Shifting of Tectonic plates away from each other.
Ocean floor spreading is considered a constructive process. It occurs at mid-ocean ridges where tectonic plates diverge, leading to the formation of new oceanic crust as magma rises and solidifies. This process adds material to the ocean floor and contributes to the growth of ocean basins. In contrast, destructive processes, such as subduction, involve the recycling of crust back into the mantle.
New crust is formed at mid-ocean ridges through a process called seafloor spreading. Magma rises to the surface, cools, and solidifies, creating new oceanic crust. This process continually adds new material to the ocean floor, expanding the Earth's crust.
The mechanism responsible for producing new oceanic crust between two diverging plates is seafloor spreading. Magma rises up from the mantle at mid-ocean ridges, solidifies upon reaching the seafloor, and forms new crust. As the plates move apart, this process continuously adds new material to the ocean floor.
The process that forms new seafloor is called seafloor spreading. It occurs at mid-ocean ridges where new oceanic crust is created through volcanic activity. As magma rises and solidifies, it adds to the seafloor, pushing older crust away from the ridge and creating a continuous process of crust formation.
Rocks from mid-ocean ridges originate from the Earth's mantle, where molten rock, or magma, rises to the surface along tectonic plate boundaries. As tectonic plates diverge, this magma erupts and solidifies, forming new oceanic crust. The ongoing process of seafloor spreading continuously adds new material to the ocean floor, resulting in the creation of basaltic rocks characteristic of mid-ocean ridges.
sea floor spreading
Volcanic eruptions are one process that adds new material to crust. Lava from the volcanoes eventually cool, forming new land. Sea floor spreading also adds new material to the crust.
Sea floor spreading mean the process by which molten material adds new oceanic crust to the ocean floor
DA ANSWER ISseafloor spreadingThe_process_by_which_molten_material_adds_new_oceanic_crust_to_the_ocean_floor_is_calledThe_process_by_which_molten_material_adds_new_oceanic_crust_to_the_ocean_floor_is_called
sea-floor spreading
Ocean floor spreading is considered a constructive process. It occurs at mid-ocean ridges where tectonic plates diverge, leading to the formation of new oceanic crust as magma rises and solidifies. This process adds material to the ocean floor and contributes to the growth of ocean basins. In contrast, destructive processes, such as subduction, involve the recycling of crust back into the mantle.
Sedimentation.
sea floor spreading
True. Sea-floor spreading occurs at mid-ocean ridges where tectonic plates are moving apart, allowing magma from the mantle to rise and solidify, forming new crust. This process continuously adds new material to the ocean floor, contributing to the expansion of the ocean basin over time.
the formation of new oceanic crust. Magma rises to the surface at mid-ocean ridges, solidifies upon contact with seawater, and creates new crust as it spreads horizontally away from the ridge axis. This process continually adds new crust to the ocean floor as tectonic plates move apart.
New crust is formed at mid-ocean ridges through a process called seafloor spreading. Magma rises to the surface, cools, and solidifies, creating new oceanic crust. This process continually adds new material to the ocean floor, expanding the Earth's crust.
sedimentation