Topographic maps disclose the areas of huge earthquakes and indicate the borders of the 12 significant tectonic plates. For example, the Pacific bowl is bounded through the earthquake area of brand-new Zealand, new Guinea, the Mariana Islands, Japan, Kamchatka, the Aleutian Islands, western phibìc America, the eastern Pacific Rise, and the Pacific-Antarctic Ridge.

You are watching: At which of these convergent plate boundaries are active volcanoes not likely to be located?


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Major resources for this expedition was detailed by NOAA Ocean exploration Program and NOAA Vents Program; video clip clips edited by invoice Chadwick, Oregon State University/NOAASee all videos for this article

The volcanoes top top the western and northern margin the the Pacific plate (New Zealand, new Guinea, Mariana Islands, Japan, Kamchatka, and also the Aleutian Islands) space all subduction volcanoes. The rift volcanoes are largely surprise along the submarine stakes of the east Pacific Rise and the Pacific-Antarctic Ridge at depths of 2 come 3 kilometres (1.2 come 1.9 miles) listed below sea level. The Cascade volcanoes in the northwestern united States and also the volcanoes in Mexico and main America are pertained to the subduction under the phibìc American key of the small Juan de Fuca and Cocos plates, which space on the east side that the Pacific Plate. Similarly, the volcanoes of the Andes are concerned the subduction that the Nazca Plate in ~ the south American Plate.

Conceptual models of exactly how subduction and rift volcanoes may form are presented schematically in the diagram and also in the video. The the 1,450 volcanoes detailed in the table of landform types, 80 percent take place along subduction zones, and 15 percent take place along rift zones. This percentages are somewhat misleading, however, since most of earth rift area are around 2 to 3 km (1.2 come 1.9 miles) below sea level, whereby volcanic activity is tough to detect. In ~ those depths energetic submarine volcanoes have actually yet to it is in observed, though countless hydrothermal areas have been uncovered along submarine rift area by research submersibles. Iceland, a segment that the Mid-Atlantic Ridge that emerges above sea level, has actually 70 volcanoes that have actually erupted throughout the previous 10,000 years. If this is a common number for a rift system, there may be several thousand potentially active volcanoes along the oceanic ridges that room the surface ar expressions the the people rift system.

Subduction volcanoes

As one oceanic plate is subducted in ~ a continent plate, seafloor sediments well-off in water and also carbon dioxide are carried beneath the overriding plate. This compounds might act together fluxes, to reduce the melt temperature of magma. Back the procedure is not clearly understood, magma apparently forms and rises through buoyancy from a depth of 100 to 200 km (60 to 120 miles). Subduction-zone volcanoes happen on the overriding plate and are counter inland from the actual key boundary follow me the ocean trench.

The rising subduction-zone magma is probably basaltic in composition and is formed by the partial melt of mantle rocks. Together the rising magma moves progressively up v the continental crust the the overriding plate, however, two points may occur to increase significantly the silica content of the magma. Crystallization that olivine and also pyroxene mineral from the basalt can leave the residual melt enriched in silica and also depleted in magnesium, iron, and calcium. This process is referred to as fractional crystallization. Also, basaltic magmas have sufficient excess warm to partly melt the continental hold rocks through which they space ascending. Since continental rocks space generally greater in silica, potassium, and sodium than are oceanic rocks, this process of assimilation and mixing can additionally play vital role in creating the wide range of compositions that happen in rocks indigenous subduction volcanoes.

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The additional gas contents of numerous magmas in ~ subduction volcanoes (which, coupled v their regularly high-viscosity magma, provides them dangerously explosive) might be defined by much more than one process. Additional water and also carbon dioxide might come indigenous both subducted seafloor sediments and also assimilated crustal rocks. Furthermore, any type of fractional crystallization has tendency to concentration volatile aspects in the residual melt. If volcanic gases kind separate fluid phases in ~ batches the ascending magma (as carbon dioxide gas is most likely to do), these liquid phases may ascend an ext rapidly 보다 the in its entirety magma body and also be focused in the top portion. Sudden development of these warm volcanic gases at atmospheric push is the obvious reason for the highly explosive nature of plenty of subduction volcanoes.