | Lugud crater | ||||||||||||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2016 Jun 18 - 2016 Jun 18 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||||||||||||||||||||||
List of 9 Events for Episode 3 at Lugud crater
|
2006 Jun 3 - 2006 Jul 25 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2006 Jun 3 - 2006 Jul 25 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1
|
2005 Jan 25 - 2005 May 25 Confirmed Eruption VEI: 2
Episode 1 | Eruption | ||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2005 Jan 25 - 2005 May 25 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||
List of 4 Events for Episode 1
|
2003 Mar 7 - 2003 Jul 23 Confirmed Eruption VEI: 1
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2003 Mar 7 - 2003 Jul 23 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1
|
2002 Nov 28 - 2002 Nov 28 Confirmed Eruption VEI: 1
Episode 1 | Eruption | ||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2002 Nov 28 - 2002 Nov 28 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||
List of 4 Events for Episode 1
|
1996 Aug 10 - 1996 Aug 10 Confirmed Eruption VEI: 2
Episode 1 | Eruption | ||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1996 Aug 10 - 1996 Aug 10 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||||||||||||
List of 6 Events for Episode 1
|
1993 Aug 25 - 1993 Sep 3 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1993 Aug 25 - 1993 Sep 3 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1
|
1992 Jun 10 - 1992 Jun 10 Confirmed Eruption VEI: 2
Episode 1 | Eruption | ||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1992 Jun 10 - 1992 Jun 10 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||
List of 4 Events for Episode 1
|
1992 Jan 8 - 1992 Jan 8 Confirmed Eruption VEI: 1
Episode 1 | Eruption | ||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1992 Jan 8 - 1992 Jan 8 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||
List of 4 Events for Episode 1
|
1991 Feb 14 - 1991 Feb 14 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1991 Feb 14 - 1991 Feb 14 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1
|
1989 Oct 25 - 1989 Dec 13 (in or after) Confirmed Eruption VEI: 2
Episode 1 | Eruption | ||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1989 Oct 25 - 1989 Dec 13 (in or after) | Evidence from Observations: Reported | |||||||||||||||||||||||||||||||||||||||
List of 6 Events for Episode 1
|
1988 Jun 21 - 1988 Jul 2 Confirmed Eruption VEI: 1
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1988 Jun 21 - 1988 Jul 2 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1
|
1987 Mar 30 (?) - 1987 Jul 2 Confirmed Eruption VEI: 1
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1987 Mar 30 (?) - 1987 Jul 2 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1
|
1986 Jun 3 - 1986 Aug 18 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1986 Jun 3 - 1986 Aug 18 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||||||||||||
List of 7 Events for Episode 1
|
1985 Oct 5 - 1985 Dec 7 Confirmed Eruption VEI: 1
Episode 1 | Eruption | ||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1985 Oct 5 - 1985 Dec 7 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||
List of 4 Events for Episode 1
|
1985 Mar 13 - 1985 Mar 14 Confirmed Eruption VEI: 1
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1985 Mar 13 - 1985 Mar 14 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||
List of 5 Events for Episode 1
|
1980 Aug 8 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1980 Aug 8 - Unknown | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
1978 Jun 27 - 1978 Sep 2 Confirmed Eruption VEI: 2
Episode 1 | Eruption | ||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1978 Jun 27 - 1978 Sep 2 | Evidence from Observations: Reported | |||||||||||||||||||||||||||||||||||||||
List of 6 Events for Episode 1
|
1970 Jun 5 - 1970 Aug 24 Confirmed Eruption VEI: 1 (?)
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1970 Jun 5 - 1970 Aug 24 | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
1969 Oct 10 - 1969 Oct 29 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1969 Oct 10 - 1969 Oct 29 | Evidence from Observations: Reported | ||||||||||||||||||||||||||||||||||||||||||||
List of 7 Events for Episode 1
|
1932 Dec - 1933 Jan Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1932 Dec - 1933 Jan | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
1927 Mar 20 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1927 Mar 20 - Unknown | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
1905 Nov 6 - 1906 Jan 16 (in or after) Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1905 Nov 6 - 1906 Jan 16 (in or after) | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
1904 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1904 - Unknown | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
1902 Jan 31 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1902 Jan 31 - Unknown | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
1894 May - 1894 Jun Confirmed Eruption VEI: 2
Episode 1 | Eruption | ||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1894 May - 1894 Jun | Evidence from Observations: Reported | |||||||||||||||||||
List of 2 Events for Episode 1
|
1893 Jul Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1893 Jul - Unknown | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
[ 1884 May - 1884 Jun ] Uncertain Eruption
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1884 May - 1884 Jun | Evidence from Unknown | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
[ 1883 Jul ] Uncertain Eruption
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1883 Jul - Unknown | Evidence from Unknown | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
1866 Confirmed Eruption VEI: 2
Episode 1 | Eruption | |||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1866 - Unknown | Evidence from Observations: Reported | ||||||||||||||||||||||||
List of 3 Events for Episode 1
|
There is no Deformation History data available for Kanlaon.
