Vulkan-Monitor
In einer Tiefe ab 100 km, ist es zwischen 1000 und 1300 Grad Celsius heiß. Gestein beginnt zu schmelzen und sammelt sich in großen, tropfenförmigen Magmaherden in 2 bis 50 km Tiefe. Wenn der Druck zu groß wird, steigt das Magma über Spalten und Klüfte an die Oberfläche: Ein Vulkan entsteht.Augenblicklich aktive Vulkane:
Mayon (Philippines) - Report for 30 April-6 May 2026 - New Eruptive Activity
Datum: Thu, 07 May 2026 04:12:12 -0400
Beschreibung:
The Philippine Institute of Volcanology and Seismology (PHIVOLCS) reported that the eruption at Mayon continued during 29 April-6 May, with a notable pyroclastic density current (PDC) from collapse events on 2 May. The activity in general was characterized by lava effusion, pyroclastic density currents (PDCs), incandescent rockfalls, ash-and-gas plumes, and occasional minor Strombolian activity. Emissions were visible daily, rising as high as 1 km above the summit and drifting mainly SW, W, and WNW. Each day the seismic network recorded 221-411 rockfalls, 0-4 PDCs, and 5-45 volcanic earthquakes. The earthquake counts included 4-25 daily periods of volcanic tremor, each lasting between one minute to just over one hour. Sulfur dioxide emissions averaged 1,586-2,087 tonnes per day. The lava flows did not advance in the Basud (E) and Bonga (SE) drainages, remaining 3.8 and 3.2 km long, respectively. Minor Strombolian activity and short periods of lava fountaining were recorded during 29 April-2 May. Two long sequences of PDCs from collapses occurred in the Mi-isi drainage on the SW flank on 2 May. The first sequence began at 1628 and lasted 39 minutes, followed by a more intense sequence with more frequent and larger PDCs that began at 1709 and lasted 95 minutes. Dense weather clouds obscured the upper half of the volcano. Most of the stations in the seismic network recorded broadband tremor, a volcanic earthquake signal that typically accompanies large-volume lava flow effusion and associated lava collapses; no explosions were recorded. The first sequence was characterized as at least seven small-volume PDCs that traveled 2-3 km and produced brownish-gray convecting ash clouds. The second sequence consisted of at least 22 PDC events, including some of the largest in the 2026 eruption so far. By 1730 more voluminous PDCs were observed descending the Mi-isi drainage as far as 4 km. These were followed by a rapid succession of PDCs that traveled more than 5 km down the flanks and generated darker ash clouds that drifted W; a PDC recorded at 1750 was the most voluminous and reached the greatest distance. Photos posted on social media showed an enormous dark ash cloud, that had accumulated from multiple PDCs, rising 5 km above the length of the deposits; after the cloud detached from the PDC it continued to move downslope as an ash curtain. Ashfall occurred across a narrow swath W of the volcano. Analysis of photos and drone images after this activity on 2 May showed that two short lava flows and part of a longer lava flow were gone, and the upper 2 km of the Mi-isi drainage was described as a deep gully. PDC deposits had filled in and spilled over the banks of the Mi-isi-Binaan channel about 4.8 km down from the summit, at around 400 m elevation, forming a deposit several meters higher than the channel banks with a lobate sloping terminus. On 3 May the Office of Civil Defense (OCD) reported that the barangays (neighborhoods) in Guinobatan, Camalig, and Ligao City (Albay) were most impacted by ashfall which lasted for about three hours. Residents reported low to no visibility in some areas due to ash in the air, and that the ashfall impacted crops, animals, and farmlands. The main roads were cleared by local authorities and firefighters by 3 May, and residents had begun clearing ash from their homes and vehicles. The OCD and other organizations distributed N95 masks, hygiene packs and necessities, food, and bottled water for communities where water sources may had been contaminated by ashfall. PHIVOLCS noted that as of 4 May there were four cities/municipalities and 109 barangays that had experienced ashfall, based on reports collected from local government officials, Disaster Risk Reduction (DRR) partners, and the PHIVOLCS Quick Response Team (QRT). In 21 barangays of Ligao City there was either trace amounts of ashfall or observable ashfall, reported as far as in Maonon (40 km SW). In Camalig ashfall was moderate to heavy in 17 barangays with the thickest deposit, 15 mm, observed in Tumpa (7 km SW); residents in barangay Ligban (10 km SSW) observed only minor ashfall. In Guinobatan ashfall was observed in 23 barangays, ranging from minimal to heavy. Residents of Doña Tomasa (7 km WSW), San Rafael (11 km SW), Muladbucad Pequeño (7 km W), and Travesia (10 km SW) reported periods of zero visibility. Residents in 53 barangays of Oas reported observable ashfall. Smaller-volume PDCs from collapses in the Mi-isi drainage periodically continued through the rest of the week. The most significant of these occurred during 0719-0726 on 5 May, traveling 3 km down the Mi-isi drainage and producing ash plumes that rose 1.9 km above the summit. New lava flows were active in the Mi-isi drainage and filled up the gully during 4-6 May. According to the Disaster Response Operations Monitoring and Information Center (DROMIC) report the number of residents that went to evacuation shelters increased after the 2 May event. By 1800 on 30 April a total of 4,022 people (1,105 families) were staying in 12 evacuation shelters and by 1800 on 3 May the numbers increased to 5,459 people (1,444 families) staying in 14 shelters; those numbers dropped to 4,905 people (1,362 families) during 4-5 May and two shelters were no longer in use. The number of individuals and families staying with friends or relatives did not change. The ongoing eruption continued to affect tens of thousands of people across the Albay province; by 1800 on 6 May the DROMIC report stated that a total of 286,939 people (70,150 families) across 160 barangays in Region V had been impacted by volcanic activity at Mayon. The Alert Level remained at 3 (on a 0-5 scale) and residents were reminded to stay away from the 6-km-radius Permanent Danger Zone (PDZ). PHIVOLCS recommended that civil aviation authorities advise pilots to avoid flying close to the summit.
