The hazard status remained at Alert Level 2, indicating a low level of volcanism. PHIVOLCS reminded the public to refrain from venturing into the 6-km Permanent Danger Zone because life-threatening volcanic flows may occur with little or no warning. Check out the latest Creative Live! Cam Webcams. Enhance your video chatting, recording and sharing experiences, all in stunning high-definition quality
The main lava flow moved SE in the general direction of Mabinit on 21 June, and the lowermost toe of the lava flow descended 300 m farther, to ~1,500 m elevation. On 22 June the lava flow reached 1,200 m elevation; by 23 June, it had descended 3.4 km from the summit to reach 600 m elevation. The webcam in Cambrils - local information and the latest Feratel live-cams in Cambrils show the current weather, and the conditions at that location .P. Garcia Avenue, University of the Philippines Campus, Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost. gov.ph/).
Mayon Volcano by Antonio Liao. .a beautiful princesssilenton the slopes. Page. Comments about Mayon Volcano by Antonio Liao. There is no comment submitted by members. PHIVOLCS reported that since the Alert Level for Mayon was lowered to 1 on 2 March, seismicity decreased, and ground and tilt monitoring data suggested regional faulting and not magmatic intrusion. Steaming from the crater was diffuse and crater incandescence had ceased in March. Sulfur dioxide emissions had decreased to below baseline levels. On 27 November the Alert Level was lowered to 0 and the public was reminded not to enter the 6-km-radius Permanent Danger Zone (PDZ). PHIVOLCS reported that during 21-27 March activity at Mayon included periods of gravity-driven lava advancement, gas-and-steam emissions, rockfalls, and quiescence. Lava flows were about 3.3 km, 4.5 km, and 1.9 km long in the Mi-isi (S), Bonga (SE), and Basud (E) drainages, respectively. Steam-and-gas emissions drifted mainly SW. At 1039 and 2133 on 23 March pyroclastic flows traveled 4-5 km down the Mi-isi drainage, producing light brown ash clouds that drifted SW. The Alert Level remained at 3 (on a 0-5 scale) and PHIVOLCS reminded residents to stay away from the 6-km-radius Permanent Danger Zone and the 7-km Extended Danger Zone on the SSW and ENE flanks."No casualties were reported during the eruption, but 8,000 people on the SW sector of the volcano and within an 8 km radius had to be evacuated. An additional 15,000 people evacuated voluntarily due to their fear of the eruption, even though they were not within the declared danger zone." Activity briefly intensified early on 7 March, when ash-laden clouds and a little incandescent material were ejected.
Quieter lava effusion with fewer fountaining events was more typical behavior beginning on 23 February. Numerous episodes of lava-collapse pyroclastic density currents were visually observed on the Mi-isi, Basud, and Bonga-Buyuan Gullies within 2-4 kilometers of the summit crater during the second half of February. Deflation of the lower slopes that began on 20 February was recorded by electronic tiltmeter, consistent with the transition to seismically quieter lava effusion at the summit crater. However, the overall electronic tiltmeter and the continuous GPS data indicated that the volcano was still inflated relative to October and November 2017 levels.By 1 June the hazard status had been decreased to Alert Level 0. Seismicity had also decreased markedly; only two HF events and two short- duration HF tremors were reported on 1 June. Crater illumination resumed the same day. SO2 flux readings were not available for the month.
A thick column of ash streamed five kilometres into the air above the Mayon volcano, with falling ash leaving the town of Guinobatan in a state of “zero visibility”, according to CNN reports. BULBCAM
Tremor, light steaming, low-frequency volcanic earthquakes, and elevated SO2 fluxes continued for several days. Also, deformation surveys conducted with laser-ranging EDM equipment indicated sustained inflation on the SE slope. Information Contacts: G. Andal, COMVOL, Quezon City; J. Wolfe, Pan Asean Technical Services, Manila.
Maho Beach Cam is a live streaming HD-quality Internet video production by PTZtv. Watch the famous airplane landings over Maho Beach at Princess Juliana International Airport (SXM) on St. Maarten. Hear those engines scream as full thrust takeoffs accelerate past our camera! If you live on St.. PHIVOLCS reported that white steam plumes from Mayon rose 750 m above the crater rim on 30 June and drifted NE, N, NW, and SW. On 1 July white plumes drifted down the flanks. A short-lived event at 1234 produced a gray gas plume. Crater incandescence was visible at night. The Alert Level remained at 2 (on a 0-5 scale) and PHIVOLCS reminded residents to stay away from the 6-km-radius Permanent Danger Zone and the 7-km Extended Danger Zone on the SSW and ENE flanks.Check out the list below of volcano webcams, sorted by geographic location. I can't guarantee that they all work – webcams are tricky to keep operational even in ideal conditions – but even clicking through a few shows just how restless many volcanoes around the globe are. If you find a broken link or discover a new webcam not on the list, let me know in the comments. Be sure to bookmark this page so you can find it when some volcano does start acting up around the world!"An eruption started at about 2030 on 7 May and gradually increased in intensity, reaching a maximum on 22 May. The event was characterized by weak lava flow extrusion at the start, and at the height of the eruption there was a fascinating night display as incandescent basaltic [andesite] lava flowed down the SW flank. Strong earthquakes were felt at the Mayon Rest House Observatory (on the N flank, elevation 760 m, figure 1) on 26 May, accompanied by voluminous ejection of ash-laden clouds and spattering of incandescent pyroclastic materials. From then on, activity began to decline, punctuated at first by short lulls, which became longer each day until ash ejections, rumblings, and volcanic tremor ceased on 29 May. Small amounts of lava continued to be extruded as of 2 June. This decline in activity suggests that the critical period of the eruption has apparently passed.According to news reports, the continuing unrest at Mayon led authorities to extend the 6-km-radius Permanent Danger Zone to 7 km in the SE quadrant of the volcano on 13 October. Seismicity and SO2 emissions increased during the previous week. During a 24-hour-monitoring period, ending the night of 17 October, 16 volcanic earthquakes were recorded beneath Mayon's lower flanks. Authorities maintained Alert Level 2 (on a scale of 0-5).