There is data available for 1 emission periods. Expand each entry for additional details.
Start Date: 1985 Mar 14 | Stop Date: 1985 Mar 14 | Method: Satellite (Nimbus-7 TOMS) |
SO2 Altitude Min: 12 km | SO2 Altitude Max: 12 km | Total SO2 Mass: 10 kt |
Data Details
Date Start | Date End | Assumed SO2 Altitude | SO2 Algorithm | SO2 Mass |
19850314 | 12.4 | 10.000 |
Maps are not currently available due to technical issues.
There are no samples for Kanlaon in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.
Copernicus Browser | The Copernicus Browser replaced the Sentinel Hub Playground browser in 2023, to provide access to Earth observation archives from the Copernicus Data Space Ecosystem, the main distribution platform for data from the EU Copernicus missions. |
MIROVA | Middle InfraRed Observation of Volcanic Activity (MIROVA) is a near real time volcanic hot-spot detection system based on the analysis of MODIS (Moderate Resolution Imaging Spectroradiometer) data. In particular, MIROVA uses the Middle InfraRed Radiation (MIR), measured over target volcanoes, in order to detect, locate and measure the heat radiation sourced from volcanic activity. |
MODVOLC Thermal Alerts | Using infrared satellite Moderate Resolution Imaging Spectroradiometer (MODIS) data, scientists at the Hawai'i Institute of Geophysics and Planetology, University of Hawai'i, developed an automated system called MODVOLC to map thermal hot-spots in near real time. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. When one is found the date, time, location, and intensity are recorded. 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. Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. There is a drop-down list with volcano names which allow users to 'zoom-in' and examine the distribution of hot-spots at a variety of spatial scales. |
WOVOdat
Single Volcano View Temporal Evolution of Unrest Side by Side Volcanoes |
WOVOdat is a database of volcanic unrest; instrumentally and visually recorded changes in seismicity, ground deformation, gas emission, and other parameters from their normal baselines. It is sponsored by the World Organization of Volcano Observatories (WOVO) and presently hosted at the Earth Observatory of Singapore.
GVMID Data on Volcano Monitoring Infrastructure The Global Volcano Monitoring Infrastructure Database GVMID, is aimed at documenting and improving capabilities of volcano monitoring from the ground and space. GVMID should provide a snapshot and baseline view of the techniques and instrumentation that are in place at various volcanoes, which can be use by volcano observatories as reference to setup new monitoring system or improving networks at a specific volcano. These data will allow identification of what monitoring gaps exist, which can be then targeted by remote sensing infrastructure and future instrument deployments. |
Volcanic Hazard Maps | The IAVCEI Commission on Volcanic Hazards and Risk has a Volcanic Hazard Maps database designed to serve as a resource for hazard mappers (or other interested parties) to explore how common issues in hazard map development have been addressed at different volcanoes, in different countries, for different hazards, and for different intended audiences. In addition to the comprehensive, searchable Volcanic Hazard Maps Database, this website contains information about diversity of volcanic hazard maps, illustrated using examples from the database. This site is for educational purposes related to volcanic hazard maps. Hazard maps found on this website should not be used for emergency purposes. For the most recent, official hazard map for a particular volcano, please seek out the proper institutional authorities on the matter. |
IRIS seismic stations/networks | Incorporated Research Institutions for Seismology (IRIS) Data Services map showing the location of seismic stations from all available networks (permanent or temporary) within a radius of 0.18° (about 20 km at mid-latitudes) from the given location of Kanlaon. Users can customize a variety of filters and options in the left panel. Note that if there are no stations are known the map will default to show the entire world with a "No data matched request" error notice. |
UNAVCO GPS/GNSS stations | Geodetic Data Services map from UNAVCO showing the location of GPS/GNSS stations from all available networks (permanent or temporary) within a radius of 20 km from the given location of Kanlaon. Users can customize the data search based on station or network names, location, and time window. Requires Adobe Flash Player. |
DECADE Data | The DECADE portal, still in the developmental stage, serves as an example of the proposed interoperability between The Smithsonian Institution's Global Volcanism Program, the Mapping Gas Emissions (MaGa) Database, and the EarthChem Geochemical Portal. The Deep Earth Carbon Degassing (DECADE) initiative seeks to use new and established technologies to determine accurate global fluxes of volcanic CO2 to the atmosphere, but installing CO2 monitoring networks on 20 of the world's 150 most actively degassing volcanoes. The group uses related laboratory-based studies (direct gas sampling and analysis, melt inclusions) to provide new data for direct degassing of deep earth carbon to the atmosphere. |
Large Eruptions of Kanlaon | Information about large Quaternary eruptions (VEI >= 4) is cataloged in the Large Magnitude Explosive Volcanic Eruptions (LaMEVE) database of the Volcano Global Risk Identification and Analysis Project (VOGRIPA). |
EarthChem | EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility Integrated Earth Data Applications (IEDA). IEDA is a collaborative effort of EarthChem and the Marine Geoscience Data System (MGDS). |