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Three earthquakes in a 30 minutes period. Minor damages in households. Many people spent the night out in the street. [6] 2021-01-23 Granada, Andalusia: 4.2 M w IV 1 Minor damage/Part of an earthquake swarm [7] [8] 2016-01-25: Alboran Sea: 6.3 M w: VI 1 30+ Moderate damage [9] 2011-05-11: Lorca, Murcia: 5.1 M w: VIII 9 403 Damage to a ...
Disastrous floods have been reported throughout the history of Valencia, from the 14th century up to the contemporary period. [5] The 1957 Valencia flood was caused by a three-day cold drop (Spanish: gota fría) (which usually leads to heavy autumn rains in Spain and France); it overflowed the banks of the Túria river and devastated the city of Valencia.
Valencia flood may refer to two severe floods in Valencia, Spain: 1957 Valencia flood; 2024 Spain floods This page was last edited on 6 ...
Blue dots on a map circulating widely on social media show weirs that are still in place, not dams removed before Valencia flooding.
A pie chart comparing the seismic moment release of the three largest earthquakes for the hundred-year period from 1906 to 2005 with that for all earthquakes of magnitudes <6, 6 to 7, 7 to 8, and >8 for the same period. The 2011 Japan quake would be roughly similar to Sumatra. Earthquakes of magnitude 8.0 and greater from 1900 to 2018.
The earthquake also triggered the world's biggest nuclear disaster since Chernobyl in 1986. 22 February 2011. New Zealand. A 6.3 magnitude earthquake hit Christchurch, killing at least 180 people.
Historical earthquakes is a list of significant earthquakes known to have occurred prior to the early 20th century. As the events listed here occurred before routine instrumental recordings — later followed by seismotomography imaging technique, [1] observations using space satellites from outer space, [2] artificial intelligence (AI)-based earthquake warning systems [3] — they rely mainly ...
The ISC-GEM Global Instrumental Earthquake Catalogue (1900-2013) (prepared at the request of the GEM Foundation) catalogs magnitude 5.5 or greater earthquakes suitable for modeling and assessing seismic hazard and risk. Epicentral locations and hypocentral depths were recalculated from original travel time data using a consistent velocity model.