Eruptions at Mayon in June and July 2001 were followed by a decrease in seismic activity beginning on 10 August. Low-frequency volcanic earthquakes and SO2 fluxes were still high and were probably related to shallow magma degassing. While various monitoring parameters continued to reflect significant unrest, the general trend was one of declining activity (BGVN 26:08).A brief helicopter flight over Albay Gulf looking at Legaspi and Santo Domingo showed the dark curtain of ash progressively blanketing these localities. Pyroclastic flows remained well within the PDZ, a fact used to conclude that additional areas were not endangered. Only small-volume pyroclastic flows were seen descending the S-flank regions (Mi-isi and Anoling gullies).
PHIVOLCS reported that at 1509 on 13 July a minor rockfall descended the Mi-isi drainage on Mayon’s S flank, generating a brownish ash cloud. The event was preceded by heavy rainfall on the upper flanks. Sulfur dioxide emissions were 2,398 tonnes/day. Precise leveling data obtained during 2-14 April indicated inflation relative to data collected in late March; electronic tilt data showed pronounced inflation on the mid-flank beginning on 25 June possibly due to a deep aseismic magma intrusion. The Alert Level remained at 2 (on a 0-5 scale) and PHIVOLCS reminded residents to stay away from the 6-km-radius Permanent Danger Zone and the 7-km Extended Danger Zone on the SSW and ENE flanks.Seismic activity and lava extrusion from Mayon decreased during 6-12 September. Steam plumes from the summit crater drifted mainly W, N, and E. Ground-deformation measurements showed an overall deflation. On 11 September, the Alert Level was lowered from 4 to 3 (scale is 0-5, 0 referring to No Alert status).Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Agence France-Presse (AFP); Gulf News
The following report was received [on] 17 October 1968. "17 October 0500Z. Continued build-up in seismic activity seems to indicate Mayon pulling out of trauma to begin another period of peak activity. Low, heavy rain clouds blanket volcano. Apparent most stream channels already nearly filled with mud and boulders. Continue maximum precaution. Watch for possible mudflows."VAAC, SO2, and MIROVA information. The Tokyo VAAC reported the first ash emission from Mayon on 13 January 2018 as a plume that rose to 5.2 km altitude and drifted SW. Many subsequent ash emissions were obscured by meteoric clouds and were only occasionally observed in satellite imagery. The ash plume from the large explosion on 22 January was observed in satellite imagery at 10.9 km altitude drifting NW. Numerous daily VAAC reports were issued through February; they were intermittent in March, ending on 23 March 2018. Plumes generally were reported at 5.2-7.6 km altitudes. Small sulfur dioxide plumes were captured by the OMI and OMPS satellite instruments on several days between 22 and 31 January 2018 (figure 37).
By the evening of 26 January 2018, the lava fountaining episodes had transitioned into aseismic lava effusion, feeding incandescent flows into the Bonga and Mi-isi gullies on the S flank, and advancing the flow in the Bonga significantly downslope to 1.8 km. Fewer fountaining episodes continued during 27-28 January. Heavy rainfall during 28-29 January remobilized deposits from pyroclastic density currents and generated sediment-laden stream flows in several channels (figure 34) and channel-confined lahars on the Binaan Channel.The summit crater continued to exhibit glow on 25 August, with varying intensity, and there was moderate steam emission. COSPEC measurements of SO2 levels in the steam plume were ~630 metric tons/day (t/d), well above the 100-200 t/d measured during quiet periods. No unusual seismicity was detected. The last sighting of crater glow was on 2 September, although it was not until 12 September that SO2 measurements by COSPEC decreased to near background.Avachinsky - info - webcamBezymianny - info - webcamGorely - info - webcamKizimen - info - webcamKliuchevskoi - info - webcams: one | two | threeKoryaksky - info - webcamKoryaksky and Avachinsky - info Avachinsky - webcamShiveluch - info - webcams: one | two | threeTobalchik - info - webcam"Eruptive activity started 9 September at 1923. Initial activity was dominantly Strombolian, with incandescent spattering at the summit and production of small lava flows. A mound of solidified lava inside the crater blocked the 1968 notch at the SW rim, so the small lava flows and initial pyroclastic flows (see below) moved predominantly NW.
At 0745 on 26 July there occurred another ash explosion with similar seismic signature. In retrospect, sequences of low-frequency seismic events were detected by the Mayon Resthouse station (780 m elevation) before the onset of explosive eruptions at 0756 on 26 July. These events were not detected at other stations or were obscured by high-frequency tremor associated with both lava flowing out at the uppermost elevations and lava fragments detaching from the advancing lava flow. Holiday Live Cam map search. Map search engine of webcams and the Map search for accomodation Easy and quick search on the HLC page through the menu. On the Holiday Live Cam webcam collecting site, you can virtually have a world-wide webcam journey PHIVOLCS reported that during 18-25 November white plumes rose from Mayon's crater and drifted WSW, WNW, NE, and SE, often downslope. As many as six volcanic earthquakes and one rockfall event were recorded per day. Sulfur dioxide emissions were below baseline levels. Alert Level remained at 3 (on a 0-5 scale). PHIVOLCS reminded residents of the 6-km-radius Permanent Danger Zone (PDZ) around the volcano and the 7-km Extended Danger Zone (EDZ) on the SE flank.June and July eruptions compared. The eruptions in June appeared to be more voluminous and produced more lavas than tephra. The estimated volume of 15 x 106 m3 was in the ratio 2/3 lava and 1/3 pyroclastics. The June eruptions also produced pyroclastic flows that ran through many gullies radiating around the cone. The 26 July eruption produced roughly similar proportions of lava and tephra (namely, 5 x 106 m3 lava; 6 x 106 m3 tephra).
