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Earthquake

Most severe and most recent earthquakes

Earthquakes occur naturally in the lithosphere, the outer rock layers of the earth. Like volcanoes and tsunamis, they occur mainly at the edges of tectonic plates. The countries bordering the Pacific, but also in Central Asia, are most clearly affected.

On further pages:
Volcanoes
Tsunamis
Tropical storms

Earthquakes today

The map and table below list all earthquakes of the last 24 hours that had a magnitude of at least 2.5 on the Richter scale and were located near inhabited areas. Quakes on the open sea are therefore not included here. The times given refer to the coordinated universal time UTC.

We update this page up to 6 times a day. We expect the next update around 14:00 UTC.

TimeRegionMagnitude
05:07Puerto Rico24 km east of Ponce2.6
03:40Puerto Rico42 km southeast of San Juan2.6
03:35Peru97 km southwest of Minas de Marcona (Ica)4.6
23:38United States43 km southeast of Hilo (Hawaii)2.5
19:26Greece25 km southwest of Pátra (West Greece)4.3
18:55Peru91 km southwest of Minas de Marcona (Ica)4.8
18:51Taiwan16 km west of Hualian (Taiwan)4.4
18:19Peru59 km west of Chuquitira (Tacna)5.6
17:35Papua New Guinea24 km north of Kimbe (West New Britain)4.4
17:12Papua New Guinea98 km northeast of Rabaul (East New Britain)5.6

The strongest earthquakes in the last 2 weeks

DateRegionMagnitude
Thu 11thPhilippinesIn the Moro Gulf, 196 km south of Pagadian City.7.1
Fri 12thPeru23 km southeast of Acarí (Arequipa)5.7
Fri 12thPapua New Guinea98 km northeast of Rabaul (East New Britain)5.6
Fri 12thPeru59 km west of Chuquitira (Tacna)5.6
Sun 7thRussia77 km south-southwest of Ust’-Kamchatsk Staryy5.5
Sun 7thRussia76 km south-southwest of Ust’-Kamchatsk Staryy5.5
Sat 6thPhilippines72 km north of Claveria (Cagayan Valley)5.5
Thu 11thGuam120 km south-southwest of Merizo Village5.4
Mon 8thPeru95 km southwest of Minas de Marcona (Ica)5.4
Sat 13thJapan127 km south-southeast of Itoman5.3

How earthquakes occur

Tectonic plate boundaries The Earth is not a solid sphere of stone, but consists of different layers with different densities and temperatures. The outermost layer is the Earth's crust and consists of brittle rock masses that float on the Earth's mantle below. Both layers together form the lithosphere. The heat in the Earth's mantle causes a slow but steady movement in which hot and therefore viscous and malleable rock masses slowly rise from the Earth's interior, cool down again and sink once more. These movements are transferred to the continental plates that make up the Earth's outer crust. In the course of many millions of years, our continents drift further and further apart.

If two tectonic plates move towards each other, they fold up at the edges and whole mountain ranges are formed over a long period of time. However, most of these plate boundaries do not run on land, but under water in the oceans. Such huge continental plates do not move at a constant speed. Unlike the deeper layers of the Earth, they are much cooler and therefore firmer. This creates great stresses, which at some point become so great that massive layers of rock break. The resulting jerky discharge of stress generates seismic waves over many kilometers. This is known as earthquakes at the surface.

While the Earth's crust is between 8 and 70 kilometers thick, most earthquakes occur at a depth of 20 to 50 kilometers. That is, where the rock plates are no longer hot enough to deform. The place where the Earth's crust first breaks open is called the hypocenter. The travel time of the seismic waves to different measuring stations often makes it possible to determine this very precisely. The term epicenter describes the location on the Earth's surface above the hypocenter.

The map on the right (source: NASA, DTAM project team) shows the most frequent epicenters of earthquakes, regardless of their magnitude, and thus illustrates the boundaries of the continental plates. In particular, earthquakes occur with striking frequency along the U.S. West Coast and along the Pacific Ring of Fire.

The most severe earthquakes since 1950

Chile, Alaska (USA) and Indonesia appear several times in the list of the most severe earthquakes over the last 60 years. The total damage column includes destroyed homes and financial losses. It does not include victims and damage from tsunamis possibly triggered by the quakes.
Date CountryRegionMagnitudeDeathsTotal damage
05/22/1960Chile
05/22/1960: Puerto Montt, Valdivia
Puerto Montt, Valdivia9.52,000
03/28/1964United States
03/28/1964: Alaska
Alaska9.215
03/11/2011Japan
03/11/2011: Honshu
Honshu9.11,475
12/26/2004Indonesia
12/26/2004: Sumatra (Aceh: Off West Coast)
Sumatra (Aceh: Off West Coast)9.11,001
11/04/1952Russia
11/04/1952: Kamchatka Peninsula
Kamchatka Peninsula9.00
02/27/2010Chile
02/27/2010: Maule, Concepcion, Talcahuano
Maule, Concepcion, Talcahuano8.8402
02/04/1965United States
02/04/1965: Aleutian Islands (Rat Islands)
Aleutian Islands (Rat Islands)8.70
03/28/2005Indonesia
03/28/2005: Sumatera (Sw)
Sumatera (Sw)8.61,303
08/15/1950India
08/15/1950: India-China
India-China8.61,530
04/11/2012Indonesia
04/11/2012: N Sumatra (Off West Coast)
N Sumatra (Off West Coast)8.610
03/09/1957United States
03/09/1957: Alaska
Alaska8.60
10/13/1963Russia
10/13/1963: Kuril Islands
Kuril Islands8.50
06/23/2001Peru
06/23/2001: Arequipa, Moquegua, Tacna, Ayacucho
Arequipa, Moquegua, Tacna, Ayacucho8.477
09/12/2007Indonesia
09/12/2007: Sumatra
Sumatra8.425
09/16/2015Chile
09/16/2015: Central
Central8.37
10/04/1994Russia
10/04/1994: Kuril Islands; Japan (Hokkaido)
Kuril Islands; Japan (Hokkaido)8.311
09/25/2003Japan
09/25/2003: Hokkaido
Hokkaido8.30
11/06/1958Russia
11/06/1958: Kuril Islands
Kuril Islands8.30
11/04/1963Indonesia
11/04/1963: Banda Sea
Banda Sea8.30
11/15/2006Russia
11/15/2006: Kuril Islands
Kuril Islands8.30


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