Sources: Disaster Response Operations Monitoring and Information Center (DROMIC),Philippine Institute of Volcanology and Seismology (PHIVOLCS) ,Philippine News Agency (PNA)
Aira (Japan) - Report for 30 April-6 May 2026 - Continuing Eruptive Activity
Datum: Thu, 07 May 2026 04:12:12 -0400
Beschreibung:
The Japan Meteorological Agency (JMA) reported ongoing eruptive activity at Minamidake Crater (Aira Caldera?s Sakurajima volcano) during 27 April-4 May. Very small eruptive events were periodically detected. Crater incandescence was visible in nighttime webcam images during 1-4 May. The Alert Level remained at 3 (on a 5-level scale), and the public was warned to be cautious within 2 km of both the Minimadake and Showa craters.
Source: Japan Meteorological Agency (JMA)
Ambae (Vanuatu) - Report for 30 April-6 May 2026 - Continuing Eruptive Activity
Datum: Thu, 07 May 2026 04:12:12 -0400
Beschreibung:
On 1 May the Vanuatu Meteorology and Geohazards Department (VMGD) reported that the eruption at Ambae was ongoing and characterized as minor. Seismicity remained at high levels with the detection of continuous volcanic tremor and volcanic-seismic events. Sulfur dioxide emissions were detected in satellite images on 30 April and thermal anomalies with variable intensities were identified in satellite images on 1 May. Photos from 1300 on 1 May showed emissions of steam, gas, and ash rising high above the crater rim. Continuous summit incandescence was also visible in photos. According to the Wellington Volcanic Ash Advisory Center (VAAC) a small ash plume rose 3 km (10,000 ft) a.s.l. and drifted NW on 6 May. The Alert Level remained at 3 (on a scale of 0-5), and the public was warned to stay outside of Danger Zone B, defined as a 3-km radius around the active vents in Lake Voui, and to stay away from drainages during heavy rains.
Sources: Vanuatu Meteorology and Geohazards Department (VMGD),Wellington Volcanic Ash Advisory Center (VAAC)
Awu (Indonesia) - Report for 30 April-6 May 2026 - Continuing Unrest
Datum: Thu, 07 May 2026 04:12:12 -0400
Beschreibung:
The Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG) reported that seismicity at Awu had increased. The seismic network recorded a total of 74 earthquakes on 4 May, many of which were shallow volcanic earthquakes. During 0000-1200 on 5 May the network recorded 15 shallow volcanic earthquakes and two deep volcanic earthquakes. Low-frequency earthquakes associated with fluid movement had not been detected, and diffuse white plumes were rising at most 200 m above the lava dome. The Alert Level remained at 2 (on a scale of 1-4) and the public was warned to stay 3 km away from the crater?s center.
Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM)
Dukono (Indonesia) - Report for 30 April-6 May 2026 - Continuing Eruptive Activity
Datum: Thu, 07 May 2026 04:12:12 -0400
Beschreibung:
The Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG) reported that eruptive activity at Dukono continued during 30 April-6 May. Daily white-and-gray ash plumes rose 400-2,000 m above the summit and drifted in multiple directions. The Alert Level remained at Level 2 (on a scale of 1-4) and the public was warned to stay 4 km away from the Malupang Warirang Crater.
Source: Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG, also known as CVGHM)
In Deutschland gibt es momentan keine aktiven Vulkane. Der Vulkanismus in Deutschland in den verangengen Jahrentausenden bzw. Jahrmillionen wurde durch Hebung der Alpen verursacht. Dass dieser Prozess noch nicht abgeschlossen ist, zeigen kleinere Erdbeben vom Rheingraben bis zur Kölner Bucht. Die Vulkane, die es in Deutschland gibt spucken zwar zur Zeit keine Lava aus, aber es gibt in Deutschland an vielen Orten heiße Quellen. Diese Thermalquellen sind ein Zeichen dafür, dass Wasser im inneren der Erde erwärmt wird. Vulkanaktivitäten aus vergangenen Zeiten sieht man in Deutschland z.B. auch am Kaiserstuhl in der oberrheinischen Ebene und am Rand der Schwäbischen Alp.
