A convergent boundary creates no new lithosphere, as it involves the collision of tectonic plates, leading to one plate being forced beneath another in a process called subduction. This results in the recycling of existing lithosphere rather than the formation of new material. Instead of producing new crust, convergent boundaries often lead to geological features like mountain ranges and deep ocean trenches.
As the lithosphere moves away from a divergent plate boundary, its thickness generally increases. This occurs because new oceanic crust is formed at the boundary through volcanic activity and then cools and solidifies as it moves away from the heat source. As it ages, the lithosphere becomes denser and thicker due to cooling and the accumulation of sediments. This process leads to a gradual thickening of the lithosphere away from the divergent boundary.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
A divergent plate boundary creates new land like the seafloor at the mid-Atlantic ridge. At these boundaries, tectonic plates move away from each other, allowing magma to rise up and solidify, forming new oceanic crust. As the crust cools and spreads outward, it creates new land in the form of the ocean floor.
New oceanic lithosphere forms as a result of seafloor spreading at mid-ocean ridges. Magma rises from the mantle, solidifies at the mid-ocean ridge, and creates new oceanic crust. This process leads to the continuous expansion of the ocean floor.
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No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
It creates a divergent boundary.
creates new crust and allows magma to come through.
Divergent
A divergent plate boundary creates new land like the seafloor at the mid-Atlantic ridge. At these boundaries, tectonic plates move away from each other, allowing magma to rise up and solidify, forming new oceanic crust. As the crust cools and spreads outward, it creates new land in the form of the ocean floor.
New oceanic lithosphere forms as a result of seafloor spreading at mid-ocean ridges. Magma rises from the mantle, solidifies at the mid-ocean ridge, and creates new oceanic crust. This process leads to the continuous expansion of the ocean floor.
The 'South Island'. A collision boundary.
Magma rises and slidifies and creates a new crust.
Magma rises and slidifies and creates a new crust.
Magma rises and slidifies and creates a new crust.
check out nasa dude have some common sense stupid you
Magma rises and slidifies and creates a new crust.