Officials worry eruption may last months, disrupting lives and livelihoods of people in its shadow Most of the ash clouds were eventually carried to the SW and W, affecting Ligao, Guinobatan, and Camalig. However, the pyroclastic flows did not travel beyond the present danger zones. The ash clouds contained high concentrations of sulfur dioxide, with COSPEC-recorded emission rates of 13,000 t/d, as expected for an eruption cloud. Aircraft were warned to avoid lingering ash clouds to the W of the volcano. The E side, towards the Legaspi airport, remained free from volcanic ash, debris, and SO2 emissions. The Mayon volcano's crater glows as it emits lava in Legazpi City, Albay province, south of Manila December 29, 2009. Policemen escort villagers living near the slopes of the Mayon volcano towards a truck during a forced evacuation at the Muladbukad grande in Guinobatan town of Legaspi..
Seismograph recordings for the past 24-hour period ending at 0600 today showed that Mayon is still giving off volcanic tremors. The seismic level of Mt. Mayon remains high and its crater's emission shows that its activity was above normal. Mayon also puffed out ashes at noon yesterday.At 1813 on 14 May, a small ash puff was emitted from the summit crater. This very brief explosion caused a small volume of ash and steam to rise less than 100 m above the crater and to later be blown NW. The Mayon Resthouse and Sta Misericordia seismic stations recorded the ash puff as a small-amplitude event. Prior to the ash explosion, one short-duration tremor was recorded. Volcanic gas outputs were notably moderate in volume, and the sulfur dioxide emission rates increased from the previous 1,824 metric tons per day (t/d) to ~3,088 t/d. The seismic characteristics associated with the ash and steam emission appeared similar to, though smaller than, previous explosions since 22 October 2002, indicating that this ash puff was very minor. This assessment was also consistent with the smaller volume of ash produced.Rockfalls due to molten lava fragments rolling down from the dome dominated activity during 13-14 May. When conditions cleared briefly on 14 May observers saw that the partial dome collapse had produced a V-shaped gash; this breach was the source of the outpouring lava. Avalanches had reached 500 m downslope as of this date.
Activity during May 2003. A small explosion from the crater at 0721 on 6 May produced a brownish ash-and-steam column that rose to ~450 m above the summit crater and was blown SW. The ash-and-steam column rose slowly with minimal noticeable force and was not detected by the volcano's seismic network, indicating a very shallow source. No significant seismicity occurred prior to the explosion. However, electronic tiltmeters on the N and S flanks continued to show inflation. Likewise, a precise leveling survey on 24 April 2003 showed a general inflation of the N flank. Alert Level 1 remained in effect.At Arimbay (approximately 2.5 km N of Legazpi City), the smell of sulfur was noticed about 5 minutes prior to the arrival of a lahar at 1530 on 3 March. The knee-deep lahar was warm but not boiling. Approximately 1.5 m of mud, stones, and boulders deposited by previous lahars blocked traffic on the Legazpi-Tabaco road in Arimbay. Also on 3 March, a pyroclastic flow, larger and darker than the one seen on 1 March, "casually" rolled down the Bonga Gully.During 22 October-4 November 2014, white plumes rose from the crater and drifted SW, WSW, WNW, and NW. Weak incandescence from the crater was noted at night on 22, 25, 27, and 28 October, and a few volcanic earthquakes and rockfall signals were periodically recorded.Volcanic activity increased at Mayon, with a lava dome collapse occurring on 13 May. On 12 May seismographs detected a series of explosions at Mayon's summit crater. The following day the SE-facing portion of the lava dome partially collapsed, leaving a V-shaped opening in the dome. The collapse produced small lava avalanches that reached a maximum runout distance of 300 m down the Bonga Gully. After the collapse, incandescence was observed at the dome and lava fragments fell into the gully. Seismic activity indicated frequent earthquakes, tremor, and explosions. On 14 May rockfalls dominated the seismicity. On 15 May there was a lull in activity, with no rockfalls or lava avalanches occurring. Alert Level 3 remained in effect, prohibiting entry within the 6-km-radius permanent danger zone. PHIVOLCS warned that lava flows and/or pyroclastic flows could be produced in the future and residents just outside of the permanent danger zone should be prepared to evacuate at any time.
Overall, unrest was accelerating. On the morning on 25 July, the bulletin also added that the current extrusion of lava was clear evidence of eruption and that more explosive eruptions were expected. At 0418 on 25 July seismometers detected more or less continuous high-frequency tremor. Although clouds shrouded Mayon, volcanologists believed these signals indicated that a lava flow had extruded from the dome, an idea confirmed when observers saw a short lava tongue draping the SE slope just below the summit crater.Scientists were alerted when the S-flank seismic station at ~800 m elevation registered an abrupt increase, from 5 rockfall events on 19 January to 48 events on 20 January. Over the same time period an upper seismic station (at 1,700 m elevation) recorded a jump from 25 to 142 events. Incandescent rockfalls became persistent.PHIVOLCS reported that during the week ending on 1 April there had been a total of 23 low-frequency earthquakes. The SO2 flux during the same period averaged 2,174 metric tons/day, which is still significantly above the baseline value of 500 tons/day. Deformation monitoring showed that the volcano was inflated, but the present trend revealed insignificant change. The crater was visible, but no glow was observed. Moderate steaming was typical. Alert Level 3 remained in effect, prohibiting entry within the 6-km-radius permanent danger zone.
During 9-15 August, explosive activity continued at Mayon after a brief respite on 8 August. Based on interpretations of seismic data, minor explosions during 9-11 and 13-15 August were accompanied by lava extrusion and collapsing lava flow fronts that released blocks and small fragments. A drop in SO2 emissions on 9 August worried volcanologists that something had blocked the flow of magma in Mayon's conduit and could therefore cause a build up in pressure resulting in a larger eruption. Visual observations were commonly obscured by clouds. On 11 August an ash plume was seen drifting ESE. On 12 August, four explosions occurred; one produced a pyroclastic flow that traveled over the SE and E slopes and generated a plume that rose to an altitude of 500 m and then drifted NE. On 15 August, a brief break in the clouds allowed for a view and confirmed the presence of fresh pyroclastic deposits from activity in the previous days. Approximately 40,000 people remained in evacuation centers and authorities maintained an Extended Danger Zone at 8 km from the summit in the SE sector.Sources: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Manila Bulletin; Associated PressThe next available report on Mayon indicated that a small phreatic eruption occurred on 7 May 2013 lasting in the range of 73-146 seconds. PHIVOLCS observed that a gray-to-brown ash cloud rose 500 m above the crater and drifted WSW. Traces of ash fell in areas WNW, affecting communities up to 19 km away. The seismic network detected a single associated rockfall event. Seismicity and gas emissions remained within background levels and indicated no increase in activity. The Alert Level remained at 0.At about 2000 on 30 June, mudflows triggered by continuous rains accompanying Typhoon Daling swept villages in the S and E sectors of Mayon. Preliminary estimates set casualties at about 100 persons with many more missing [but see 6:7].Faint crater glow continued to be observed during nights with good visibility in October and November. Moderate steam emission covered 30-50% of the crater and blue volcanic fumes sometimes moved slowly downslope.
