Showing posts with label Arabian Plate. Show all posts
Showing posts with label Arabian Plate. Show all posts

Saturday, 1 November 2025

Magnitude 6.0 Earthquake in Balıkesir Province, Turkey.

The United States Geological Survey recorded a Magnitude 6.0 Earthquake at a depth of 8.0 km, about 4 km to the southeast of the municipality of Sındırgı in Balıkesir Province, Turkey,  slightly before 10.,50 pm local time (slightly before 7.50 pm GMT) on Monday 27 October 2025. No casualties have been reported following this event, but several buildings damaged during another Earthquake in August are reported to have collapsed. The Earthquake was felt across western Turkey, and in parts of southern Bulgaria.

The approximate location of the 27 October 2025 Balıkesir Province Earthquake. USGS.

Balıkesir Province lies close to the boundary between the Anatolian Plate, to the north, the Aegean Sea Plate (underlying the Peloponnese, Attica, The Cyclades Islands, Crete, the Dodecanese Islands and Turkey to the southeast of the Taurus Mountains) to the west and the African Plate to the south. Northern Greece and the north coast of Turkey lie on the Eurasian Plate. Both countries are highly prone to earthquakes because of this.

To the east the Arabian Plate  is being pushed north and west by the movement of the African Plate, further to the south. This leads to a zone of tectonic activity within the province, as the Arabian and Anatolian plates are pushed together, along the East Anatolian Fault, and past one-another, along the Dead Sea Transform.

Simplified map of the plate movements of the eastern Mediterranean. Univeriteit Utrecht.

This movement also leads to a zone of faulting along the northern part of Turkey, the North Anatolian Fault Zone, as the Anatolian Plate is pushed past the Eurasian Plate, which underlies the Black Sea and Crimean Peninsula  (transform faulting). This is not a simple process, as the two plates constantly stick together, then break apart as the pressure builds up, leading to Earthquakes, which can be some distance from the actual fault zone. 

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Wednesday, 13 August 2025

At least one fatality following Magnitude 6.1 Earthquake in eastern Turkey.

The United States Geological Survey recorded a Magnitude 6.1 Earthquake at a depth of 10.0 km, about 10 km to the southwest of the municipality of Bigadiç in Balıkesir Province, Turkey,  slightly before 7.55 pm local time (slightly before 4.55 pm GMT) on Sunday 10 August 2025. Sixteen buildings are reported to have collapsed following the event, although the majority are reported to have been derelict before the event, with at least one fatality, an 81-year-old woman who died after being rescued from the remains of a collapsed building, with 29 more people having been injured.

Local residents removing debris from collapsed buildings following an Earthquake in northeast Turkey on 10 August 2025. Bahadir Demirçeriven/AP.

Balıkesir Province lies close to the boundary between the Anatolian Plate, to the north, the Aegean Sea Plate (underlying the Peloponnese, Attica, The Cyclades Islands, Crete, the Dodecanese Islands and Turkey to the southeast of the Taurus Mountains) to the west and the African Plate to the south. Northern Greece and the north coast of Turkey lie on the Eurasian Plate. Both countries are highly prone to earthquakes because of this.

The approximate location of the 10 August 2020 Balıkesir Province Earthquake. USGS.

To the east the Arabian Plate  is being pushed north and west by the movement of the African Plate, further to the south. This leads to a zone of tectonic activity within the province, as the Arabian and Anatolian plates are pushed together, along the East Anatolian Fault, and past one-another, along the Dead Sea Transform.

Simplified map of the plate movements of the eastern Mediterranean. Univeriteit Utrecht.

This movement also leads to a zone of faulting along the northern part of Turkey, the North Anatolian Fault Zone, as the Anatolian Plate is pushed past the Eurasian Plate, which underlies the Black Sea and Crimean Peninsula  (transform faulting). This is not a simple process, as the two plates constantly stick together, then break apart as the pressure builds up, leading to Earthquakes, which can be some distance from the actual fault zone. 

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Tuesday, 4 July 2023

Magnitude 5.4 Earthquake off the northeast coast of Azerbaijan.

The United States Geological Survey recorded a Magnitude 5.4 Earthquake at a depth of 59.7 km off the northeast coast of Azerbaijan slightly after midnight local time on Tuesday 4 July 2023 (slightly 8.00 pm on Monday 4 July GMT). There are no reports of any damage or casualties associated with this event, but people have reported feeling it along the northeastern part of the coast of Azerbaijan, and adjacent parts of the Caspian Sea coast of Russia.

The approximate location of the 4 July 2023 Azerbaijan Earthquake. USGS.

Earthquakes are a common problem in Azerbaijan, which is located on the southern part of the Eurasian Plate, close to the boundary with the Arabian and Anatolian Plates. The Arabian Plate is being pushed northwards by the movement of the African Plate further to the south, pushing the Anatolian Plate to the west, and creating stress in the rocks around the Caspian Sea Basin, and creating the uplift that has led to the formation of the Caucasus Mountains.

The movement of the Arabian Plate into the Eurasian Plate from the south. El-Isa & Franke (2002).

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Tuesday, 7 February 2023

Number of dead now known to exceed 6000 following major Earthquakes in southeastern Turkey.

The number of people now known to have died following a pair of major Earthquakes in southeastern Turkey on Monday 6 February 2023 has now exceeded 6000, and is expected to rise further over the coming days. The first Earthquake struck slightly after 4.15 am local time (slightly after 1.15 am GMT), and was measured by the United States Geological Survey as a Magnitude 7.8 event at a depth of 17.9 km, 4 km to the east of the city of Nurdağı in Gaziantep Province. The second event was recorded as a Magnitude 7.5 event at a depth of 10.0 km, 4 km to the southeast of the town of Ekinözü in Kahramanmaraş Province. The two events were punctuated and followed by dozens of smaller Earthquakes, many with Magnitudes of 5.0 or greater.

