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Darwin Rise

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Coordinates: 10°N 180°W / 10°N 180°W / 10; -180
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This is an old revision of this page, as edited by GeoWriter (talk | contribs) at 12:18, 4 September 2018 (→Sources: Stein and Stein "The Superswell and Darwin Rise: Thermal no longer?" - changed date from "after 1999" to "c. 1999" for formatting reasons although it could be any date between between 2000 and February 2017). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

10°N 180°W / 10°N 180°W / 10; -180

Darwin Rise is located in Pacific Ocean
Darwin Rise
Darwin Rise
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Location in the Pacific Ocean[1]

The Darwin Rise is broad triangular region in the north central Pacific Ocean where there is a concentration of atolls.

During his voyage across the globe Charles Darwin realised that vertical crustal motion must be responsible for the formation of continents and ocean basins, as well as isolated atolls in the Pacific. He deduced that the central basin of the Pacific had subsided while surrounding areas had risen. In 1964 U.S. geologist Henry Menard subsequently named the uplifted area in the Pacific after the English naturalist.[2]

Geological context

Covering an area of 12,000 km × 3,000 km (7,500 mi × 1,900 mi), the Darwin Rise is limited to the east by the Izu-Bonin and Mariana trenches, to the west by the Line Islands.[3] Two major plateaux, the Shatsky Rise to the north and the Ontong Java Plateau to the south, border the Darwin Rise. How these plateaux relate to the rise remains disputed.[3]

There are six major chains of seamounts on the rise — the Japanese, Magellan, Wake, Marshall Islands, Line Islands seamounts and the Mid-Pacific Mountains — and numerous minor clusters. The ages of these seamounts in general follow the motion of the Pacific Plate from 130 to 180 Ma, as predicted by conventional hotspot theory, and decrease from west to east and north to south. This age-distance pattern is, however, not corroborated by the limited data available.[3]

Origin

In 1964, Henry Menard proposed that this was a superswell raised by volcanism during the Cretaceous (120-80 mya).[4] A problem with this conjecture is that this region actually has a sea floor at a normal depth that happens to possess an abundance of sea mounts.[5][6]

Instead this feature may have formed from diapirs or plumes rising from the Earth's upper mantle, which results in chains of sea mounts along the direction of the plate motion. However, this idea remains in dispute and an alternate hypothesis involving multiple "plumelets" has been proposed.[7]

In the 1980s it was proposed that the Darwin Rise was the South Pacific Superswell 100 Ma and that the volcanoes of the Darwin Rise erupted over the same mantle region as the volcanoes of French Polynesia today.[8] Hence, U.S. geologist Marcia McNutt proposed that the Darwin Rise is a palaeo-superswell.[9]

See also

References

Notes

  1. ^ Stein & Stein c. 1999, Figure 1: Map of the south Pacific showing place names
  2. ^ Stein & Stein 1993, Introduction, p. 53; Darwin 1845: When later dealing with other continents he became so fixed in his belief in vertical movements of the crust and the erosive power of the sea that he excluded other possible explanations[…] [1]; Menard 1964
  3. ^ a b c Janney & Castillo 1999, Setting and Age Constraints, pp. 10572, 10574
  4. ^ For an illustration of Menard's model of the evolution of the Darwin Rise see Stein & Stein 1993, Fig. 1, p. 54
  5. ^ DeLaughter, Stein & Stein 2005, p. 272
  6. ^ Foulger 2010, p. 220
  7. ^ Janney & Castillo 1999, Abstract
  8. ^ McNutt 1998, p. 213
  9. ^ McNutt 1998, Fig. 2, p. 212

Sources

  • Darwin, C. (1845). The Voyage of the Beagle. {{cite book}}: Invalid |ref=harv (help)
  • DeLaughter, J. E.; Stein, C. A.; Stein, S. (2005). "Hotspots: A view from the swells". In Foulger, G. R.; Natland, J. H.; Presnall, D. C.; Anderson, D. L. (eds.). Plates, Plumes, and Paradigms (PDF). The Geological Society of America. doi:10.1130/0-8137-2388-4.257. ISBN 0-8137-2388-4. Retrieved 18 February 2017. {{cite book}}: Invalid |ref=harv (help)
  • Foulger, G. R. (2010). Plates vs Plumes: A Geological Controversy. John Wiley and Sons. ISBN 1-4443-3679-7. {{cite book}}: Invalid |ref=harv (help)
  • Janney, P. E.; Castillo, P. R. (1999). "Isotope geochemistry of the Darwin Rise seamounts and the nature of long-term mantle dynamics beneath the south central Pacific" (PDF). Journal of Geophysical Research. 104 (B5): 10571–10590. Bibcode:1999JGR...10410571J. doi:10.1029/1998JB900061. Retrieved 19 February 2017. {{cite journal}}: Invalid |ref=harv (help)
  • McNutt, M. K. (1998). "Superswells" (PDF). Reviews of Geophysics. 36 (2): 211–244. doi:10.1029/98RG00255. Retrieved 19 February 2017. {{cite journal}}: Invalid |ref=harv (help)
  • Menard, H. W. (1964). Marine Geology of the Pacific. New York: McGraw-Hill. OCLC 545637. {{cite book}}: Invalid |ref=harv (help)
  • Stein, C. A.; Stein, S. (1993). "Constraints on Pacific midplate swells from global depth‐age and heat flow‐age models" (PDF). In Pringle, M. S.; Sager, W. W.; Sliter, W. V. (eds.). The Mesozoic Pacific: geology, tectonics, and volcanism. Vol. 77. Washington, D.C.: Geophysical Union. pp. 53–76. doi:10.1029/GM077p0053. Retrieved 19 February 2017. {{cite book}}: |journal= ignored (help); Invalid |ref=harv (help)
  • Stein, Carol A.; Stein, Seth (c. 1999). "The Superswell and Darwin Rise: Thermal no longer?". {{cite web}}: Invalid |ref=harv (help)


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