Talk:Pacific–Farallon Ridge

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On 26 October 2024, it was proposed that this article be moved from Pacific-Farallon Ridge to Pacific–Farallon Ridge. The result of the discussion was moved.

Wiki Education Foundation-supported course assignment

Latest comment: 2 years ago1 comment1 person in discussion

This article is or was the subject of a Wiki Education Foundation-supported course assignment. Further details are available on the course page. Student editor(s): Cadotc.

Above undated message substituted from Template:Dashboard.wikiedu.org assignment by PrimeBOT (talk) 06:00, 17 January 2022 (UTC)Reply

General thoughts and ideas for expansion and improvement

Latest comment: 7 years ago1 comment1 person in discussion

This article clearly needs more from diagrams to content to citations. As far as diagrams, this article could use a map showing where the ridge used to exist and what plates it was near and etc. For content, we need a more clear timeline of the evolution of this ridge from when it was at its prime to its eventual subduction to the remnants and legacy of the ridge today. Apparently this ridge was also really productive in producing a lot of oceanic lithosphere so a whole section could be made on this topic alone. Here are some topics with references that I want to add to this page.

More history on the ridge including better timeline of when it subducted beneath the North American plate. (30 MA)^[1]

Productivity of the ridge was high- it accounts for almost 45% of oceanic lithosphere created since 83 MA.^[2]

Greater details on legacy of the ridge like how San Andreas Fault formed and etc. ^[3]

More references needed- preferably ones that are not journals or textbooks since that is what we have so far. Cadotc (talk) 06:01, 21 April 2017 (UTC)Reply

References

^ MacLeod, C. J.; Tyler, Paul A.; Walker, C. L. (228). Tectonic, Magmatic, Hydrothermal and Biological Segmentation of Mid-ocean Ridges. Geological Society of London. ISBN 9781897799727.
^ Rowan, Christopher; Rowley, David (June 2014). "Spreading behaviour of the Pacific-Farallon ridge system since 83 Ma". Geophysical Journal International. 197 (3). doi:https://doi-org.offcampus.lib.washington.edu/10.1093/gji/ggu056. {{cite journal}}: Check |doi= value (help); External link in |doi= (help)
^ Neal, Clive R.; Sager, William W.; Sano, Takashi; Erba, Elisabetta. Origin, Evolution, Environmental Impact of Oceanic LIPs. Geological Society of America. p. 97. ISBN 9780813725116.

Move discussion in progress

Latest comment: 21 days ago1 comment1 person in discussion

There is a move discussion in progress on Talk:Kula-Farallon Ridge which affects this page. Please participate on that page and not in this talk page section. Thank you. —RMCD bot 05:48, 26 October 2024 (UTC)Reply

Add topic

[1] MacLeod, C. J.; Tyler, Paul A.; Walker, C. L. (228). Tectonic, Magmatic, Hydrothermal and Biological Segmentation of Mid-ocean Ridges. Geological Society of London. ISBN 9781897799727.

[2] Rowan, Christopher; Rowley, David (June 2014). "Spreading behaviour of the Pacific-Farallon ridge system since 83 Ma". Geophysical Journal International. 197 (3). doi:https://doi-org.offcampus.lib.washington.edu/10.1093/gji/ggu056. {{cite journal}}: Check |doi= value (help); External link in |doi= (help)

[3] Neal, Clive R.; Sager, William W.; Sano, Takashi; Erba, Elisabetta. Origin, Evolution, Environmental Impact of Oceanic LIPs. Geological Society of America. p. 97. ISBN 9780813725116.

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