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Azores hotspot

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61: 169:. The increased melt production within the mantle may have supported a longer lived magma chamber causing the crust to be thicker. However, the Mid Atlantic Ridge has also been shown to have affected the characteristics of the Azores Plateau. It has been suggested that the main volcanic ridges on the plateau were created at the Mid Atlantic Ridge spreading axis. 159:
The Mid Atlantic Ridge is a zone of extension that permits magma to rise, forming dikes and surface volcanism. Areas of excess magmatism on the Mid Atlantic Ridge have been called hotspots e.g. the Azores. Gravity field modelling studies have shown that the crustal thickness in this area is 60%
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and the Azores archipelago (formed of 9 islands extending a distance of 480 km which have been volcanically active for around 7 Myr). The archipelago lies on the lateral branch of the Mid-Atlantic Ridge near the junction of three major tectonic plates; the
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anomalies have been mapped beneath the Azores in the upper 250–300 km. This has been suggested to be a signature of a plume that created the Azores Plateau. Another theory is that the excess volcanism simply results from excess extension at this unusual
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is elevated. The hotspot is asymmetrical (north and south). It is thought that crust at ridges is formed by a combination of processes (magmatic and tectonic) with magma addition coming from short lived
249:; Briais, A.; Deplus, C.; Escartin, J.; Georgen, J.; Lin, J.; Mercouriev, S.; Meyzen, C.; Muller, M.; Pouliquen, G.; Rabain, A. & da Silva, P. (1999). 191:"Interaction between the Mid-Atlantic Ridge and the Azores hot spot during the last 85 Myr: Emplacement and rifting of the hot spot-derived plateaus" 342:
In Plates, Plumes, and Planetary Processes, Edited by G.R. Foulger and D.M. Jurdy, Geological Society of America Special Paper 530, Boulder, CO
18: 250: 251:"Mid-Atlantic Ridge–Azores hotspot interactions: along-axis migration of a hotspot-derived event of enhanced magmatism 10 to 4 Ma ago" 477: 405: 190: 835: 504: 361:"Ridge-hotspot interaction along the Mid-Atlantic Ridge between 37°30′ and 40°30′N: the UTh disequilibrium evidence" 840: 126:. This unique location causes the area to have ridge-hotspot interaction with a variation of volcanic processes. 845: 340:
Smith, A. G. (2007). "A plate model for Jurassic to recent intraplate volcanism in the Pacific Ocean basin".
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Silveria, G.; Stutzmann, E.; Davaille, A.; Montagner, J.; Mendes-Victor, L. & Sebai, A. (2006).
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Upper mantle structure beneath the Azores hotspot from finite-frequency seismic tomography
8: 709: 562: 406:"Discovery of a magma chamber and faults beneath a Mid-Atlantic Ridge hydrothermal field" 424: 318: 229: 209: 747: 582: 444: 221: 99: 567: 452: 277: 767: 757: 752: 648: 620: 539: 513: 490: 436: 385: 360: 326: 302: 76: 472: 225: 800: 762: 643: 448: 428: 380: 322: 273: 213: 300: 795: 777: 704: 615: 587: 529: 521: 401: 246: 161: 148: 88: 742: 699: 671: 597: 557: 534: 135: 119: 110: 80: 399: 829: 772: 732: 727: 719: 610: 572: 549: 166: 139: 123: 34: 20: 812: 737: 440: 95: 245: 663: 217: 432: 404:; Canales, J. P.; Dusunur, D.; Escartin, J. & Miranda, M. (2006). 358: 400:
