Ophiolites are created under mid-ocean ridges and represent a vertical section beneath a ridge system. One of the best ophiolites is seen in the Troodos range in Southern Cyprus. The topmost layer is invariably pillow lavas which are usually basaltic lavas that were erupted under water.
Then as an ocean closes due to subduction, part of the ocean ridge system MAY be scrapped off and by a process called OBDUCTION be forced onto the plate which is over-riding which is usually the continental plate. If the processes cause the obducted mass to rise above sea level the result is an ophiolite.
So whilst they are created at mid-ocean ridges they are the result of subduction.
Both subduction zones and spreading centers.
It was formed from converget bounderies.
It was formed from converget bounderies.
Subduction.
False. Hotspot volcanoes form above mantle plumes, which are localized upwellings of hot mantle material. Subduction zone volcanoes form due to the subduction of one tectonic plate beneath another, resulting in magma generation due to the melting of the subducted plate.
Composite or stratovolcanoes typically form along subduction zones. These volcanoes are characterized by their steep-sided profile, explosive eruptions due to the presence of viscous magma, and alternating layers of lava flows and volcanic ash. Subduction zones are where one tectonic plate slides beneath another plate, leading to magma formation and volcanic activity.
Subduction zones form along some tectonic plate boundaries. Of the three general types of tectonic plate boundaries, we will see them form at some (but not all) of what are called convergent plate boundaries.
In subduction zones, the scraping lithosphere can form a ridged springboard that is loaded by the subducting lithosphere. When the load is enough to overcome the friction of subduction, it can unload within minutes causing massive earthquakes along the fault.
a ocean and a lake
by plate tectonics
Volcanic arcs and oceanic trenches commonly form at subduction zones.
Japan formed as a result of a subduction zone.