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The
Kythira Strait, located within the Western Hellenic arc, is subject to submergence on account of normal faulting which results in "extensional deformation and rotation" between two major segments of the external arc. According to Papadopoulos and Kijko, the Western Hellenic arc has high seismic
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activity, resulting in deformations in the strait which are active. Here the "seismic slip" recorded is on the order of 0.3 cm/year. Also reported in the strait are earthquakes at shallow and intermediate depths, with surface-wave magnitudes of up to 8.0.
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to the central and western
Mediterranean passes through the strait and are often subject to strong winds and shipwreck on Cape Maleas. To circumvent this, the shorter and safer route via the
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The
Kythira Strait's Tsunami Warning System (TWS) comprises two interrelated elements. One is based on the seismographic observations and the other is related to tide-gauge recordings.
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Kokinou, Eleni; Kamberis, Evangelos (2009). "The structure of the
KythiraâAntikythira strait, offshore SW Greece (35.7°â36.6°N)".
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The
Kythira Strait represents one of the most dangerous navigational hazards in the Mediterranean. The strait between Kythera and
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Neogene and
Quaternary vertical tectonics in the south Hellenic arc and their effect on concurrent sedimentation processes
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Soloviev, Sergey L.; Solovieva, Olga N.; Go, Chan N.; Kim, Khen S.; Shchetnikov, Nikolay A. (14 March 2013).
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Individual
Studies by Participants to the International Institute of Seismology and Earthquake Engineering
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230:. National Archives and Records Service, U.S. General Services Administration. 1984. p. 53.
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63:. It measures approximately 100 kilometres (62 mi) in length and is situated between the
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was found dangerous in ancient days by the Greek mariners. Most sea-traffic from
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374:. International Institute of Seismology and Earthquake Engineering.
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Guides to the microfilmed records of the German Navy, 1850â1945
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20:
View of the
Kythira Strait in the distance of southern Greece
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The Ionian
Islands: Corfu, Cephalonia, Ithaka and Beyond
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350:Tsunami Research at the End of a Critical Decade
168:Geological Society, London, Special Publications
376:It is considered to be a "dextral wrench zone".
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74:Many ships have sunk in the area, including
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353:. Springer Science & Business Media.
133:pathway and in modern times, through the
347:Hebenstreit, Gerald T. (14 March 2013).
129:, first through the use of the overland
397:Springer Science & Business Media.
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368:KensetsushŠKenchiku Kenkyūjo (1993).
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59:Strait is situated within the Western
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469:Landforms of Islands (regional unit)
213:KensetsushŠKenchiku Kenkyūjo 1993
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265:. Liturgical Press. p. 40.
380:Peters, Jeroen Martien (1985).
259:Campbell, Joan Cecelia (2009).
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326:Freely, John (15 May 2008).
262:Phoebe: Patron and Emissary
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141:Earthquakes and tsunami
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430:35.84278°N 23.23250°E
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310:Soloviev et al. 2013
125:has been used since
474:Landforms of Attica
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127:classical antiquity
101:Navigational hazard
464:Landforms of Crete
435:35.84278; 23.23250
300:, pp. 119â20.
123:Isthmus of Corinth
67:and the island of
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459:Straits of Greece
404:978-94-015-9510-0
360:978-94-017-3618-3
339:978-1-84511-696-5
272:978-0-8146-5281-7
29:Kythirian Straits
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332:. I. B. Tauris.
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53:Southern Greece
41:Kithera Channel
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55:. The Kythiraâ
25:Kythira Strait
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61:Hellenic arc
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244:Freely 2008
201:Peters 1985
174:: 343â360.
107:Cape Maleas
80: (H05)
65:Peloponnese
57:Antikythira
35:Antikythira
448:Categories
421:23°13â²57â³E
418:35°50â²34â³N
153:References
117:, and the
88: (62)
86:Gloucester
188:129436795
119:Black Sea
84:HMS
78:Greyhound
76:HMS
115:Istanbul
92:SS
45:waterway
33:Kythiraâ
454:Kythira
131:Diolkos
94:Ivernia
49:Kythira
43:) is a
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111:Athens
90:, and
37:Strait
27:(also
184:S2CID
69:Crete
399:ISBN
355:ISBN
334:ISBN
267:ISBN
47:off
176:doi
172:311
51:in
39:or
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