Seafloor Spreading.
The process is called "subduction." It occurs when one tectonic plate moves beneath another at a convergent boundary, where the oceanic plate is forced down into the mantle at a subduction zone. This process leads to the recycling of old oceanic crust back into the mantle.
The process is called subduction. Subduction occurs at convergent plate boundaries when one tectonic plate moves beneath another and sinks into the mantle. This process is crucial for the recycling of Earth's lithosphere.
The crust is the outer layer of the lithosphere.
The process in which an oceanic plate sinks and pulls the rest of the tectonic plate with it is called subduction. This occurs at convergent plate boundaries where an oceanic plate collides with a continental or another oceanic plate, leading to the denser oceanic plate being forced beneath the lighter plate. As the oceanic plate descends into the mantle, it creates a trench and can trigger geological activity such as earthquakes and volcanic eruptions. This process is a key component of the Earth's tectonic cycle and contributes to the recycling of the lithosphere.
Seafloor Spreading.
Continental and oceanic
This process is called seafloor spreading. It occurs at mid-ocean ridges where tectonic plates move apart, allowing magma to rise from the mantle and solidify as new oceanic lithosphere. As the plates continue to separate, the new lithosphere gets pushed away from the ridge, creating a continuous cycle of formation and movement.
The process of thrusting oceanic lithosphere into the mantle along a convergent plate boundary is called subduction. This occurs when one tectonic plate is forced below another due to their collision, leading to the recycling of Earth's crust and the formation of volcanic arcs.
The process is called "subduction." It occurs when one tectonic plate moves beneath another at a convergent boundary, where the oceanic plate is forced down into the mantle at a subduction zone. This process leads to the recycling of old oceanic crust back into the mantle.
This process is called seafloor spreading. As magma rises from the mantle to the surface at mid-ocean ridges, it cools and solidifies to form new oceanic lithosphere. This continuous process helps in the expansion of the ocean basins and the movement of tectonic plates.
Slab Pull Force occurs when a denser oceanic plate is forced beneath a less dense continental plate or oceanic plate in a process called subduction. It's the force caused by suction of the cold dense lithosphere into the asthenosphere at destructive margins. Basically, because lithosphere is denser than asthenosphere, there is gravitational imbalance which is passed on to the crust. this causes the lithosphere to be sucked inwards at the oceanic trenches into deep asthenosphere.
The process is called subduction. Subduction occurs at convergent plate boundaries when one tectonic plate moves beneath another and sinks into the mantle. This process is crucial for the recycling of Earth's lithosphere.
The crust is the outer layer of the lithosphere.
A mid-ocean ridge is where magma pushes up on oceanic lithosphere, creating new oceanic crust as the magma solidifies. The heat from the magma causes the lithosphere to rise and spread apart, resulting in seafloor spreading. This process is fundamental in plate tectonics theory.
The process in which an oceanic plate sinks and pulls the rest of the tectonic plate with it is called subduction. This occurs at convergent plate boundaries where an oceanic plate collides with a continental or another oceanic plate, leading to the denser oceanic plate being forced beneath the lighter plate. As the oceanic plate descends into the mantle, it creates a trench and can trigger geological activity such as earthquakes and volcanic eruptions. This process is a key component of the Earth's tectonic cycle and contributes to the recycling of the lithosphere.
The crust and the upper mantle are a geological part of the earth called the lithosphere. There are 2 parts of the lithosphere: the oceanic lithosphere, which is made up of land underneath water, and the continental lithosphere, which is the the part made of just land. The lithosphere lies on top of the asthenosphere. The lithosphere is made up of tectonic plates, which are pieces of land floating on the lithosphere.