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The extension of the top layer required for this excursion of the arc and the trench comes from thinning of the back-arc ("in back of the arc"), weakening the crust there. There was already a mountain chain north of the arc, a legacy from the Alpine
Orogeny, called the "inner arc." Its tops are the
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The direction of subduction is northward. Locations on the arc or near it on the north side are therefore called "outer" as they are at the outer margin of the plate. Locations further north are "inner." Generally the motion of subduction is from outer to inner. It so happens that, due to back-arc
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A combined diagram of the Aegean and
Anatolian Plates. The southern margin of the Hellenic arc is shown, which is the trend line of the faults separating the arc and the Hellenic Trench. The body of the arc is the chain called the outer Hellenides, which includes west Peloponnesus, Crete, Rhodes,
261:. The two arcs are considered distinct, being from different orogenies. The term "Hellenic Arc" most often refers to the marginal, or "non-volcanic" arc, also called the Aegean forearc in the direction from outer to inner, which is consonant with the Hellenic Trench being the foredeep.
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extension, the
Hellenic Arc and Trench are moving in the reverse direction, from inner to outer, accounting for the severe arcuate form. There are in essence two layers at the subduction zone, a bottom one moving from outer to inner, and a top one moving from inner to outer.
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The current geometry of the
Hellenic arc is a result of the southwards migration of the subduction zone. This has led to extension both along the line of the arc as it bulged out and extension perpendicular to the arc, which is the current tectonic state.
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group. It encroaches on mainland terrain in the
Peloponnesus, on Crete, on Rhodes, and on the southern coast of Anatolia, thus being encompassed by both Greece and Turkey.
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from which it is in the process of diverging. The arc itself is mainly marine, the mountaintops appearing as islands in the Ionian Sea, Crete and its environs, or in the
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earthquakes in the last hundred years of instrumental recording and the location for at least two historical events that were probably of about magnitude 8 or more, the
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Papadopoulos, G. A.; Ganas, A.; Karastathis, C. (2004). "Seismicity
Properties as a Marker of the Active Plate Convergence in the western Hellenic Arc".
257:. In addition, a chain of volcanos has appeared across it, due to magma breaking through the weakened crust; hence, this "inner arc" is termed the
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344:"Incipient continental collision and plate-boundary curvature: Late Pliocene–Holocene transtensional Hellenic forearc, Crete, Greece"
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The
Hellenic arc is one of the most active seismic zones in western Eurasia. It has regularly been the source for
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425:"Tectonic Summary of Greece"
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259:South Aegean Volcanic Arc
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64:Hellas and the Aegean Sea
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231:Hellenic subduction zone
368:10.1144/0016-764902-067
423:USGS (29 March 2010).
456:at Wikimedia Commons
308:1303 Crete earthquake
152:35.21389°N 24.96694°E
304:365 Crete earthquake
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360:2003JGSoc.160..161T
320:Mediterranean Ridge
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285:Development
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131:Coordinates
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329:References
294:Seismicity
279:Cyprus arc
243:Dodecanese
223:subduction
215:Aegean Sea
207:Aegean arc
143:24°58′01″E
140:35°12′50″N
91:middle arc
58:middle arc
376:219542417
118:Geography
110:Etymology
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314:See also
306:and the
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123:Location
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406:Bibcode
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