The southern part of the Aegean Plate, near Crete, is considered a subduction zone because the African Plate pushes beneath is. (1) As a refresher, a subduction zone is a "place where two lithospheric plates come together, one riding over the other." (2) In the case of Greece, the southern part of the Aegean Plate 'rides over' the northern part of the African Plate. Because of this motion, there are many shallow and normal earthquakes along this southern Aegean plate boundary, as well as having caused the formation of the Hellenic Arc which is made up of both active and inactive volcanoes. (3) For example, the Santorini Volcano, one of the most active ones, last erupting in 1950.
At the north part of the Aegean Plate is the Eurasian Plate, there is a divergent boundary, which is when "two tectonic plates that are moving away from each other" and this creates a space that is filled with new crustal material sourced from molten magma that forms below. (4) This kind of seismic activity not only causes earthquakes but also caused the formation of the Gulf of Corinth. (5)
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Great tectonic entry. Next weeks we'll discuss in detail seismicity and volcanoes so you can discuss them further....lots of hazards going your way...
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ReplyDeleteThis is interesting! Greece is one of my top places I have been interested in for a while now. I think the information you gave was great, and like the country I chose it has many earthquakes due to the fact it is located by a subduction zone. Thank you for this entry! I can't wait to read more about Greece this semester.
Miriam, great post! It's very interesting and informative. I never knew Greece had a volcano, much less an active one. My country is also located on a subduction zone & has some earthquakes. Thanks for all the info!
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