Singh, S. C.; Crawford, W. C.; Carton, H.; Seher, T.; Combier, V.;
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is relatively young and is associated with a bathymetric swell, a
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thought to have formed over the last 20 Mya. Negative velocity
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Bourdon, B.; Langmuir, C. H. & Zinder, A. (1996).
296: 294: 827: 189:Gente P.; Dyment J.; Maia M.; Goslin J. (2003). 307:Journal of Volcanology and Geothermal Research 303:"Azores hotspot signature in the upper mantle" 291: 154: 498: 352: 239: 393: 98:. The Azores hotspot lies just east of the 505: 491: 182: 384: 59: 828: 486: 339: 129: 64:The Azores hotspot is marked 1 on map 198:Geochemistry, Geophysics, Geosystems 365:Earth and Planetary Science Letters 258:Earth and Planetary Science Letters 13: 134:The Azores archipelago rises from 104: 14: 857: 466: 327:10.1016/j.jvolgeores.2006.03.022 138:, which is an area of thickened 109:The Azores domain comprises the 836:Hotspots of the Atlantic Ocean 333: 57:Volcanic hotspot at the Azores 1: 473:Azores Hotspot Deep Signature 278:10.1016/S0012-821X(99)00234-4 175: 512: 386:10.1016/0012-821x(96)00092-1 160:greater than normal and the 7: 155:Hotspot–ridge relationships 10: 862: 809: 786: 718: 690: 662: 629: 596: 548: 520: 841:Geography of the Azores 377:1996E&PSL.142..175B 270:1999E&PSL.173..257C 65: 846:Geology of the Azores 811:Proposed mechanisms: 631:Indo-Australian Plate 63: 788:South American Plate 692:North American Plate 218:10.1029/2003GC000527 116:North American Plate 433:10.1038/nature05105 425:2006Natur.442.1029S 419:(7106): 1029–1032. 319:2006JVGR..156...23S 210:2003GGG.....4.8514G 30: /  130:The Azores Plateau 100:Mid-Atlantic Ridge 66: 823: 822: 91:and ocean island 853: 507: 500: 493: 484: 483: 460: 459: 457: 451:. Archived from 410: 397: 391: 390: 388: 371:(1–2): 175–189. 356: 350: 349: 337: 331: 330: 298: 289: 288: 286: 280:. Archived from 255: 243: 237: 236: 234: 228:. Archived from 195: 186: 79:in the Northern 54: 53: 51: 50: 49: 47: 42: 41: 36: 31: 28: 27: 26: 23: 861: 860: 856: 855: 854: 852: 851: 850: 826: 825: 824: 819: 805: 782: 714: 686: 658: 625: 592: 544: 522:Antarctic Plate 516: 511: 469: 464: 463: 455: 408: 398: 394: 357: 353: 338: 334: 299: 292: 284: 253: 244: 240: 232: 193: 187: 183: 178: 172: 162:spreading ridge 157: 149:triple junction 132: 107: 105:Geological area 89:gravity anomaly 58: 45: 43: 39: 37: 33: 32: 29: 24: 21: 19: 17: 16: 12: 11: 5: 859: 849: 848: 843: 838: 821: 820: 810: 807: 806: 804: 803: 798: 792: 790: 784: 783: 781: 780: 775: 770: 765: 760: 755: 750: 745: 740: 735: 730: 724: 722: 716: 715: 713: 712: 707: 702: 696: 694: 688: 687: 685: 684: 682:Juan Fernández 679: 674: 668: 666: 660: 659: 657: 656: 651: 646: 641: 639:East Australia 635: 633: 627: 626: 624: 623: 618: 613: 608: 602: 600: 598:Eurasian Plate 594: 593: 591: 590: 585: 580: 575: 570: 565: 560: 554: 552: 546: 545: 543: 542: 537: 532: 526: 524: 518: 517: 510: 509: 502: 495: 487: 481: 480: 475: 468: 467:External links 465: 462: 461: 458:on 2013-12-20. 392: 351: 332: 313:(1–2): 23–34. 290: 287:on 2013-12-20. 264:(3): 257–269. 238: 235:on 2013-12-20. 