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/); Sentinel Hub Playground (URL: https://www.sentinel-hub.com/explore/sentinel-playground); Global Sulfur Dioxide Monitoring Page, Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center (NASA/GSFC), 8800 Greenbelt Road, Goddard, Maryland, USA (URL: https://SO2.gsfc.nasa.gov/).On the evening of 23 August, staff at the Lignon Hill Observatory in Legazpi observed moderate to intense glow from the crater of Mayon. Moderate steam emissions rising ~300 m above the summit preceded the observation of glow. The Philippine Institute of Volcanology and Seismology (PHIVOLCS) increased the Alert Level to 2, indicating that volcanic activity had increased slightly. PHIVOLCS also recommended strict compliance with the 6-km-radius permanent danger zone, an area restricted to regular human activity, especially below the Bonga channel on the SE flank. The PHIVOLCS Quick Response Team was dispatched to augment monitoring staff at the Lignon Hill and Mayon Resthouse observatories.PHIVOLCS reported that on 28 October a minor ash explosion from Mayon produced a brownish ash plume that rose 600 m above the crater and drifted NE. The Alert Level remained at 2 (on a scale of 0-5). The 7-km Extended Danger Zone (EDZ) on the SE flank and the 6-km Permanent Danger Zone (PDZ) in all other areas remained in effect.Surface activity at Mayon consisted of incandescent lava fragments rolling down the slopes and glow coming from the summit crater. Moderate white steam emissions continued from the summit. The number of daily volcanic earthquakes was low during 20-24 September, with 1-3 events per day. On the 25th there were 14 earthquakes recorded. There were also 114 tremor episodes that day, also a high for the week ending on 26 September. Sulfur dioxide flux remained above normal, between 1,200 and 2,200 metric tons/day.
Credit: Mayon Volcano Observatory. Renato Solidum, head of PHIVOLCS said lava flowed about 800 m (0.5 miles) from the crater on Monday morning and ash clouds appeared mid-slope as lava fragments rolled downs. It was hard to track down the lava flow given the thick clouds shrouding the volcano.. The Mayon Volcano is an active stratovolcano in the Philippines on the island of Luzon, in the province of Albay in the Bicol Region. The near perfectly cone shaped volcano is situated 15 kilometres northwest of Legazpi City
en Mayon Volcano's eruption in 1834 started a wave of migration from the neighboring province of Albay to the rich verdant slopes of Tigaon. en Yet, that is the situation of thousands living in the towns and barrios (small villages) around majestic Mayon Volcano in the Bicol region of the.. On 17 March at 1254, 1350, 1609, and 1619 partial collapse of the new lava flow on the volcano's upper middle slopes produced voluminous secondary pyroclastic flows, with the associated ash clouds blown to the SW. On 19 March at 0138, 0203, and 0300 similar secondary pyroclastic flows occurred with ash clouds that blew NE. The billowing ash clouds did not originate from the crater, but from the side of the lava flow that failed on the volcano's upper slope, and from descending detached lava fragments along Bonga Gully. Scientists expected the series of secondary pyroclastic flows due to the instability of volcanic material deposited on steep ground.Following the phreatic eruption on 7 May 2013 that killed 7 climbers (BGVN 38:04), there has been little increase in volcanic activity at Mayon volcano. Seismicity has mostly receded to baseline levels, aside from occasional volcanic earthquakes. These earthquakes occur about once every other day, with minimal earthquakes in June and September. The activity reported by the Philippine Institute of Volcanology and Seismology (PHIVOLCS) in table 12 below represents a continuation of table 11 from a previous Bulletin report (BGVN 34:12). Rockfalls and earthquakes are plotted in figure 22.
Rockfalls, small avalanches, moderate steam emission, and fair-to-bright crater glow dominated the visible volcanic activity at Mayon during the week. Partial lava-dome collapses occurred on 11 June at 1347 and on 12 June at 1819. The 11 June collapse produced a small pyroclastic flow that descended the Bonga Gully, reaching an elevation of 1,480 m and producing a thin ash cloud that drifted to the E. The 12 June collapse sparked a period of vigorous, continuous emission of lava fragments for ~1 hour. During the week up to 198 rockfall events were detected per day. A maximum of 2,700 metric tons of SO2 was measured per day, which was lower than the previous week but above the baseline value of 500 tons/day. Alert Level 3 remained in effect, prohibiting entry within the 6-km-radius permanent danger zone. PHIVOLC warned that residents around the volcano, especially those staying in areas facing the Bonga Gully and the SE sector, should be vigilant and prepared to evacuate at any time. A danger zone has been extended to five miles around the crater of the Philippines' most-active volcano.Jan PHIVOLCS inferred that Mayon had again entered a mild eruptive stage. The character of unrest resembled activity observed between mid May and 20 June, prior to explosive eruptions on 24 June. Scientists recognized that an explosive and hazardous eruption could occur anytime. By 23 July, PHIVOLCS gave the Albay provincial government a notice of increasing unrest and by 25 July, the Municipal Mayors were informed of reactivation and possible explosive eruption of Mayon.
