Subduction. This process occurs at convergent plate boundaries where one lithospheric plate is forced beneath another due to differences in density, causing earthquakes and volcanic activity.
The kind of plate boundary where one lithospheric plate slides under another is a convergent boundary. This process is called subduction.
A convergent plate boundary involves one lithospheric plate sliding under another, leading to subduction zones where one plate is forced beneath the other. This process is associated with the formation of deep ocean trenches and volcanic arcs.
The downward movement of a lithospheric plate into the asthenosphere is known as subduction. This process occurs at convergent plate boundaries where one plate is forced beneath another due to differences in density. Subduction can result in the formation of deep oceanic trenches and volcanic activity.
The answer is subduction.
A continental plate is colliding with another continental plate, causing upward motion. A lithospheric plate is colliding with another lithospheric plate of similar bouyancy, causing upward motion.
A subduction zone is a region where one lithospheric plate is being forced beneath another. This process is caused by the convergence of tectonic plates, leading to the formation of deep oceanic trenches and volcanic arcs. Subduction zones are associated with intense seismic activity and volcanic eruptions.
The Cascade Range was formed by the subduction of the Juan de Fuca plate beneath the North American plate. This process created volcanic activity along the subduction zone, leading to the formation of the Cascade volcanoes. The range extends from northern California to British Columbia, with peaks such as Mount Rainier and Mount Hood.
The last person to answer was a complete and total idiot. The correct answer is the Pacific Plate.
Subduction is the process where one tectonic plate moves beneath another plate into the Earth's mantle at a convergent boundary. This can lead to the formation of deep ocean trenches and volcanic activity. It is a fundamental process in plate tectonics that drives the movement and interaction of Earth's lithospheric plates.
When one tectonic plate moves beneath another plate, it creates a subduction zone. This happens because the descending plate is denser and heavier, causing it to sink into the mantle beneath the overriding plate. This process leads to the formation of a deep trench and can trigger earthquakes and volcanic activity.
The principle behind this phenomenon is known as plate tectonics, where lithospheric plates float on the semi-fluid asthenosphere. When one plate subducts beneath another, it forms a convergent boundary. This process can lead to the formation of deep ocean trenches, volcanic arcs, and seismic activity.