The thin crust of a rift zone causes melting in the upper mantle, resulting in volcanic activity.
so magma can cool below earth surface to from igneous rocks.
The thinned crust in rift zones results in the formation of magma (molten rock) in the upper mantle, which then rises through the crust. As a result, rift zones often have active volcanoes, which form new igneous rocks.
There are many explanation to your question. The most abundant type of rocks in collision zones are metamorphic rocks. But if there is a igneous it can as a result of convergence boundaries. In subduction zones where rising magma are penetrate through weaker rocks to form form lava and when solidified forms igneous rocks. You can also find them in accretion zones. Where 2 continental plates are accreted due to plate movement. They are not newly formed igneous. they have been there for years before accretion.
The thin crust of a rift zone causes melting in the upper mantle, resulting in volcanic activity.
Rift zones are lowlands composed of igneous rock.
Igneous rocks form only in certain places. Fractionation occurs mostly where tectonic plates are either moving apart at mid ocean ridges or pushing together at subduction zones.
Usually deep underground from heat and pressure, at regional metamorphic zones in areas of continental collisions, and in contact zones where parent rock is metamorphosed from proximity to an intrusive igneous body.
Intrusive igneous rocks form beneath the Earth's surface in settings like magma chambers and batholiths. Extrusive igneous rocks form on the Earth's surface from volcanic eruptions, such as at mid-ocean ridges, subduction zones, and hot spots.
Three methods of intrusive igneous rock formation are magma cooling and solidifying deep within the Earth's crust, magma forcing its way into existing rock formations and solidifying, and magma being injected into cracks and crevices in the surrounding rocks and cooling to form igneous rocks.
Yes, andesitic rock is indeed an igneous rock that has a composition situated between basaltic and granitic rocks. It typically contains a moderate amount of silica, ranging from about 57% to 63%, which gives it characteristics that are intermediate between the two. Andesitic rocks are commonly found in volcanic arcs and are often associated with subduction zones.
At a convergent boundary, the processes of subduction, where one tectonic plate is forced beneath another, can lead to the formation of metamorphic rocks such as schist and gneiss. Additionally, the intense heat and pressure generated by the collision of two plates can cause the melting of rocks, leading to the formation of igneous rocks like granite.
The thin crust of a rift zone causes melting in the upper mantle, resulting in volcanic activity.