Strong and shallow M6.3 earthquake hits Turkey – Greece border region


A strong and shallow earthquake registered by the EMSC hit near the coast of western Turkey (Turkey – Greece border region) at 12:28 UTC on June 12, 2017. The agency is reporting a depth of 9 km (5.6 miles). USGS is reporting M6.3 at a depth of 10.4 km (6.4 miles).

According to the USGS, the epicenter was located 5 km (3.1 miles) S of Plomarion (population 2 996), Greece, 25.8 km (16 miles) SW Mytilini (population 28 322), Greece, 44.8 km (27.9 miles) NW of Foca (population 15 189), 48.2 km (29.9 miles) WSW of Dikili (population 14 125), 51.7 km (32.1 miles) SSW of Ayvalik (population 35 193), Turkey. This is about 87 km (54 miles) NW of Izmir (population 2 501 000), Turkey, according to the EMSC.

There are more than 2.5 million people living within 100 km (61 miles).

About 5 000 people are estimated to have felt very strong shaking (VII on Modified Mercalli Intensity Scale) and about 185 000 people strong (VI) shaking.

The mayor of Plomarion (5 km / 3.1 miles) N of the epicenter, said several old and new buildings have been damaged. 

Serious damage reports are coming from the island of Lesbos, Greece (see videos below). According to the GreekReporter, at least one person that was trapped in ruins on Lesbos was pulled out of the wreckage dead. There are reports, however, that another person remains trapped in the ruins of her home. Major damage has been reprted in the village of Vrisa of Polichnitos in southern Lesbos. "Half of the village has been greatly damaged and many houses have collapsed," said Nikos Karasavvas, the Deputy Mayor of Environment and Emergency of the Municipality of Lesbos.

At least 25 aftershocks were recorded, all below M5.0.

This is one of the strongest earthquakes the region has seen in the last 100 years.

Turkey Greece border region earthquake June 12, 2017 - ShakeMap

Yellow alert for shaking-related fatalities and economic losses. Some casualties and damage are possible and the impact should be relatively localized. Past yellow alerts have required a local or regional level response. Estimated economic losses are less than 1% of GDP of Greece.

Overall, the population in this region resides in structures that are vulnerable to earthquake shaking, though resistant structures exist. The predominant vulnerable building types are ductile reinforced concrete frame and reinforced/confined masonry construction.

Recent earthquakes in this area have caused secondary hazards such as landslides that might have contributed to losses.

Estimated population exposure to earthquake shaking

Turkey Greece border region earthquake June 12, 2017 - Estimated population exposure

Turkey Greece border region earthquake June 12, 2017 - Estimated population exposure - Table

Selected cities exposed

Turkey Greece border region earthquake June 12, 2017 - Selected cities exposed

Historic seismicity

Turkey Greece earthquake June 12, 2017 - Historical seismicity

Regional deadly earthquakes from 1500 to 2000

Western Turkey deadly earthquakes between 1500 and 2000

Source: T. Utsu; International Handbook of Earthquake and Engineering Seismology; vol. A; 691-718


Seismotectonics of the Mediterranean region and vicinity

The Mediterranean region is seismically active due to the northward convergence (4-10 mm/yr) of the African plate with respect to the Eurasian plate along a complex plate boundary. This convergence began approximately 50 Ma and was associated with the closure of the Tethys Sea. The modern day remnant of the Tethys Sea is the Mediterranean Sea. The highest rates of seismicity in the Mediterranean region are found along the Hellenic subduction zone of southern Greece, along the North Anatolian Fault Zone of western Turkey and the Calabrian subduction zone of southern Italy. Local high rates of convergence at the Hellenic subduction zone (35mm/yr) are associated with back-arc spreading throughout Greece and western Turkey above the subducting Mediterranean oceanic crust. Crustal normal faulting throughout this region is a manifestation of extensional tectonics associated with the back-arc spreading. The region of the Marmara Sea is a transition zone between this extensional regime, to the west, and the strike-slip regime of the North Anatolian Fault Zone, to the east. The North Anatolian Fault accommodates much of the right-lateral horizontal motion (23-24 mm/yr) between the Anatolian micro-plate and Eurasian plate as the Anatolian micro-plate is being pushed westward to further accommodate closure of the Mediterranean basin caused by the collision of the African and Arabian plates in southeastern Turkey. Subduction of the Mediterranean Sea floor beneath the Tyrrhenian Sea at the Calabrian subduction zone causes a significant zone of seismicity around Sicily and southern Italy. Active volcanoes are located above intermediate depth earthquakes in the Cyclades of the Aegean Sea and in southern Italy.

In the Mediterranean region there is a written record, several centuries long, documenting pre-instrumental seismicity (pre-20th century). Earthquakes have historically caused widespread damage across central and southern Greece, Cyprus, Sicily, Crete, the Nile Delta, Northern Libya, the Atlas Mountains of North Africa and the Iberian Peninsula. The 1903 M8.2 Kythera earthquake and the 1926 M7.8 Rhodes earthquakes are the largest instrumentally recorded Mediterranean earthquakes, both of which are associated with subduction zone tectonics. Between 1939 and 1999 a series of devastating M7+ strike-slip earthquakes propagated westward along the North Anatolian Fault Zone, beginning with the 1939 M7.8 Erzincan earthquake on the eastern end of the North Anatolian Fault system. The 1999 M7.6 Izmit earthquake, located on the westward end of the fault, struck one of Turkey's most densely populated and industrialized urban areas killing, more than 17,000 people. Although seismicity rates are comparatively low along the northern margin of the African continent, large destructive earthquakes have been recorded and reported from Morocco in the western Mediterranean, to the Dead Sea in the eastern Mediterranean. The 1980 M7.3 El Asnam earthquake was one of Africa's largest and most destructive earthquakes within the 20th century.

Large earthquakes throughout the Mediterranean region have also been known to produce significant and damaging tsunamis. One of the more prominent historical earthquakes within the region is the Lisbon earthquake of November 1, 1755, whose magnitude has been estimated from non-instrumental data to be about 8.0. The 1755 Lisbon earthquake is thought to have occurred within or near the Azores-Gibraltar transform fault, which defines the boundary between the African and Eurasian plates off the west coast of Morocco and Portugal. The earthquake is notable for both a large death toll of approximately 60,000 people and for generating a tsunami that swept up the Portuguese coast inundating coastal villages and Lisbon. An earthquake of approximately M8.0 near Sicily in 1693 generated a large tsunami wave that destroyed numerous towns along Sicily's east coast. The M7.2 December 28, 1908 Messina earthquake is the deadliest documented European earthquake. The combination of severe ground shaking and a local tsunami caused an estimated 60,000 to 120,000 fatalities. (USGS)

Featured image credit: USGS


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