earthquake ...
At transform plate boundaries, the lithosphere slides past each other horizontally. This movement can cause earthquakes as the tectonic plates experience frictional forces. The lithosphere is neither created nor destroyed at transform plate boundaries.
Oceanic lithosphere is destroyed when it is subducted at a convergent plate boundary and forced into the mantle where it melts. You shouldn't use the internet to look up answers on a test. You should use your notes and textbook! DW Thanks for the answer but um, What about people in online school, where the only "textbook" you get is an agenda? yeah the awnser for Gradpoint is Convergent Boundary
Yes, the amount of lithosphere formed at mid-ocean ridges through seafloor spreading is balanced by the amount destroyed at subduction zones. This process, known as plate tectonics, maintains a relatively constant amount of lithosphere on Earth's surface.
The process of plate tectonics drives the creation and destruction of lithosphere. As new lithosphere is formed at mid-ocean ridges through seafloor spreading, older lithosphere is consumed at subduction zones, creating a balance between formation and destruction over time. This equilibrium maintains a relatively constant amount of lithosphere on Earth.
the lithosphere is the solid upper part of the mantle and the crust, which are spilt up into plates on the earth surface, which are constantly moving. at destructive plate boundaries the plates can get subducted and "recycled" into the mantle, hence lithosphere is destroyed. at mid ocean ridges new crust (lithopshere) is constantly being made. this all leads to the dynamic and continuous cycles of lithosphere being destroyed and created, hence continually changing.
dicks
Lithosphere is neither destroyed nor created.
It destroyed the land...
No, oceanic lithosphere is not destroyed at a transform fault boundary. Transform boundaries involve horizontal sliding of plates past each other, causing lateral movement rather than creation or destruction of lithosphere.
The location wherein most lithosphere is destroyed are the subduction zones. These zones are along the Ring of Fire where Asia and the American continents are closing together.
At transform plate boundaries, the lithosphere slides past each other horizontally. This movement can cause earthquakes as the tectonic plates experience frictional forces. The lithosphere is neither created nor destroyed at transform plate boundaries.
Oceanic lithosphere is destroyed when it is subducted at a convergent plate boundary and forced into the mantle where it melts. You shouldn't use the internet to look up answers on a test. You should use your notes and textbook! DW Thanks for the answer but um, What about people in online school, where the only "textbook" you get is an agenda? yeah the awnser for Gradpoint is Convergent Boundary
Yes, the amount of lithosphere formed at mid-ocean ridges through seafloor spreading is balanced by the amount destroyed at subduction zones. This process, known as plate tectonics, maintains a relatively constant amount of lithosphere on Earth's surface.
The lithosphere is primarily destroyed by tectonic processes such as subduction, where one tectonic plate is forced beneath another, leading to melting in the mantle. Additionally, volcanic activity can contribute to the destruction of the lithosphere as molten rock (magma) erupts and alters the surface. Erosion and weathering also play a role in breaking down lithospheric materials over time.
Yes, in convergent boundaries, lithosphere crust can be destroyed. When two tectonic plates collide, typically an oceanic plate subducts beneath a continental plate or another oceanic plate, leading to the bending and melting of the subducted crust. This process can result in the formation of deep ocean trenches and volcanic arcs, effectively recycling the lithosphere into the mantle.
The process of plate tectonics drives the creation and destruction of lithosphere. As new lithosphere is formed at mid-ocean ridges through seafloor spreading, older lithosphere is consumed at subduction zones, creating a balance between formation and destruction over time. This equilibrium maintains a relatively constant amount of lithosphere on Earth.
Most lithosphere is created at divergent plate boundaries, where tectonic plates move away from each other. This can occur along mid-ocean ridges or rift valleys on continents. Magma rises to the surface, cools, and solidifies to form new lithosphere.