
A review published within the journal Tectonics has supplied new insights into the forces that trigger tectonic actions in Europe’s most seismically lively areas. Researchers used superior satellite tv for pc knowledge to trace land actions in Greece, western Turkey and the southern Balkan nations.
Tectonic plates diverge, converge, or transfer past one another in opposing instructions at speeds of 0.1 to 90 millimeters per 12 months. At many plate boundaries, rocks on either side of the fault stay caught for many years or centuries whereas the plates proceed to maneuver. This causes materials stress to construct up on the plate boundaries.
If that stress turns into too nice and the rocks break unfastened, the relative motion might be meters in a single brief time period: an earthquake. A staff of geoscientists used a sophisticated mechanical model to estimate the forces behind these actions on the tectonic boundary between the African and Eurasian plates. The model contains essential fault zones recognized for his or her earthquakes.
Using this model, for the primary time, scientists have been in a position to decide the utmost relative velocity within the hypothetical case of no friction on the plate boundaries. They additionally decided the precise present velocity. The larger the distinction between the utmost and present velocity of a plate, the extra stress builds up and thus the larger the chance of a serious earthquake.
“We can now estimate how rapidly the stress builds up,” says Rob Govers, affiliate professor at Utrecht University and lead creator of the research. “This is essential info for assessing the danger of main earthquakes.”

Smooth passage
The subduction zones to the south, west and east of the Aegean Sea—where the African plate slides to a depth of 1300 km beneath Europe—seem to play a vital position. The stress builds up slowly alongside the plate boundaries, except for the Kephalonia fault zone.
As a end result, most plate boundaries have nearly the utmost attainable velocity, and the plates slide easily past or over one another. The velocity alongside the infamous North Anatolian fault can also be easy, besides close to Istanbul, where an earthquake is anticipated.
“The motion predictions of our model correspond very nicely with satellite tv for pc observations,” says Govers. “This offers us confidence in our findings, which supply a brand new understanding of the seismic exercise within the area.”
The model additionally predicts observations that weren’t a part of the research, such because the fault actions in the course of the earthquakes round Santorini in February 2025.
Predictions
The subsequent step is to hyperlink these new insights to historic earthquake knowledge. From this, you’ll be able to estimate roughly at what stress factors plates have damaged unfastened.
“If you hyperlink this to our model and when earlier main earthquakes occurred, you’ll be able to theoretically predict when and where the subsequent main earthquake is prone to happen within the coming a long time,” provides Govers. This info can be utilized to enhance constructing pointers and different protecting measures.
More info:
Rob Govers et al, Probabilistic Assessment of the Causes of Active Deformation in Greece, Western Anatolia, and the Balkans Using Finite Element Models, Tectonics (2025). DOI: 10.1029/2024TC008658
Provided by
Utrecht University
Citation:
Satellite knowledge present perception into tectonic actions in south-eastern Europe ( 5)
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