The U.S. Air Force Weather Agency (AFWA) reported that an eruption had occurred on 4 June 2007. It sent a steam-and-ash plume seen on satellite imagery up to 4 km altitude, which blew toward the SW.The fountaining episodes typically lasted 20 minutes; the longest lasted 50 minutes. They were separated by repose periods lasting 30 minutes to 1 hour. Some episodes were followed by 10-20 minutes of intermittent 2-Hz tremor, the amplitude of which varied greatly suggesting that each tremor episode consisted of a series of tremor events. The tremor did not correlate with any visible steaming. Continuous, strong gas jets, glowing "like a blowtorch" and emitting a continuous "jet plane sound," were visible from Legazpi city, 14 km SE of the summit. They appeared to be in the summit crater, 100-200 m upslope from the vent.PHIVOLCS reported that during 14-20 February daily activity at Mayon continued to be characterized by lava effusion from the summit crater, rockfalls, lava fountains, steam emissions, advancing lava flows on the flanks, and pyroclastic flows. Weak and sporadic lava fountaining events each lasted between 5 and 239 minutes, and were sometimes accompanied by rumbling sounds audible with a 10-km radius. Heavy rainfall on 14 February caused lahars in the Anoling drainage, and sediment-laden streams in most channels where pyroclastic flow deposits were emplaced. During 16-17 February lava fountains were 200-500 m tall and generated steam plumes that drifted SW, WSW, and NW. A lava-fountaining event that began at 0103 on 17 February lasted for 12 hours and 18 minutes. Lava flows 3.3 km, 4.5 km, and 900 m long in the Mi-isi (S), Bonga (SE), and Basud (E) drainages, respectively, continued to be active. Pyroclastic flows traveled 4.2-4.6 km in the Mi-isi, Bonga, and Basud drainages. The Alert Level remained at 4 (on a 0-5 scale) and the public was warned to remain outside of the Danger Zone, defined as an area within an 8-km radius. Information Contacts: Raymundo S. Punongbayan and Ernesto Corpuz, Philippine Institute of Volcanology and Seismology (PHIVOLCS), C.P. Garcia St. Diliman, Quezon City, Philippines (URL: http://www.phivolcs.dost. gov.ph/). Hawaii Volcanoes - Halema`uma`u Crater USGS Hawaii Volcanoes - Kilauea Summit Hawaii Volcanoes - Pu`u `O`o Crater Isle Royale - Tobin Harbor Isle Royale - Mott Island Dock. Joshua Tree - View from Belle Mountain Lassen Volcanic - Kohm Yah-mah-nee Lassen Volcanic - Manzanita..
On 30 July at 1315, Mayon produced a mild ash ejection. MVO reported a small ash plume that rose 1 km. Seismicity associated with the event lasted for about 1 minute. As with the 16 July event, other monitoring, including SO2 flux readings, did not indicate further activity. Mayon's Alert Level was undisclosed for the month.At around 1605 and 1702 on 29 June, Mayon erupted again and sent relatively small pyroclastic flows down the Bonga Gully to the SE. Over the period 30 June to 19 July, Mayon's apparent activity waned and the hazard status was eventually lowered to level 3 (which states that an eruption may still be expected within the coming weeks). Observations in support of reduced activity included a general deflation of the edifice, decreased seismic activity, lowered gas emission rates, and the disappearance of summit incandescence. The first eruptive episode ended and scientists inferred that intrusions into the cone had ceased.
This cam is also a long running cam that has recorded some of the most astounding wildlife footage. This is a 24/7 cam controlled by a dedicated team of observers across the world. Live Web Cam | Djuma Waterhole. safariLIVE Stream This Video Is about Mayon Volcano Final Eruption 2018. Red Alert presents the threat of a deadly lahar flow on areas near Mayon Volcano. This past week, the Mayon Volcano has been active recently for spewing lava and fog that alarmed residents who live nearby
182 Gönderi - Mayon Volcano konumunda çekilen Instagram fotoğraflarını ve videolarını gör Phreatic eruptions at Mayon on 13 July produced ash that fell up to approximately 5.3 km NE in Calbayog, Malilipot. The Alert Level was raised from 1 to 3 (scale is 0-5, 0 referring to No Alert status) after observers reported lava flows on the SE slopes, the predominant direction for lava flows and rockfalls. On 16 July, a danger zone 6 km from the summit was extended to 7 km in the SE area. Incandescent material was shed from an 800 m long lava flow moving SSE towards Bonga gully on 16 and 17 July. On 18 July, PHIVOLCS reported that the lava flow reached 1 km in length and incandescent boulders rolled 3 km towards the Bonga gully. The following report was received [on] 14 October 1968. "Mayon Volcano, Philippines. As of 12 October [at] 1100. Moderate crater steam emission persists. Low seismic activity. As of 13 October [at] 1300 steam activity continues in crater. Lull in seismicity. As of 14 October [at] 1200 steam emission now mild, but renewed volcanic microseisms of appreciable magnitude."Philippine Red Cross, on Monday, tweeted: “Just in. Another explosion of Mayon Volcano taken at 5:50pm today.PHIVOLCS reported that during 5-11 December white steam plumes periodically emitted from Mayon drifted mainly WSW. Crater incandescence was sometimes visible at night. A four-minute long event recorded by the seismic network began at 1224 on 9 December, and produced a grayish-brown ash plume that drifted W. The Alert Level remained at 2 (on a 0-5 scale) and PHIVOLCS reminded residents to stay away from the 6-km-radius Permanent Danger Zone and the 7-km Extended Danger Zone on the SSW and ENE flanks.
