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This type of boundary is called a convergent boundary or subduction zone, where the oceanic plate is pushed beneath the continental plate. The descending oceanic plate melts due to the heat and pressure, leading to volcanic activity and the formation of volcanic arcs.
Subduction zones, trenches and volcanic islands: the boundary that is oceanic. Trenches and volcanic islands: an oceanic-continental boundary. Folded mountain ranges: a continental and continental collision.
A passive continental margin is not tectonically active, meaning it does not experience significant geological activity like earthquakes or volcanic eruptions. In contrast, an active continental margin is located near a tectonic plate boundary, leading to geological activity such as subduction zones, earthquakes, and volcanic eruptions.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
A constructive boundary is also known as a divergent boundary. It is a tectonic plate boundary where plates move away from each other, resulting in the formation of new crust through volcanic activity and the upwelling of magma from within the Earth's mantle.
Convergent Boundary (Subduction Zone)
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This type of boundary is called a convergent boundary or subduction zone, where the oceanic plate is pushed beneath the continental plate. The descending oceanic plate melts due to the heat and pressure, leading to volcanic activity and the formation of volcanic arcs.
Subduction zones, trenches and volcanic islands: the boundary that is oceanic. Trenches and volcanic islands: an oceanic-continental boundary. Folded mountain ranges: a continental and continental collision.
continental volcanic arc
Oceanice oceanic has a trench, which is usually the deepest part of the ocean. It also has a volcanic island. That is how Islands are found in the center of oceans. oceanic convergent has similar features but do not have islands but instead volcanic arc on the continents.
A passive continental margin is not tectonically active, meaning it does not experience significant geological activity like earthquakes or volcanic eruptions. In contrast, an active continental margin is located near a tectonic plate boundary, leading to geological activity such as subduction zones, earthquakes, and volcanic eruptions.
The area of volcanic activity far from a tectonic plate boundary is called a "hotspot." Hotspots are characterized by plumes of hot mantle material that can create volcanic islands and chains, such as the Hawaiian Islands. These volcanic activities occur independently of tectonic plate movements, often resulting in long-lived eruptions in a localized area.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
The hot spot volcanic activity is not dependent on the subduction and melting of oceanic crust. The hot spot simply appears to be a non-moving place in the Earth's mantle where heat rises from the interior.
A constructive boundary is also known as a divergent boundary. It is a tectonic plate boundary where plates move away from each other, resulting in the formation of new crust through volcanic activity and the upwelling of magma from within the Earth's mantle.
Transform boundaries do not produce volcanic activity.