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Hellenic arc

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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. 249:
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 468: 344:"Incipient continental collision and plate-boundary curvature: Late Pliocene–Holocene transtensional Hellenic forearc, Crete, Greece" 44: 136: 77: 298:
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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trends parallel to its southern side. The Aegean Sea Plate, a microplate, is often considered part of the
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Mountain chain located on the southern margin of the Aegean Sea Plate
254: 448: 274: 395: 416: 398:American Geophysical Union, Fall Meeting Abstracts 341: 126:The center of Crete is at about center of the arc 32:southwestern Turkey, and all the islands between. 460: 264: 389: 273:in the west to just east of the island of 342:ten Veen, J.H.; Kleinspehn, K.L. (2003). 181:Aegean Sea, Ionian Sea, Mediterranean Sea 335: 461: 217:located on the southern margin of the 422: 277:in the east, where it links to the 221:. Geologically it results from the 13: 269:The Hellenic arc extends from the 84: 51: 14: 485: 442: 348:Journal of the Geological Society 469:Megathrust earthquakes in Greece 447: 83: 76: 50: 43: 25: 213:mountain chain of the southern 284: 1: 328: 293: 425:"Tectonic Summary of Greece" 265:Geometry of the Hellenic arc 7: 313: 10: 490: 113:Hellenic Republic (Greece) 259:South Aegean Volcanic Arc 190: 185: 175: 171:southern outer Hellenides 167: 130: 122: 117: 109: 67:Show map of Mediterranean 64:Hellas and the Aegean Sea 37: 24: 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 410:2004AGUFM.T53B0483P 360:2003JGSoc.160..161T 320:Mediterranean Ridge 229:under it along the 148: /  97:middle arc (Greece) 21: 157:35.21389; 24.96694 100:Show map of Greece 19: 474:Geology of Greece 452:Media related to 199: 198: 481: 451: 436: 435: 433: 431: 420: 414: 413: 393: 387: 386: 384: 382: 339: 219:Aegean Sea Plate 178: 163: 162: 160: 159: 158: 153: 149: 146: 145: 144: 141: 101: 87: 86: 80: 68: 54: 53: 47: 29: 22: 18: 489: 488: 484: 483: 482: 480: 479: 478: 459: 458: 445: 440: 439: 429: 427: 421: 417: 394: 390: 380: 378: 340: 336: 331: 325: 316: 296: 287: 267: 235:Hellenic Trench 195: 176: 156: 154: 150: 147: 142: 139: 137: 135: 134: 105: 104: 103: 102: 99: 98: 95: 94: 93: 92: 88: 71: 70: 69: 66: 65: 62: 61: 60: 59: 55: 33: 17: 12: 11: 5: 487: 477: 476: 471: 444: 443:External links 441: 438: 437: 415: 388: 354:(2): 161–181. 333: 332: 330: 327: 323: 322: 315: 312: 295: 292: 286: 283: 271:Ionian islands 266: 263: 239:Eurasian Plate 197: 196: 191: 188: 187: 186:Administration 183: 182: 179: 173: 172: 169: 165: 164: 132: 128: 127: 124: 120: 119: 115: 114: 111: 107: 106: 96: 90: 89: 82: 81: 75: 74: 73: 72: 63: 57: 56: 49: 48: 42: 41: 40: 39: 38: 35: 34: 30: 15: 9: 6: 4: 3: 2: 486: 475: 472: 470: 467: 466: 464: 457: 455: 450: 426: 419: 411: 407: 403: 399: 392: 377: 373: 369: 365: 361: 357: 353: 349: 345: 338: 334: 326: 321: 318: 317: 311: 309: 305: 301: 291: 282: 280: 276: 272: 262: 260: 256: 250: 246: 244: 240: 236: 232: 228: 227:African Plate 224: 220: 216: 212: 208: 204: 194: 189: 184: 180: 174: 170: 166: 161: 133: 129: 125: 121: 116: 112: 108: 79: 46: 36: 28: 23: 454:Hellenic arc 446: 428:. Retrieved 418: 401: 397: 391: 379:. Retrieved 351: 347: 337: 324: 297: 288: 268: 251: 247: 206: 203:Hellenic arc 202: 200: 192: 20:Hellenic arc 300:magnitude 7 285:Development 177:Adjacent to 168:Archipelago 155: / 131:Coordinates 463:Categories 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 404:: 0483. 314:See also 306:and the 255:Cyclades 123:Location 430:26 July 406:Bibcode 381:26 July 356:Bibcode 225:of the 211:arcuate 374:  275:Rhodes 233:. The 209:is an 193:Greece 372:S2CID 432:2010 383:2010 201:The 364:doi 352:160 205:or 465:: 402:53 400:. 370:. 362:. 350:. 346:. 310:. 281:. 434:. 412:. 408:: 385:. 366:: 358::

Index


middle arc is located in Mediterranean
middle arc is located in Greece
35°12′50″N 24°58′01″E / 35.21389°N 24.96694°E / 35.21389; 24.96694
arcuate
Aegean Sea
Aegean Sea Plate
subduction
African Plate
Hellenic subduction zone
Hellenic Trench
Eurasian Plate
Dodecanese
Cyclades
South Aegean Volcanic Arc
Ionian islands
Rhodes
Cyprus arc
magnitude 7
365 Crete earthquake
1303 Crete earthquake
Mediterranean Ridge
"Incipient continental collision and plate-boundary curvature: Late Pliocene–Holocene transtensional Hellenic forearc, Crete, Greece"
Bibcode
2003JGSoc.160..161T
doi
10.1144/0016-764902-067
S2CID
219542417
Bibcode

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