GeoCam.tv offers many free live streaming webcams, cctv, and other cams, in real-time, from around the world, presented on a Google Maps Mashup Since the last report (BGVN 25:04), activity was variable at Mayon. The following report covers activity during April 2000-May 2001, but does not include the event that began on 24 June 2001; details of that eruption will appear in a subsequent issue. This report was compiled from reports posted on the Philippine Institute of Volcanology and Seismology (PHIVOLCS) website.The following 86 samples associated with this volcano can be found in the Smithsonian's NMNH Department of Mineral Sciences collections, and may be availble for research (contact the Rock and Ore Collections Manager). Catalog number links will open a window with more information.After the large eruption on 24 June volcanic activity returned to relatively low levels for several days. During this period, rockfalls dominated the seismic records as lava slowly flowed to the SE down the Bonga Gully. PHIVOLCS reported that due to diminished lava extrusion lava was not expected to reach populated areas. Volcanic activity increased on 29 June when explosions occurred at 1605 and 1702. These explosions generated pyroclastic flows that traveled down the Bonga Gully and generated billowing ash clouds that ascended to ~4 km above the volcano. The pyroclastic flows reached ~3 km to the SE of the summit towards the general direction of Matanag Gully. During the eruption a portion of the Upper Basud Gully in the volcano's eastern sector collapsed. On 1 July, SO2 emission rates were as high as 8,700 metric tons per day, a value about 5-fold higher than on 29 June. By 2 June the rate of SO2 emission greatly decreased to 840 tons per day. PHIVOLCS stated that due to the ongoing significant inflation of the volcanic cone and anomalous rapid decline of SO2 emission rates a high likelihood of continued explosive eruptions in the coming days remains. Accordingly, the hazard status remained in the top category, Alert Level 5 (hazardous eruption in progress).
PHIVOLCS reported that 11 earthquakes were detected during 14-15 September, with steam plumes drifting NW and ENE. On 15 September, three ash explosions produced a brownish ash plume that rose 700 m above the crater and drifted SW. On 28 October a minor explosion produced a brownish ash plume that rose 600 m above the crater and drifted NE, preceded by 13 volcanic earthquakes over the previous 24-hour period..35 km during 26 July-1 August to reach a maximum distance of 5.8 km SSE from the summit on 1 August. Smaller lava flows and incandescent blocks descended adjacent gullies. On July 29, light ash accumulation was reported about 12 km S and SE, in Daraga municipality and Legazpi City and vicinity, respectively. Emissions of sulfur-dioxide reached ~12,500 tons per day on 31 July, a record high for the current period of unrest.
PHIVOLCS reported that during 15 to 19 March, 10-37 low-frequency earthquakes were recorded daily. An average of 2,900 metric tons per day (t/d) of SO2 was recorded during the previous week, which was significantly above the baseline value of 500 t/d. Many days a slight inflationary trend was detected at the volcano's edifice and moderate steaming was seen. No incandescence was observed at the crater. PHIVOLCS warned that instrumental and visual observations suggested that an eruption may occur in the coming weeks and that the volcano remained at Alert Level 3. Observations revealed that the lava dome growing at the summit had overlapped the pre-existing SE rim of the summit crater. Further growth of the lava dome towards the SE could result in rockfalls and avalanches that would be channeled down the SE-flank Bonga Gully. In addition, large pyroclastic flows could occur down the volcano's SE slope.PHIVOLCS reported that the increase in volcanic activity, which has occurred since a lava dome was spotted in Mayon's summit crater on 10 January, led them to raise the Alert Level from 2 to 3 (an increased tendency towards eruption, with magmatic outbursts possible within the coming weeks) on 25 January. During the previous week the monitoring networks had detected numerous volcanic earthquakes, continued inflation at the edifice, and very high gas emission from the summit crater (5,040 metric tons per day). In addition, several ash ejections coincided with earthquakes that originated from beneath the lava dome, which appeared to grow during the week. The ash-laden volcanic plumes typically rose up to 500 m above the crater and generally drifted with the prevailing wind to the WNW and NW. Download this free picture about Philippines Mayon Volcano from Pixabay's vast library of public domain images and videos
PHIVOLCS reported that during 18-24 April white steam plumes from Mayon drifted NW, W, SW, and NE. Crater incandescence was visible at night. The sulfur dioxide flux was 796 tonnes/day on 17 April. The Alert Level remained at 2 (on a 0-5 scale) and PHIVOLCS reminded residents to stay away from the 6-km-radius Permanent Danger Zone and the 7-km Extended Danger Zone on the SSW and ENE flanks.. At 2000 on 23 June the Alert Level was raised from 3 to 4 when the already substantial lava extrusions changed from quiet effusions to more explosive, but nonetheless non-destructive, Strombolian outbursts. The latter were first observed in the crater at 1909 on 23 June. Small explosions in the crater sent molten lava up to 50 m above the rim. The Decade Volcanoes list is a list of 16 volcanoes worldwide identified by the International Association of Volcanology and Chemistry of the Earth's Interior (IAVCEI) as being worthy of particular study in light of their history of large, destructive eruptions and proximity to populated areas Beginning at 0700 on 25 June there was a slight increase in seismicity and SO2 emission. The COSPEC measured an SO2 flux of 4,800 tons/day, compared with 4,200 tons/day the previous day. SO2 fluxes normally average 500 tons/day. A short interval of high-frequency tremor was also recorded.In time, observations from Bonga, ~8 km SE of the summit, indicated that incandescent rockfalls were apparently caused by slowly ascending magma entering the dome. The magma was degassed but hot, presumably a remnant of magma erupted during 2000. PHIVOLCS later postulated that ascending magma punched an exit point on the SE flank of the growing lava dome. This material then spilled into the Bonga Gully, with hot lava boulders as big as trucks falling, rolling, and sliding to form a pyroclastic apron on slopes at 1,800-2,000 m elevation. Rockfall activity, monitored via the seismic network, progressively increased in frequency until magma discharge was sufficient to form a stubby lava flow on 17 June. By 20 June, the seismograms displayed more or less merging codas of high-frequency tremor, which suggested that lava extrusion dominated earlier rockfall activity. As seen earlier, the lava flow was thought to represent relatively fresh but still degassed magma.
