Mohns Ridge: Difference between revisions
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[[File:JanMayenlocation.PNG|thumb|Map showing the location of the Mohns Ridge and other major geological features of the northernmost Atlantic]] |
[[File:JanMayenlocation.PNG|thumb|Map showing the location of the Mohns Ridge and other major geological features of the northernmost Atlantic]] |
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The '''Mohns Ridge''' is |
The '''Mohns Ridge''' is an ultraslow-spreading segment of the [[Mid-Atlantic Ridge]] located to the north of [[Jan Mayen]] in the Arctic Ocean.<ref>{{Cite web |title=Marine Regions · Mohns Ridge (Ridge) |url=https://www.marineregions.org/gazetteer.php/gazetteer.php?p=details&id=4224 |access-date=2023-01-16 |website=www.marineregions.org}}</ref> It is bounded to the south by the Jan Mayen [[fracture zone]], and transitions to [[Knipovich Ridge]] in the north-east. |
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== Geology == |
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⚫ | In 2008, a black smoker vent field named [[Loki's Castle]] was discovered along one of the axial volcanic ridges in the area.<ref>{{Cite journal |last1=Pedersen |first1=Rolf B. |last2=Rapp |first2=Hans Tore |last3=Thorseth |first3=Ingunn H. |last4=Lilley |first4=Marvin D. |last5=Barriga |first5=Fernando J. A. S. |last6=Baumberger |first6=Tamara |last7=Flesland |first7=Kristin |last8=Fonseca |first8=Rita |last9=Früh-Green |first9=Gretchen L. |last10=Jorgensen |first10=Steffen L. |date=2010-11-23 |title=Discovery of a black smoker vent field and vent fauna at the Arctic Mid-Ocean Ridge |journal=Nature Communications |language=en |volume=1 |issue=1 |pages=126 |doi=10.1038/ncomms1124 |issn=2041-1723 |pmc=3060606 |pmid=21119639 |
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The ridge started forming 53 My ago, as the [[Greenland Plate]] and [[Eurasian Plate]] started separating. Four separate axial volcanic ridges have been discovered along Mohns Ridge.<ref>{{Cite thesis |title=The Morphology of the Mohn's Ridge - with Special Focus on Listric and Detachment Faults and their Link to the Formation of Seafloor-massive Sulfides |url=https://ntnuopen.ntnu.no/ntnu-xmlui/handle/11250/2452116 |publisher=NTNU |date=2017 |degree=Master thesis |first=Hauke |last=Reimers}}</ref> |
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== Notable features == |
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⚫ | Several active and non-active hydrothermal vent fields have been located along Mohns Ridge. In 2008, a black smoker vent field named [[Loki's Castle]] was discovered along one of the axial volcanic ridges in the area.<ref>{{Cite journal |last1=Pedersen |first1=Rolf B. |last2=Rapp |first2=Hans Tore |last3=Thorseth |first3=Ingunn H. |last4=Lilley |first4=Marvin D. |last5=Barriga |first5=Fernando J. A. S. |last6=Baumberger |first6=Tamara |last7=Flesland |first7=Kristin |last8=Fonseca |first8=Rita |last9=Früh-Green |first9=Gretchen L. |last10=Jorgensen |first10=Steffen L. |date=2010-11-23 |title=Discovery of a black smoker vent field and vent fauna at the Arctic Mid-Ocean Ridge |journal=Nature Communications |language=en |volume=1 |issue=1 |pages=126 |bibcode=2010NatCo...1..126P |doi=10.1038/ncomms1124 |issn=2041-1723 |pmc=3060606 |pmid=21119639}}</ref> |
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The [[Schulz Bank]] seamount is located on the northern part of the ridge, as Mohns Ridge transitions into the [[Knipovich Ridge]].<ref>{{Cite journal |last=Meyer |first=H.K. |last2=Davies |first2=A.J. |last3=Roberts |first3=E.M. |last4=Xavier |first4=J.R. |last5=Ribeiro |first5=P.A. |last6=Glenner |first6=H. |last7=Birkely |first7=S.-R. |last8=Rapp |first8=H.T. |date=2023-01 |title=Beyond the tip of the seamount: Distinct megabenthic communities found beyond the charismatic summit sponge ground on an arctic seamount (Schulz Bank, Arctic Mid-Ocean Ridge) |url=https://linkinghub.elsevier.com/retrieve/pii/S0967063722002333 |journal=Deep Sea Research Part I: Oceanographic Research Papers |language=en |volume=191 |pages=103920 |doi=10.1016/j.dsr.2022.103920}}</ref> |
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== References == |
== References == |
Revision as of 19:12, 11 December 2023
The Mohns Ridge is an ultraslow-spreading segment of the Mid-Atlantic Ridge located to the north of Jan Mayen in the Arctic Ocean.[1] It is bounded to the south by the Jan Mayen fracture zone, and transitions to Knipovich Ridge in the north-east.
Geology
The ridge started forming 53 My ago, as the Greenland Plate and Eurasian Plate started separating. Four separate axial volcanic ridges have been discovered along Mohns Ridge.[2]
Notable features
Several active and non-active hydrothermal vent fields have been located along Mohns Ridge. In 2008, a black smoker vent field named Loki's Castle was discovered along one of the axial volcanic ridges in the area.[3]
The Schulz Bank seamount is located on the northern part of the ridge, as Mohns Ridge transitions into the Knipovich Ridge.[4]
References
- ^ "Marine Regions · Mohns Ridge (Ridge)". www.marineregions.org. Retrieved 2023-01-16.
- ^ Reimers, Hauke (2017). The Morphology of the Mohn's Ridge - with Special Focus on Listric and Detachment Faults and their Link to the Formation of Seafloor-massive Sulfides (Master thesis thesis). NTNU.
- ^ Pedersen, Rolf B.; Rapp, Hans Tore; Thorseth, Ingunn H.; Lilley, Marvin D.; Barriga, Fernando J. A. S.; Baumberger, Tamara; Flesland, Kristin; Fonseca, Rita; Früh-Green, Gretchen L.; Jorgensen, Steffen L. (2010-11-23). "Discovery of a black smoker vent field and vent fauna at the Arctic Mid-Ocean Ridge". Nature Communications. 1 (1): 126. Bibcode:2010NatCo...1..126P. doi:10.1038/ncomms1124. ISSN 2041-1723. PMC 3060606. PMID 21119639.
- ^ Meyer, H.K.; Davies, A.J.; Roberts, E.M.; Xavier, J.R.; Ribeiro, P.A.; Glenner, H.; Birkely, S.-R.; Rapp, H.T. (2023-01). "Beyond the tip of the seamount: Distinct megabenthic communities found beyond the charismatic summit sponge ground on an arctic seamount (Schulz Bank, Arctic Mid-Ocean Ridge)". Deep Sea Research Part I: Oceanographic Research Papers. 191: 103920. doi:10.1016/j.dsr.2022.103920.
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Further reading
- Dauteuil, O.; Brun, J.-P. (1996-08-01). "Deformation partitioning in a slow spreading ridge undergoing oblique extension: Mohns Ridge, Norwegian Sea". Tectonics. 15 (4): 870–884. doi:10.1029/95TC03682. ISSN 1944-9194.