180: 179: 177: 174: 167:magma chambers 156: 153: 136:Azores Plateau 131: 128: 120:Eurasian Plate 111:Azores Plateau 106: 103: 81:Atlantic Ocean 70:Azores hotspot 56: 46:Azores hotspot 35:38.5°N 28.75°W 9: 6: 4: 3: 2: 858: 847: 844: 842: 839: 837: 834: 833: 831: 818: 814: 808: 802: 799: 797: 794: 793: 791: 789: 785: 779: 776: 774: 771: 769: 766: 764: 761: 759: 756: 754: 751: 749: 746: 744: 741: 739: 736: 734: 731: 729: 726: 725: 723: 721: 720:Pacific Plate 717: 711: 708: 706: 703: 701: 698: 697: 695: 693: 689: 683: 680: 678: 675: 673: 670: 669: 667: 665: 661: 655: 652: 650: 647: 645: 642: 640: 637: 636: 634: 632: 628: 622: 619: 617: 614: 612: 609: 607: 604: 603: 601: 599: 595: 589: 586: 584: 581: 579: 576: 574: 571: 569: 566: 564: 561: 559: 556: 555: 553: 551: 550:African Plate 547: 541: 538: 536: 533: 531: 528: 527: 525: 523: 519: 515: 508: 503: 501: 496: 494: 489: 488: 485: 479: 476: 474: 471: 470: 454: 450: 446: 442: 438: 434: 430: 426: 422: 418: 414: 407: 403: 396: 387: 382: 378: 374: 370: 366: 362: 355: 347: 343: 336: 328: 324: 320: 316: 312: 308: 304: 297: 295: 283: 279: 275: 271: 267: 263: 259: 252: 248: 242: 231: 227: 223: 219: 215: 211: 207: 203: 199: 192: 185: 181: 173: 170: 168: 163: 152: 150: 145: 141: 140:oceanic crust 137: 127: 125: 124:African Plate 121: 117: 112: 102: 101: 97: 94: 90: 86: 82: 78: 75: 71: 62: 55: 52: 817:Plate theory 813:Mantle plume 605: 578:Sierra Leone 453:the original 416: 412: 395: 368: 364: 354: 345: 341: 335: 310: 306: 282:the original 261: 257: 241: 230:the original 204:(10): 1–23. 201: 197: 184: 171: 158: 133: 108: 96:geochemistry 69: 67: 40:38.5; -28.75 15: 710:Yellowstone 664:Nazca Plate 563:New England 38: / 830:Categories 748:Louisville 583:St. Helena 402:Cannat, M. 348:: 471–496. 247:Cannat, M. 176:References 44: ( 768:Rarotonga 758:Marquesas 753:Macdonald 677:Galápagos 654:Lord Howe 649:Tasmantid 621:Jan Mayen 540:Kerguelen 801:Trindade 763:Pitcairn 644:Crosgove 514:Hotspots 441:16943836 226:56297775 122:and the 74:volcanic 796:Noronha 778:Society 705:Bermuda 616:Iceland 588:Tristan 568:RĂ©union 530:Balleny 449:4301009 421:Bibcode 373:Bibcode 315:Bibcode 266:Bibcode 206:Bibcode 77:hotspot 25:28°45′W 22:38°30′N 743:Hawaii 700:Anahim 672:Easter 606:Azores 558:Canary 535:Erebus 447:  439:  413:Nature 224:  144:S-wave 118:, the 93:basalt 85:Azores 83:. The 773:Samoa 733:Bowie 728:Arago 611:Eifel 573:Shona 456:(PDF) 445:S2CID 409:(PDF) 285:(PDF) 254:(PDF) 233:(PDF) 222:S2CID 194:(PDF) 72:is a 738:Cobb 437:PMID 68:The 429:doi 417:442 381:doi 369:142 346:430 323:doi 311:156 274:doi 262:173 214:doi 832:: 815:· 443:. 435:. 427:. 415:. 411:. 379:. 367:. 363:. 344:. 321:. 309:. 305:. 293:^ 272:. 260:. 256:. 220:. 212:. 200:. 196:. 151:. 506:e 499:t 492:v 431:: 423:: 389:. 383:: 375:: 329:. 325:: 317:: 276:: 268:: 216:: 208:: 202:4 48:)

Index

38°30′N 28°45′W / 38.5°N 28.75°W / 38.5; -28.75 (Azores hotspot)

volcanic
hotspot
Atlantic Ocean
Azores
gravity anomaly
basalt
geochemistry
Mid-Atlantic Ridge
Azores Plateau
North American Plate
Eurasian Plate
African Plate
Azores Plateau
oceanic crust
S-wave
triple junction
spreading ridge
magma chambers
"Interaction between the Mid-Atlantic Ridge and the Azores hot spot during the last 85 Myr: Emplacement and rifting of the hot spot-derived plateaus"
Bibcode
2003GGG.....4.8514G
doi
10.1029/2003GC000527
S2CID
56297775
the original
Cannat, M.
"Mid-Atlantic Ridge–Azores hotspot interactions: along-axis migration of a hotspot-derived event of enhanced magmatism 10 to 4 Ma ago"

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