During September, 36 high-frequency and 31 low-frequency earthquakes were recorded plus 129 low-frequency and 16 high-frequency tremor episodes. From 1 to 9 October, 19 high-frequency and seven low-frequency earthquakes were detected in addition to 71 harmonic tremor episodes.As of mid-September, the dominant seismicity consisted of occasional high-frequency volcanic earthquakes (<5 events/day); they were large enough to be located, and occurred within the E and N parts of the edifice. Observations of the crater area disclosed that some multi-phase events were due to large lava blocks detaching from the vent. The vent is open to the SE as a result of the 1993 explosions. A preliminary investigation of a water well in Malilipot (ENE of the summit) on 25 August revealed a slight decrease in water level, also an indicator of volcanic unrest. However, further measurements of water wells on the SE and S margins of lahar fans around Mayon, where most wells are located, did not show measurable or significant changes. PHIVOLCS therefore concluded that little ground deformation was taking place.At 0746 on 7 March, a parallel collapse of the new lava flow deposit in the upper middle slopes produced a voluminous secondary pyroclastic flow. The billowing ash cloud descended the Bonga Gully to the SE. Explosions shook the Mayon volcano, while fountains of lava spewed from its summit today (Jan. 22), causing the Philippines government to raise the hazard level from 3 to 4 Live Science is supported by its audience. When you purchase through links on our site, we may earn an affiliate commission
Reference. Horton, K.A., Williams-Jones, G., Garbeil, H., Elias, T., Sutton, A.J., Mouginis-Mark, P., Porter, J.N., and Clegg, S., 2006, Real-time measurement of volcanic SO2 emissions: validation of a new UV correlation spectrometer (FLYSPEC): Bull. Volc., v. 68, no. 4, p. 323-327 (doi:10.1007/s00445-005-0014-9). Mount Mayon in the Phillippines is an active volcano that is on the brink of eruption. Seismologists are monitoring the volcano, which last erupted in 2014, after it started recording higher levels of activity in January 2018. The alert level has been raised to level 4, suggesting an eruption is imminent
On 10 January aerial observers noted that the dome appeared to have a spiny, blocky surface, which resulted from the crater floor being pushed upward by rising magma. Slight incandescence was also emanating from the crater. Correlation spectrometer (COSPEC) measurements detected an elevated SO2 emission rate of 2,300 t/d. Seismicity also remained elevated. Ground deformation measured on the N flank continued to indicate tilting. Over the next week, activity remained high. Crater glow, however, was weak, and only visible from a distance with a telescope.. There was relatively little seismicity, slight inflation, occasional observations of incandescence at the summit, and a moderate amount of steam emission. SO2 flux remained well above the baseline of 500 metric tons per day (t/d) (table 7). SO2 emission rates reflected continued degassing of cooling magma, and ground-deformation data continued to indicate the absence of magma intrusion. On 21 August the Alert Level was lowered to 3 and, following a continued decrease in activity, on 19 October it was lowered to 1.
On 10 August 2008 an explosion and resulting ash plume followed weeks of increased activity and summit incandescence (BGVN 34:02). According to a Philippine Information Agency (PIA) Daily News Reader press release, the 10 August eruption was followed by an M 5.8 earthquake on 15 August and a series of aftershocks that continued through at least 20 August.. On the evening of 12 September 2004 the very faint glow at the summit of Mayon intensified slightly. The brighter incandescence, observable from Lignon Hill Volcano Observatory and in Legaspi City proper, coincided with a slight increase in the overall background tremor detected by seismographs around the volcano. However, there were no significant changes in ground deformation or SO2 measurements. A news report also noted that volcanic material emitted from the crater that day set fire to grass on the volcano's slopes.Brief periods of weak fountaining and lava flows were observed during 7-24 March. The fountaining generated dark gray ash plumes that rose 100-300 m above the summit crater before drifting SW, and were sometimes audible more than 10 km from the summit crater. At night, lava flows continued moving downslope within 3.3, 4.5, and 1.9 km of the crater in the Mi-isi, Bonga, and Basud gullies. Steam plumes rose as high as 2.5 km above the summit before drifting SW on 7 March. Intermittent bluish steam-laden plumes rose to 700 m before drifting SW on 14 March. A slight inflation of the lower flanks beginning on 11 March 2018 was recorded by electronic tiltmeters through at least 22 March. Overall deformation data indicated that the edifice was still inflated relative to pre-eruption baselines. Mayon Volcano remains on Level 4 alert. As of 5 February, 86,000 people are affected, with 65,000 people staying in 59 evacuation centres. The Mayon seismic monitoring network recorded 108 volcanic related earthquakes as of 11 February that resulted in lava fountains Further Reference. Sawada, Y., 1987, Study on analysis of volcanic eruption cloud image data obtained by the Geostationary meteorological Satellite (GMS): Technical Reports of the Meteorological Research institute (Japan), no. 22, 335 p.
05/2019 (BGVN 44:05) Intermittent ash emissions; persistent summit incandescence, October 2018-April 2019Following a quiet interval that started at 1420 on 26 February, more vigorous activity resumed on the evening of the 27th. Seven ash-and-gas explosions occurred between 1950 and 2237, the most significant of which (at 2144 and 2237) were accompanied by lava fountaining with ejection of volcanic bombs. Large incandescent fragments were ejected to ~500 m above the crater rim. Ground deformation measurements showed that the edifice remained inflated. COSPEC readings of SO2 flux remained significantly above normal at 4,900 t/d. Explosion earthquakes and harmonic tremor accompanied the lava fountaining and persisted even when the activity had apparently subsided.
Mayon is a frequently active volcano in the Philippines that produces ash plumes, lava flows, pyroclastic flows, and lahars. In early 2018, eruptive activity included lava fountaining that reached 700 m above the summit, and lava flows that traveled down the flanks and collapsed to produce pyroclastic flows (figure 39). Lava fountaining and lava flows decreased then ceased towards late March. Lava effusion was last detected on 18 March 2018, and the last pyroclastic flow for this eruptive episode occurred on 27 March 2018 (see BVGN 43:04). The hazard status for was lowered from alert level 4 to 3 (on a scale of 0 to 5) on 6 March 2018 due to decreased seismicity and degassing; the level was lowered again to 2 on 29 March. This report summarizes the activity during April through September 2018 and is based on daily bulletins issued by the Philippine Institute of Volcanology and Seismology (PHIVOLCS) and satellite data.At 1658 on 22 June Mayon emitted an ash column that rose 7-10 km above the vent (figure 8). The emission was recorded by the seismic network of the Philippines Institute of Volcanology and Seismology (PHIVOLCS) as an explosion that lasted for 10 minutes. No volcanic earthquakes nor other visible signs of abnormal activity were observed before the explosion. During May, however, low-frequency volcanic earthquakes had been recorded intermittently, accompanied by faint crater glow.What worried the volcanologists was the accumulated mud which could cascade down the volcano's side in the event of strong rains. Because of the threat of mudflows, they urged the safety measures remain in effect.Colima - info - webcamIztaccihuatl & Popocatépetl - Iztaccihuatl info - webcamMichoacán-Guanajuato Volcanic Field - info - one | twoPico de Orizaba - info - webcamPopocatépetl - info - webcam: Altzomoni Tlamacas | Tlamacas | Tianguismanalco | four
Information Contacts: Philippine Institute of Volcanology and Seismology (PHIVOLCS); Associated Press (URL: http://www.ap.org/); Daily Mail (URL: http://www.dailymail.co.uk); NOAA (URL: http://www.aoml.noaa.gov); and Philippine Daily Inquirer (URL: http://www.inquirer.net/). The article said that (according to Bernardo Rafaelito Alejandro, head of the Office of Civil Defense in Bicol) the foreign nationals and their guide were about half a kilometer from the crater when the 0800 explosion occurred. Another group, consisting of about seven climbers on another trail suffered three injuries (all Indonesians). Other articles raised sometimes inconsistent details about the number, composure, and locations of the various groups on the volcano.
