2010 Pacaya | |
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| Total costs | N/A |
| Deaths | 3 |
Pacaya is an active complex volcano in Guatemala, which first erupted approximately 23,000 years ago and has erupted at least 23 times since the Spanish conquest of Guatemala. It rises to an elevation of 2,552 metres (8,373 ft). After being dormant for over 70 years, it began erupting vigorously in 1961 and has been erupting frequently since then. Much of its activity is Strombolian, but occasional Plinian eruptions also occur, sometimes showering the area of the nearby Departments with ash.Pacaya is a popular tourist attraction. It is even the home to the popular Guatemala Impact Marathon which pioneered the use of a running route across the lava field created by the 2010 eruption and supports the local communities through runners endeavouring to complete the challenge. It lies 30 kilometers (19 miles) southwest of Guatemala City and close to Antigua. The volcano sits inside the Escuintla Department.Villagers near Pacaya ignored an evacuation request as the volcano threw ashes into the air in March 2021.
Source: Wikipedia 1960 Agadir earthquake | |
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| Total costs | N/A |
| Deaths | 12000 |
The 1960 Agadir earthquake occurred 29 February at 23:40 Western European Time near the city of Agadir, located in western Morocco on the shore of the Atlantic Ocean. Despite the earthquake's moderate Mw scale magnitude of 5.8, its relatively shallow depth (15.0 km) resulted in strong surface shaking, with a maximum perceived intensity of X (Extreme) on the Mercalli intensity scale. Between 12,000 and 15,000 people (about a third of the city's population of the time) were killed and another 12,000 injured with at least 35,000 people left homeless, making it the most destructive and deadliest earthquake in Moroccan history. Particularly hard hit were Founti, the Kasbah, Yachech (iḥšaš) and the Talbordjt area. The earthquake's shallow focus, close proximity to the port city of Agadir, and unsatisfactory construction methods were all reasons declared by earthquake engineers and seismologists as to why it was so destructive.
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