The approximate location of the Magnitude 7.8 Earthquake which hit southeastern Turkey slightly after 4.15 am on Monday 6 February 2023. USGS.

The majority of the recorded fatalities s far have come from Turkey, where the number of confirmed dead had reached 3381 by 9.00 am local time on Tuesday 7 February, however it is thought that the final number of dead will be far higher in neighbouring Syria, where only 1444 fatalities had been recorded by the same time, but where infrastructure has been weakened by years of civil conflict, hampering rescue efforts. It is feared that the eventual death toll will exceed 20 000.

People search through rubble following an earthquake in Diyarbakir, Turkey, on 6 February 2023. Sertac Kayar/Reuters.

Around 380 000 people in Turkey have been rehomed in temporary shelters following the event, with reports of over 11 000 collapsed buildings, of which 5775 have been confirmed. Around 8000 people have been pulled alive from beneath collapsed buildings in Turkey, where about 23 million people across ten provinces are thought to have been affected by the event.

A man walks past collapsed buildings in Hatay, Turkey. Burak Kara/Getty Images.

Southeastern Turkey lies at the boundary between the Eurasian Plate to the north and east, the Anatolian Plate to the west and the Arabian Plate to the south. The Arabian Plate  is being pushed north and west by the movement of the African Plate, further to the south. This leads to a zone of tectonic activity within the province, as the Arabian and Anatolian plates are pushed together, along the East Anatolian Fault, and past one-another, along the Dead Sea Transform.

In Diyarbakir, north-east of Gaziantep, a search is now under way for people trapped in damaged buildings. Anadolu Agency/Getty Images.

This movement also leads to a zone of faulting along the northern part of Turkey, the North Anatolian Fault Zone, as the Anatolian Plate is pushed past the Eurasian Plate, which underlies the Black Sea and Crimean Peninsula  (transform faulting). This is not a simple process, as the two plates constantly stick together, then break apart as the pressure builds up, leading to Earthquakes, which can be some distance from the actual fault zone.

Plate movements and fault zones around the Anatolian Plate. Mike Norton/Wikimedia Commons.

The northward movement of the African and Arabian Plates also causes folding and uplift in the Caucasus Mountains, which separate Georgia from Russia. Again this is not a smooth process, with the rocks sticking together, then moving sharply as the pressure builds up enough to break them apart, which can also lead to Earthquakes in the region.

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Friday, 2 December 2022

Magnitude 5.7 Earthquake in Hormozgan Province, Iran.

The United States Geological Survey recorded a Magnitude 5.7 Earthquake at a depth of 4.7 km roughly 49 km to the northeast of the port of Bandar-e Lengeh in Hormozgan Province, Iran, slightly after 6.45 pm local time (slightly after 3.15 pm GMT) on Wednesday 30 November 2022. There are no reports of any damage or casualties associated with this event, but many people in the United Arab Emirates reported feeling it.

The location of the 30 November 2022 Hormozgan Province Earthquake. USGS.

Iran is situated on the southern margin of the Eurasian Plate. Immediately to the south lies the Arabian Plate, which is being pushed northward by the impact of Africa from the south. This has created a zone of faulting and fold mountains along the southwest coast of the country, known as the Zagros Thrust Belt, while to the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and creating frequent Earthquakes, some of which can be very large.

The movement of the Arabian Plate and extent of the Zagros Thrust Belt. Rasoul Sorkhabi/Geo ExPro.

The population of Iran is particularly at risk from Earthquakes as, unlike most other Earthquake-prone nations, very few buildings in the country are quake-resistant. The majority of residential buildings in Iran are made of mud-brick, a building material particularly vulnerable to Earthquakes as the bricks often liquefy, trapping people inside and quickly asphyxiating them with dust. This is particularly dangerous at night when the majority of people are inside sleeping.

Section through the Zagros Fold Belt. Sarkarinejad & Azizi (2007).

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Tuesday, 26 July 2022

Magnitude 5.4 Earthquake in Hormozgan Province, Iran.

The United States Geological Survey recorded a Magnitude 5.4 Earthquake at a depth of 10.0 km roughly 51 km to the northeast of the port of Bandar-e Lengeh in Hormozgan Province, Iran, slightly after 4.05 pm local time (slightly after 8.35 pm GMT) on Saturday 23 July 2022. There are no reports of any damage or casualties associated with this event, but many people in the United Arab Emirates reported feeling it.

The location of the 23 July 2022 Hormozgan Province Earthquake. USGS.

Iran is situated on the southern margin of the Eurasian Plate. Immediately to the south lies the Arabian Plate, which is being pushed northward by the impact of Africa from the south. This has created a zone of faulting and fold mountains along the southwest coast of the country, known as the Zagros Thrust Belt, while to the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and creating frequent Earthquakes, some of which can be very large.

The movement of the Arabian Plate and extent of the Zagros Thrust Belt. Rasoul Sorkhabi/Geo ExPro.

To the northeast of this the geology is dominated by three large tectonic blocks, the Central Iran, Lut and Helmand, which move separately in response to pressure from the south, stretching and compressing the rock layers close to the surface and again creating frequent Earthquakes.

The population of Iran is particularly at risk from Earthquakes as, unlike most other Earthquake-prone nations, very few buildings in the country are quake-resistant. The majority of residential buildings in Iran are made of mud-brick, a building material particularly vulnerable to Earthquakes as the bricks often liquefy, trapping people inside and quickly asphyxiating them with dust. This is particularly dangerous at night when the majority of people are inside sleeping.

Section through the Zagros Fold Belt. Sarkarinejad & Azizi (2007).

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