Hot mantle rock rises to fill rift zones. When rock rises, a decrease in pressure causes hot mantle rock to melt and form magma.
At divergent boundaries, two plates move apart from each other and the space that this creates is filled with new crustal material sourced from molten magma that forms below.
Plates move apart at divergent boundaries, also known as spreading centers. This process is usually associated with the formation of new crust as magma rises from the mantle to fill in the gap created by the moving plates. An example of a divergent boundary is the Mid-Atlantic Ridge.
As the plates move away from each other at divergent boundaries, the lithosphere becomes thinner. A set of deep cracks form in the rift zone. The convection currents of the mantle can form a weak spot, and the heated, less dense magma rises up to fill the gap.Seafloor SpreadingMagma rises from magma chambers at the rifts in the sea floor. Cooling and hardening then occurs.
Basalts are produced on divergent plate boundaries because the extensional forces at these boundaries cause the mantle to melt, generating magma that rises to the surface and solidifies as basaltic rock. This process, known as decompression melting, occurs due to the reduced pressure on the mantle rocks as the tectonic plates move apart, leading to the formation of basaltic oceanic crust.
Magma rises and melts at divergent plate boundaries in the ocean due to the decompression melting that occurs as tectonic plates move apart. As the plates separate, pressure on the mantle decreases, causing the mantle to melt and create magma that rises to the surface, forming new oceanic crust.
Metamorphism typically occurs at convergent boundaries, where tectonic plates collide, and at divergent boundaries, where plates move apart. It also occurs at transform boundaries, where plates slide past each other horizontally. Metamorphism can also occur at hot spots, where magma from the mantle rises to the surface.
Hot mantle rock rises to fill rift zones. When rock rises, a decrease in pressure causes hot mantle rock to melt and form magma.
At divergent boundaries, two plates move apart from each other and the space that this creates is filled with new crustal material sourced from molten magma that forms below.
Magma from the mantle rises to fill the void created by plates pulling apart. This process can lead to the formation of new oceanic crust at mid-ocean ridges.
Plates move apart at divergent boundaries, also known as spreading centers. This process is usually associated with the formation of new crust as magma rises from the mantle to fill in the gap created by the moving plates. An example of a divergent boundary is the Mid-Atlantic Ridge.
divergent
Basalt is the type of igneous rock commonly produced at divergent plate boundaries. This rock forms from the solidification of magma that rises to the Earth's surface through the process of seafloor spreading, which occurs at divergent boundaries.
True. Oceanic lithosphere is created at divergent boundaries where tectonic plates move away from each other. Magma rises from the mantle to fill the gap and solidifies to form new oceanic crust.
As the plates move away from each other at divergent boundaries, the lithosphere becomes thinner. A set of deep cracks form in the rift zone. The convection currents of the mantle can form a weak spot, and the heated, less dense magma rises up to fill the gap.Seafloor SpreadingMagma rises from magma chambers at the rifts in the sea floor. Cooling and hardening then occurs.
Basalts are produced on divergent plate boundaries because the extensional forces at these boundaries cause the mantle to melt, generating magma that rises to the surface and solidifies as basaltic rock. This process, known as decompression melting, occurs due to the reduced pressure on the mantle rocks as the tectonic plates move apart, leading to the formation of basaltic oceanic crust.
Hot mantle rock rises where the plates are moving apart. This releases pressure on the mantle, which lowers its melting temperature. Lava erupts through long cracks in the ground, or fissures