20:
616:
140:
that uplifted the ocean floor of the still young
Pacific Plate. Reefs developed on the subsiding islands and renewed volcanism in the Late Cretaceous helped maintain some of eastern islands but inevitably the guyots sank to their present depth. It has been proposed that the MPM has crossed over
98:) above the surrounding ocean floor and is covered with several layers of thick sedimentary sequences that differ from those of other plateaux in the North Pacific. About 50 seamounts are distributed over the MPM. Some of the highest points in the range are above sea level which include
128:
with a lava composition similar to those found in
Iceland and the Galapagos Islands, and they probably formed similarly at or near a rift system. In the Cretaceous, they formed large tropical islands located closer to the Equator that began to sink in the late Mesozoic.
141:
several hotspots, and the MPM guyots are indeed older on the western MPM than the eastern part, but the guyots do not form chains that can be traced to any known hotspots. The MPM, nevertheless, must have originated over the South
Pacific
648:
290:
Ladd, H.S.; Newman, W.A.; Sohl, N.F. (1974). Cameron, A.M.; Cambell, B.M.; Cribb, A.B.; Endean, R.; Jell, J.S.; Jones, O.A.; Mather, P.; Talbot, F.H. (eds.).
833:
838:
87:
641:
19:
498:"The geologic history of the Mid-Pacific Mountains in the central North Pacific Ocean: a synthesis of deep-sea drilling studies"
634:
606:
62:
358:
401:
Karig, D. E.; Peterson, M. N. A.; Short, G. G. (1970). "Sediment-capped guyots in the Mid-Pacific
Mountains".
176:
archipelago, begins near the eastern part of the MPM. The formation of the MPM thus probably occurred at the
697:
177:
742:
843:
727:
582:"31. Synthesis of Drilling Results From the Mid-Pacific Mountains: Regional Context and Implications"
560:
539:
439:
410:
381:. Geological Society of America Memoirs. Vol. 64. Geological Society of America. pp. 1â92.
346:
292:
812:
551:
Winterer, E. L.; Metzler, C. V. (1984). "Origin and subsidence of guyots in MidâPacific
Mountains".
752:
747:
732:
717:
302:
797:
787:
782:
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702:
772:
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484:
455:
757:
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807:
792:
181:
137:
103:
692:
762:
568:
509:
476:
447:
418:
382:
354:
154:
71:
Underwater mountain range from the southern tier of the Japan Trench to the
Hawaiian Islands
83:
564:
543:
443:
414:
350:
165:
430:
Kroenke, L. W.; Kellogg, J. N.; Nemoto, K. (1985). "Mid-pacific mountains revisited".
827:
722:
687:
620:
581:
497:
459:
422:
334:
150:
146:
118:
91:
802:
615:
488:
374:
169:
158:
90:. Of volcanic origin and Mesozoic in age, it is located on the oldest part of the
514:
99:
95:
208:, Morphology, Age, Plate-Tectonic Setting, and Previous Studies, pp. 1073â1074
142:
114:
496:
Thiede, J.; Dean, W. E.; Rea, D. K.; Vallier, T. L.; Adelseck, C. G. (1981).
572:
110:
626:
480:
451:
173:
386:
580:
Winterer, E. L.; Sager, W. W.; Firth, J. V.; Sinton, J. M. (1995).
530:
Wilde, P. (2010). "Supervolcanoes in the Mid-Pacific
Mountains?".
125:
630:
586:
Proceedings of the Ocean
Drilling Program, Scientific Results
359:
10.1130/0091-7613(2001)029<0695:HMPHAF>2.0.CO;2
86:
located in the central North
Pacific Ocean or south of the
467:
Menard, H. W. (1959). "Geology of the
Pacific sea floor".
335:"How many Pacific hotspots are fed by deep-mantle plumes?"
301:. Second International Coral Reef Symposium. Vol. 2.
277:
280:, Origin and Formation of Igneous Basement, pp. 508â509
604:
379:
64 : Sunken Islands of the Mid-Pacific Mountains
253:
241:
205:
145:. Among the guyots in the Mid-Pacific Mountains are
680:
664:
291:
315:
502:Initial Reports of the Deep Sea Drilling Project
305:: The Great Barrier Reef Committee. p. 513.
265:
642:
403:Deep Sea Research and Oceanographic Abstracts
375:"Sunken Islands of the Mid-Pacific Mountains"
109:The ocean floor of the MPM dates back to the
8:
553:Journal of Geophysical Research: Solid Earth
132:The MPM formed in the Early Cretaceous (at
649:
635:
627:
513:
94:and rises up to 2 km (1.2 mi) (
294:Darwin guyot, the Pacific's oldest atoll
611:
198:
217:
229:
180:and the Easter hotspot, or where the
168:chain, a lineament that includes the
7:
333:Clouard, V.; Bonneville, A. (2001).
242:Kroenke, Kellogg & Nemoto 1985
14:
614:
18:
88:HawaiianâEmperor seamount chain
36:HawaiianâEmperor seamount chain
1:
834:Plateaus of the Pacific Ocean
515:10.2973/dsdp.proc.62.162.1981
316:Clouard & Bonneville 2001
133:
839:Geology of the Pacific Ocean
423:10.1016/0011-7471(70)90029-X
266:Winterer & Metzler 1984
860:
532:AGU Fall Meeting Abstracts
326:General and cited sources
373:Hamilton, E. L. (1956).
