When divergence occurs in the oceanic lithosphere, it leads to the formation of mid-ocean ridges where new crust is created as magma rises from the mantle and solidifies. This process is responsible for the spreading of the ocean floor and the formation of new oceanic crust.
At a transform fault boundary, two tectonic plates slide past each other horizontally. This movement can cause earthquakes as the plates grind against each other. There is no creation or destruction of crust at this type of boundary.
The lithosphere sinking into the mantle occurs at a convergent plate boundary, specifically in subduction zones. In these regions, one tectonic plate is forced beneath another, typically an oceanic plate descending beneath a continental plate or another oceanic plate. This process leads to the formation of deep ocean trenches and volcanic arcs. The subduction of the lithosphere is a key driver of tectonic activity and geological phenomena associated with plate interactions.
Neither production nor consumption of lithosphere occurs at these boundaries.
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.
transform fault boundary
transform fault boundary
When two plates grind past each other without creating or destroying lithosphere, they form a transform plate boundary. This type of boundary can result in earthquakes due to the build-up of stress along the fault line where the two plates are in contact. One well-known example of a transform plate boundary is the San Andreas Fault in California.
At a transform plate boundary, plates slide past each other horizontally in opposite directions without creating or destroying lithosphere. This movement is characterized by lateral shearing, where the plates grind against each other, causing earthquakes.
When a divergent boundary occurs beneath oceanic lithosphere, the rising convection current below lifts the lithosphere producing a mid-ocean ridge!!!Hope i helped.
The boundary between continental crust and oceanic crust occurs at the base of the lithosphere. This boundary is known as the Mohorovičić discontinuity, or Moho. It separates the less dense continental crust from the more dense oceanic crust below.
When divergence occurs in the oceanic lithosphere, it leads to the formation of mid-ocean ridges where new crust is created as magma rises from the mantle and solidifies. This process is responsible for the spreading of the ocean floor and the formation of new oceanic crust.
At a transform fault boundary, two tectonic plates slide past each other horizontally. This movement can cause earthquakes as the plates grind against each other. There is no creation or destruction of crust at this type of boundary.
The lithosphere sinking into the mantle occurs at a convergent plate boundary, specifically in subduction zones. In these regions, one tectonic plate is forced beneath another, typically an oceanic plate descending beneath a continental plate or another oceanic plate. This process leads to the formation of deep ocean trenches and volcanic arcs. The subduction of the lithosphere is a key driver of tectonic activity and geological phenomena associated with plate interactions.
divergent boundary
A place where the crust of the lithosphere has fractured is known as the asthenosphere. The asthenosphere is located below the lithosphere and is where plate tectonic movement occurs.
When a wave strikes a boundary, it can undergo reflection, transmission, or absorption. Reflection occurs when the wave bounces off the boundary and travels in the opposite direction. Transmission happens when the wave passes through the boundary and continues traveling in the same medium. Absorption occurs when the wave's energy is absorbed by the boundary material.