Azores hotspot

From Wikipedia, the free encyclopedia
Jump to navigation Jump to search
The Azores hotspot is marked 1 on map.

The Azores hotspot is a volcanic archipelago in the Northern Atlantic Ocean. The Azores is relatively young and is associated with a bathymetric swell, a gravity anomaly and ocean island basalt geochemistry.[1] The Azores hotspot lies near the Mid-Atlantic Ridge, which lies just west of the hotspot.[2]

Geological area[edit]

The Azores domain comprises the Azores Plateau and the Azores archipelago (formed of 9 islands extending a distance of 480 km) which has been volcanically active for around 7 Myr. The archipelago lies on the lateral branch of the Mid-Atlantic Ridge near the junction of three major tectonic plates; the North American Plate, the Eurasian Plate and the African Plate.[3] This unique location causes the area to have ridge-hotspot interaction with a variation of volcanic processes.

The Azores Plateau[edit]

The Azores archipelago rises from Azores Plateau, which is an area of thickened oceanic crust thought to have formed over the last 20 Mya. Negative velocity S-wave anomalies have been mapped beneath the Azores in the upper 250–300 km. This has been suggested to be a signature of a plume that created the Azores Plateau.[3] Another theory is that the excess volcanism simply results from excess extension at this unusal triple junction.[4]

Hotspot–ridge relationships[edit]

The Mid Atlantic Ridge is a zone of extension that permits magma to rise, forming dikes and surface volcanism. areas of excess magmatism on the Mid Atlantic Ridge have been called "hotspots" e.g. the Azores. Gravity field modelling studies have shown that the crustal thickness in this area is 60% greater than normal and spreading ridge is elevated.[5] The "hotspot" is asymmetrical (north and south). It is thought that crust at ridges is formed by a combination of processes (magmatic and tectonic) with magma addition coming from short lived magma chambers.[6] The increased melt production within the mantle may have supported a longer lived magma chamber causing the crust to be thicker. However, the Mid Atlantic Ridge has also been shown to have affected the characteristics of the Azores Plateau. It has been suggested that the main volcanic ridges on the plateau were created at the Mid Atlantic Ridge spreading axis. The Azores "hotspot" has unique geomorphological characteristics displayed in the Azores Plateau, archipelago and the area of ridge that passes through it.

References[edit]

  1. ^ Gente P.; Dyment J.; Maia M.; Goslin J. (2003). "Interaction between the Mid-Atlantic Ridge and the Azores hot spot during the last 85 Myr: Emplacement and rifting of the hot spot-derived plateaus" (PDF). Geochemistry Geophysics Geosystems. 4 (10): 1–23. Bibcode:2003GGG.....4.8514G. doi:10.1029/2003GC000527. Archived from the original (PDF) on 2013-12-20.
  2. ^ Cannat, M.; Briais, A.; Deplus, C.; Escartin, J.; Georgen, J.; Lin, J.; Mercouriev, S.; Meyzen, C.; Muller, M.; Pouliquen, G.; Rabain, A. & da Silva, P. (1999). "Mid-Atlantic Ridge–Azores hotspot interactions: along-axis migration of a hotspot-derived event of enhanced magmatism 10 to 4 Ma ago" (PDF). Earth and Planetary Science Letters. 173 (3): 257–269. Bibcode:1999E&PSL.173..257C. doi:10.1016/S0012-821X(99)00234-4. Archived from the original (PDF) on 2013-12-20.
  3. ^ a b Silveria, G.; Stutzmann, E.; Davaille, A.; Montagner, J.; Mendes-Victor, L. & Sebai, A. (2006). "Azores hotspot signature in the upper mantle" (PDF). Journal of Volcanology and Geothermal Research. 156 (1–2): 23–34. Bibcode:2006JVGR..156...23S. doi:10.1016/j.jvolgeores.2006.03.022.
  4. ^ Smith, A. G. (2007). "A plate model for Jurassic to recent intraplate volcanism in the Pacific Ocean basin". In Plates, Plumes, and Planetary Processes, edited by G.R. Foulger and D.M. Jurdy, Geological Society of America Special Paper 530, Boulder, CO. 430: 471–496.
  5. ^ Bourdon, B.; Langmuir, C. H. & Zinder, A. (1996). "Ridge-hotspot interaction along the Mid-Atlantic Ridge between 37°30′ and 40°30′N: the UTh disequilibrium evidence". Earth and Planetary Science Letters. 142: 175–189. Bibcode:1996E&PSL.142..175B. doi:10.1016/0012-821x(96)00092-1.
  6. ^ Singh, S. C.; Crawford, W. C.; Carton, H.; Seher, T.; Combier, V.; Cannat, M.; Canales, J. P.; Dusunur, D.; Escartin, J. & Miranda, M. (2006). "Discovery of a magma chamber and faults beneath a Mid-Atlantic Ridge hydrothermal field" (PDF). Nature. 442 (7106): 1029–1032. Bibcode:2006Natur.442.1029S. doi:10.1038/nature05105. PMID 16943836. Archived from the original (PDF) on 2013-12-20.

External links[edit]