164:The western half of the
573:10.1029/JB089iB12p09969
698:Bonhomme Richard Guyot
178:Pacific-Farallon Ridge
124:The MPM is a range of
672:Mid-Pacific Mountains
658:Mid-Pacific Mountains
117:, some of the oldest
76:Mid-Pacific Mountains
54:Mid-Pacific Mountains
278:Winterer et al. 1995
136:110 Ma) over a
63:class=notpageimage|
565:1984JGR....89.9969W
544:2010AGUFM.V13C2368W
444:1985GML.....5...77K
415:1970DSRA...17..373K
351:2001Geo....29..695C
303:Brisbane, Australia
738:Cape Johnson Guyot
559:(B12): 9969â9979.
481:10.1007/BF02158108
452:10.1007/BF02233931
432:Geo-marine Letters
254:Thiede et al. 1981
206:Thiede et al. 1981
821:
820:
681:Individual guyots
182:Easter Microplate
851:
763:Resolution Guyot
743:Jacqueline Guyot
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628:
619:
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387:10.1130/MEM64-p1
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318:, Easter, p. 696
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209:
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184:is now located.
155:Resolution Guyot
135:
55:
46:
37:
28:
22:
859:
858:
854:
853:
852:
850:
849:
848:
824:
823:
822:
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728:NAVOCEANO Guyot
676:
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625:
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603:
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84:oceanic plateau
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49:
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44:
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31:
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26:
12:
11:
5:
857:
855:
847:
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841:
836:
826:
825:
819:
818:
816:
815:
813:Niemeyer Guyot
810:
805:
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795:
790:
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665:The main group
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639:
631:
624:
623:
602:
601:
577:
548:
527:
493:
475:(6): 205â213.
464:
427:
409:(2): 373â378.
398:
370:
345:(8): 695â698.
329:
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308:
282:
270:
258:
246:
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222:
210:
197:
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166:Easter hotspot
70:
61:
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52:
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50:
43:
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34:
33:
32:
25:
24:
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17:
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13:
10:
9:
6:
4:
3:
2:
856:
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832:
831:
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786:
784:
781:
779:
776:
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771:
769:
766:
764:
761:
759:
756:
754:
753:Stetson Guyot
751:
749:
748:Caprina Guyot
746:
744:
741:
739:
736:
734:
733:Revelle Guyot
731:
729:
726:
724:
723:Allison Guyot
721:
719:
718:Shepard Guyot
716:
714:
711:
709:
706:
704:
701:
699:
696:
694:
691:
689:
688:Horizon Guyot
686:
685:
683:
679:
673:
670:
669:
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647:
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541:
538:: V13Câ2368.
537:
533:
528:
516:
511:
508:: 1073â1120.
507:
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220:, p. 206
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187:
185:
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179:
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151:Horizon Guyot
148:
147:Allison Guyot
144:
139:
130:
127:
122:
120:
119:oceanic crust
116:
112:
107:
105:
104:Marcus Island
101:
97:
93:
92:Pacific Plate
89:
85:
82:) is a large
81:
77:
64:
21:
803:Darwin Guyot
798:Harvey Guyot
788:Menard Guyot
783:Heezen Guyot
778:Thomas Guyot
713:Murray Guyot
703:Renard Guyot
671:
657:
593:. Retrieved
589:
585:
556:
552:
535:
531:
519:. Retrieved
505:
501:
472:
468:
438:(2): 77â81.
435:
431:
406:
402:
390:. Retrieved
378:
362:. Retrieved
342:
338:
311:
293:
285:
273:
261:
249:
237:
225:
213:
201:
170:Line Islands
163:
159:Darwin Guyot
131:
123:
108:
79:
75:
73:
27:Shatsky Rise
844:Wake Island
773:Allen Guyot
768:Ewing Guyot
595:2 September
521:2 September
469:Experientia
364:9 September
218:Menard 1959
100:Wake Island
96:Darwin Rise
828:Categories
758:Hill Guyot
708:Hess Guyot
392:26 October
268:, Abstract
256:, Abstract
244:, Abstract
232:, Abstract
230:Wilde 2010
143:Superswell
121:on Earth.
115:Cretaceous
808:SIO Guyot
793:HIG Guyot
460:129287640
193:Citations
45:Hess Rise
111:Jurassic
66:Location
693:A Guyot
561:Bibcode
540:Bibcode
489:9383923
440:Bibcode
411:Bibcode
347:Bibcode
339:Geology
188:Sources
174:Tuamotu
138:hotspot
621:Oceans
607:Portal
487:
458:
126:guyots
485:S2CID
456:S2CID
299:(PDF)
597:2018
523:2018
394:2017
366:2018
172:and
157:and
102:and
74:The
590:143
569:doi
510:doi
477:doi
448:doi
419:doi
383:doi
355:doi
80:MPM
830::
588:.
584:.
567:.
557:89
555:.
536:13
534:.
506:62
504:.
500:.
483:.
471:.
454:.
446:.
434:.
417:.
407:17
405:.
377:.
353:.
343:29
341:.
337:.
161:.
153:,
149:,
134:c.
106:.
650:e
643:t
636:v
609::
599:.
575:.
571::
563::
546:.
542::
525:.
512::
491:.
479::
473:1
462:.
450::
442::
436:5
425:.
421::
413::
396:.
385::
368:.
357::
349::
113:-
78:(
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