Mayon volcano is a beautifully symmetrical volcano with a steep upper slope of 35-40° and is capped by a small summit crater 200 m in diameter. Mayon eruptions produce lava flows, pyroclastic flows and mud flows which threaten populations at the base of the volcano. A 6 km radius permanent danger.. PHIVOLCS reported that during 23-29 May white steam plumes from Mayon drifted WNW, WSW, and SW, sometimes rising 250-300 m above the crater rim. Crater incandescence was visible each night. The Alert Level remained at 2 (on a 0-5 scale) and PHIVOLCS reminded residents to stay away from the 6-km-radius Permanent Danger Zone and the 7-km Extended Danger Zone on the SSW and ENE flanks. Copyright Ⓒ 2016 Tahiti Airport Motel. © 2016 - By CREA PASSION - Créateur de sites web touristiques à Tahiti. Live Cam 1. Live Cam 2. Information importante. Circonstances exceptionnelles liées au Coronavirus
A level 4 alert means Mt Mayon is active, with persistent tremors, low-frequency type earthquake. But a level 5 alert signifies a hazardous eruption is underway.Japan - The Japanese Meteorological Agency has a page of 40+ webcams, but the names are all in Japanese. Google Translate does a good job of translating the names of volcanoes in the table on the right-hand side of the page to find your volcano of choice. However, they don't allow direct links to the webcams, so the Japanese volcano webcams listed below are in addition to those on the JMA website. [R3cam] Mobile Cam 3. [MUcam] Mauna Ulu Cam. [HPcam] Holei Pali from Holei Pali. Kīlauea Volcano, Lower East Rift Zone. [PGcam] Fissures in Leilani Estates from Puʻu Honuaula. [L1cam] Alaʻili Steaming Activity from ʻĪʻīlewa Crater. Mauna Loa Volcano, South Caldera Another series of ash ejections began at 1211 on 29 February. The largest event occurred at 1501 and produced a 14-km-high eruption column. This event also generated several pyroclastic flows that descended all sides of the volcano. Pyroclastic flows that were channeled by gullies in the SW, S, and SE reached up to 5-6 km from the summit. Smaller pyroclastic flows that followed gullies in other sectors stopped ~2-3 km from the crater. Ash from the tall eruption column and from pyroclastic flows drifted to the W and SW. The ash ejections were generally accompanied by rumbling sounds. Vigorous lava fountaining began at 1531 and ballistic projectiles fell within 1.5 km of the crater. Lava flows were observed on 1 March to have reached the 1,000 m elevation, or about 2.3 km from the summit.According to a news article, the Albay Province Public Safety and Emergency Management Office stated that more than 54,000 people were in evacuation shelters as of 30 September. On 12 October the Office of the Governor of Albay issued a statement noting that 12,602 families (about 56,000 people) had been relocated to 46 evacuation centers.
The following report was received [on] 16 October 1968. "16 October 0800 Z Mayon exhibited marked increase seismic activity admidst down rushing of mudflows. Mudflows triggered by intermittent heavy rains seem to have affected all sectors around volcano yesterday afternoon. Initial OMCC report indicated that all known critical areas in the SW, S, and SE sectors hit again. There's something truly captivating about seeing a volcano spurt out oozing lava during the night. It's one of those few times that you could really feel like the earth is alive and animated. It's my first time to see the famous Mayon Volcano here in Albay and it's such a sight to see it like this The PHIVOLCS reported that volcanic activity remained high at Mayon. Abundant low-frequency volcanic earthquakes associated with dome growth took place on 7, 8, 9, 11, and 12 February and consisted of 29, 30, 29, 45, and 30 events, respectively. Also on 12 February seismometers detected 2 rockfalls. The crater emitted voluminous steam and sulfur, with a maximum of ~7,100 metric tons of SO2 detected on 12 February. Tiltmeters on the volcano's N flank continued to detect slight edifice inflation. On 11 February, PHIVOLCS reported that most of the springs in the E and S quadrants of the volcano showed a decrease in discharge, despite increasing rainfall. Inclement weather prevented observations of the volcano. Mayon remained at Alert Level 3 (on a scale of 0-5).A 21 November 2009 article from Vox Bikol confirmed that as of 17 November, Mayon continued to exhibit summit incandescence and emit fluctuating amounts of SO2. Due to the continuing unrest PHIVOLCS installed additional seismic monitoring equipment, including three sets of broadband instruments from the Japan International Cooperating Agency (JICA).On 21 June lavas were seen exiting from two points of the dome. Two lobes descended, both on the SE side (in the general direction of the settlements of Buyuan and Mabinit). Magma ascent through the uppermost levels of the volcano's conduit appeared to be associated with high-frequency harmonic tremor at all five seismic stations in the vicinity of the volcano. Magma intruding the summit area also exerted pressure on the edifice and influenced ground tiltmeters. The COSPEC instrument measured the highest SO2 flux of the June episode: ~9,000 t/d.