Usually referred to as a "fault".
Joints
faults
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.
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.
Plutonic or intrusive igneous rock
plateau
These are obviously called the "polar zones," the Arctic and the Antarctic.
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 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.
An example of a mitigation activity is installing a flood barrier to reduce the impact of flooding on a community. This proactive measure helps prevent damage to properties and infrastructure by diverting or containing floodwaters.
There are three methods of intrusive igneous rock formation. Igneous rock can form at mid ocean ridges, subduction zones, and at the continental crust if it is pushed together.
Earth's polar zones are also called the Earth's Frigid Zones.
Rift zones are lowlands composed of igneous rock.
because it is
so magma can cool below earth surface to from igneous rocks.
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.
Both of these zones are called polar regions.
Building earthquake-resistant structures n earthquake zones is a mitigation activity.
The thin crust of a rift zone causes melting in the upper mantle, resulting in volcanic activity.