and an independent earthquake, even though this last one is very likely to have been triggered by the swarm activity. October 15, 2020, an earthquake swarm occurred on Philippine Island of Panay ranging Magnitude 2.5-4.5. Most of these quakes felt in Iloilo City. The last earthquake swarm also hit Panay island on November 5, 2018 (Including Antique, Iloilo and Guimaras) ranging Magnitude 4.0-4.8. The First earthquake (Magnitude 4.7) at 7:45 A.M, occurred at San Jose Antique. Just a few minutes after, the second quake (Magnitude 4.0) occurred at Sibunag Guimaras. At 10:54 A.M, The third quake (Magnitude 4.8) Occurred at Guimbal Iloilo, Intensity 4 was felt in Iloilo City A series of earthquakes that hit Mindanao in 2019 were classified as an earthquake swarm.On October 16 2019, a Magnitude 6.3 (Mwp) Struck Tulunan cotabato (Epicenter of earthquake). Intensity VII was felt in Tulunan, M'lang, Makilala and Kidapawan City, Cotabato. Intensity VI was felt in Digos City, Davao del Sur; Sto. Nino, South Cotabato; Tacurong City, Sultan Kudarat. On October 29 2019, a Magnitude 6.6 (Mww) struck Tulunan Cotabato again. At least ten deaths were reported and four hundred individuals were injured. Intensity VII was recorded in Tulunan and Makilala, Cotabato; Kidapawan City; Digos City, Bansalan, Magsaysay, Davao del Sur and Malungon, Sarangani. Intensity VI was recorded in Koronadal City and Davao City. Just 2 days after on October 31 2019, an earthquake struck Tulunan Cotabato again (Magnitude 6.5Mww) The death toll of two quakes was raised into 24 and 563 were injured and 11 are still missing. Eva's Hotel in Kidapawan City collapsed during the quake October 14-18 2021 an earthquake swarm occurred on Camarines Sur ranging Magnitude 1.7-4.3 with the depth of 1–40 km. Some of these events were felt on Camarines Norte and Albay. PHIVOLCS recorded at least 27 earthquakes (10 were felt) in Camarines Sur. Europe Czech Republic / Germany The western Bohemia/Vogtland region is the border area between the Czech Republic and Germany where earthquake swarms were first studied at the end of the 19th century. Swarm activity is recurrent there, sometimes with large maximum magnitudes, as for instance in 1908 (maximum magnitude 5.0), 1985–1986 (4.6), 2000 (3.2), or 2008 (3.8). This latter swarm occurred near Nový Kostel in October 2008 and lasted only 4 weeks, but up to 25,000 events were detected by WEBNET, the local monitoring network. The swarm is located on a steeply-dipping