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JAKARTA (Reuters) -A magnitude 7.3 earthquake struck west of Indonesia's Sumatra Island on Tuesday, Indonesia's geophysics agency (BMKG) said, triggering a tsunami warning for around two hours.
Earthquakes in East Timor are frequent but rarely cause damage. ... Maluku, Indonesia: 5.6 M w VI Minor damage [3] 2021-12-11 Maluku, Indonesia: 5.4 M w VI
Large numbers of earthquakes of smaller magnitude occur very regularly due to the meeting of major tectonic plates in the region. Based on the records of the USGS, Indonesia has had more than 150 earthquakes with magnitude > 7 in the period 1901–2019.
The earthquake was the largest in the region since a deep-focus M w 7.9 struck in 1996. [8] The shaking was reportedly most intense on the Selayar Islands, reaching a maximum Modified Mercalli intensity of VI (Strong) according to the Meteorology, Climatology, and Geophysical Agency (BMKG). [2] The earthquake was also felt V in Ranakah. [9]
The subduction zone produced two destructive earthquakes and tsunamis in 2006 and 1994. An intraslab earthquake in 2009 also caused severe destruction. [5] Compared to the highly oblique convergence across the plate boundary in Sumatra, near Java, it is close to orthogonal. However, there is still a small component of left-lateral strike-slip ...
Fatalities occurred in every month of the year. Earthquake activity was lowest in June, while August was the most active and deadliest month. Major events also took place in Indonesia, Japan, China, Pakistan, Mexico and Peru. A M 7.3 quake in China was the most intense event of the year (MMI X, Extreme).
Up to 66,900 people died from earthquakes in 2023, the highest death toll for earthquakes since 2010. At least 59,488 people died in the Turkey–Syria doublets of February, which dominated world headlines because of its extensive devastation; the first mainshock was also the largest earthquake of the year at M w 7.8.
Sulawesi lies within the complex zone of interaction between the Australian, Pacific, Philippine and Sunda plates in which many small microplates are developed. The main active structure onshore in the western part of Central Sulawesi is the left-lateral NNW-SSE Palu-Koro strike-slip fault that forms the boundary between the North Sula and Makassar blocks.