1.0Aegeus Societyhttps://www.aegeussociety.org/en/john_ahttps://www.aegeussociety.org/en/author/john_a/A Seismic History of Crete - Aegeus Societyrich600338<blockquote class="wp-embedded-content" data-secret="5wadpBAUBU"><a href="https://www.aegeussociety.org/en/new_book/a-seismic-history-of-crete/">A Seismic History of Crete</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="https://www.aegeussociety.org/en/new_book/a-seismic-history-of-crete/embed/#?secret=5wadpBAUBU" width="600" height="338" title="“A Seismic History of Crete” — Aegeus Society" data-secret="5wadpBAUBU" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script type="text/javascript">
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https://www.aegeussociety.org/wp-content/uploads/2012/12/a-seasmic-history-of-crete.jpg324450The seismicity in Greece and in the adjacent regions is the highest in the Western Eurasia. One of the most active seismotectonic structures in that region is the Hellenic Arc and Trench (H-AT) system. The island of Crete occupies the central segment of H-AT just to the north of the front where the lithospheric plates of Africa and Eurasia converge and the former bends and subducts beneath the later.