Louisville hotspot

The Louisville hotspot is believed to lie close to the Pacific-Antarctic Ridge, although its exact present location is uncertain.{{cite book|last=Condie|first=Kent C.|title=Mantle Plumes and Their Record in Earth History|publisher=Cambridge University Press|year=2001|pages=19|url=https://books.google.com/books?id=JaV8V8mufhoC&pg=PA19|isbn=0-521-01472-7}}

The Louisville hotspot has produced the Louisville Ridge, which is one of the longest seamount chains on Earth, stretching some {{convert|4300|km|mi|0|abbr=on}}{{cite conference |last1=Vanderkluysen |first1=L. |last2=Mahoney |first2=J. J. |last3=Koppers |first3=A. A. |last4=Lonsdale |first4=P. F. |url=https://adsabs.harvard.edu/abs/2007AGUFM.V42B..06V |title=Geochemical Evolution of the Louisville Seamount Chain |conference=American Geophysical Union |date=Fall 2007 |id=Abstract no. #V42B-06 |bibcode=2007AGUFM.V42B..06V}} from the Pacific-Antarctic Ridge to the Tonga Trench where it subducts under the Indo-Australian Plate as part of the Pacific Plate.

The Louisville hotspot is believed to have been active since at least 78.8 ± 1.3 Ma based on age of the oldest seamount (Osbourn{{Cite journal|last1=Koppers|first1=Anthony A. P.|last2=Gowen|first2=Molly D.|last3=Colwell|first3=Lauren E.|last4=Gee|first4=Jeffrey S.|last5=Lonsdale|first5=Peter F.|last6=Mahoney|first6=John J.|last7=Duncan|first7=Robert A.|date=December 2011|title=New 40Ar/39Ar age progression for the Louisville hot spot trail and implications for inter-hot spot motion|journal=Geochemistry, Geophysics, Geosystems|language=en|volume=12|issue=12|pages=n/a|doi=10.1029/2011gc003804|bibcode=2011GGG....12.AM02K|s2cid=55376246 |issn=1525-2027|doi-access=free}}{{Cite journal|last1=Koppers|first1=Anthony A. P.|last2=Yamazaki|first2=Toshitsugu|last3=Geldmacher|first3=Jörg|last4=Gee|first4=Jeffrey S.|last5=Pressling|first5=Nicola|last6=Koppers|first6=Anthony A. P.|last7=Yamazaki|first7=Toshitsugu|last8=Geldmacher|first8=Jörg|last9=Gee|first9=Jeffrey S.|date=2012-11-25|title=Limited latitudinal mantle plume motion for the Louisville hotspot|journal=Nature Geoscience|language=En|volume=5|issue=12|pages=911–917|doi=10.1038/ngeo1638|bibcode=2012NatGe...5..911K|issn=1752-0894}}). This duration is comparable to that of the Hawaiian-Emperor seamount chain, although the rate of volcanism at the two chains are relatively different by 50% with volcanic activity at each seamount location being shorter in the Louisville seamounts at about 4 million years compared to more like 6 million years.{{cite journal|first1=D. E. |last1=Heaton|first2= A. A. P. |last2=Koppers|title=High-Resolution 40Ar/39Ar Geochronology of the Louisville Seamounts IODP Expedition 330 Drill Sites: Implications for the Duration of Hot Spot-related Volcanism and Age Progressions|journal=Geochemistry, Geophysics, Geosystems|language=en|volume=20|issue=8|year=2019|pages=4073–4102 |doi=10.1029/2018GC007759 |bibcode=2019GGG....20.4073H |s2cid=198407241 |url= https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018GC007759}} The Louisville Ridge has a relatively small bend compared to that in the Hawaiian-Emperior chain. During the Early Oligocene period, the Louisville hotspot's magma source rate was much steadier than the Hawaii hotspot rate, and had a lower total volume in eruption. During the Late Oligocene, the magma source decreased to a small fraction of that in the Hawaiian-Emperor seamount chain, such that none of the volcanoes has emerged above sea level in the past 11 million years. The Louisville Ridge is only half as wide as the Hawaiian-Emperior seamount chain. Therefore, unlike the Hawaii hotspot, the Louisville hotspot is believed to have decreased in activity with time.

The Louisville hotspot may have helped create the Ontong Java Plateau, the world's largest oceanic plateau, around 120 million years ago. The modelled locations of the plateau and hotspot at the time do not coincide under one recent plate reconstruction, arguing against this, although other factors mean their linkage may still be possible.{{cite book |last1=Antretter |first1=M. |last2=Riisager |first2=P. |last3=Hall |first3=S. |last4=Zhao |first4=X. |last5=Steinberger |first5=B. |year=2004 |url=http://sp.lyellcollection.org/cgi/content/abstract/229/1/21 |chapter=Modelled palaeolatitudes for the Louisville hot spot and the Ontong Java Plateau |title=Origin and Evolution of the Ontong Java Plateau |publisher=Geological Society |location=London |series=Special Publications |volume=229 |pages=21–30 |doi=10.1144/GSL.SP.2004.229.01.03|s2cid=129116505 }} One other factor is compositional studies which would suggest that only part of the Ontong Java Plateau that separated quite early is related to the Louisville hotspot.{{cite journal|last1=Vanderkluysen |first1=L. |last2=Mahoney |first2=J. J. |last3=Koppers |first3=A. A. |last4=Beier |first4=C. |last5=Regelous |first5=M. |last6=Gee |first6=J. S. |last7=Lonsdale |first7=P. F. |title= Louisville Seamount Chain: Petrogenetic processes and geochemical evolution of the mantle source |journal= Geochemistry, Geophysics, Geosystems |year= 2014 |volume=15 |issue=6 |page=2380-400|doi=10.1002/2014GC005288|bibcode=2014GGG....15.2380V |s2cid=128524309 |doi-access=free }} The compositional studies also define that the hot spot magma produces a distinct alkali basalt compared to the eruptives from the Hawaii hotspot.

• Louisville Ridge
• Christmas Island Seamount Province
• Arago hotspot
• Rarotonga hotspot
• Hollister Ridge
• Osbourn Seamount the oldest of the Louisville Ridge

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Category:Hotspots of the Pacific Ocean