The magma spills over the ridge and pushes the old sea floor away toward a subduction zone where the old sea floor melts.
Magma erupts along mid ocean ridges forming new ocean floor. Mid ocean ridges are found at divergent boundaries where two ocean plates are pushing apart.
It is a place where volcanism or hot water heated by the underlying magma erupts on the ocean floor.
Nothing . . . tsunamis are ocean waves, not volcanoes.
The magma spills over the ridge and pushes the old sea floor away toward a subduction zone where the old sea floor melts.
In sea floor spreading, molten material rises from the mantle and erupts along mid-ocean ridges. These underwater mountain ranges serve as the sites where tectonic plates diverge, allowing magma to flow up and solidify, creating new oceanic crust. As this process continues, it pushes older crust away from the ridge, gradually expanding the ocean floor.
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.
Basaltic magma erupts along mid-ocean ridges primarily due to tectonic plate divergence, which creates space for magma to rise from the mantle. As the plates pull apart, the pressure decreases, allowing the mantle rock to partially melt and form basaltic magma. The relatively low viscosity of basaltic magma facilitates its ascent, leading to frequent eruptions and the formation of new oceanic crust at these ridges. Additionally, the continuous supply of heat from the mantle ensures ongoing volcanic activity in these regions.
Magma is extruded as lava at the mid-ocean ridges when they are pulled apart.
magma comes through the ocean surface and makes volcanoes
it makes more magma.
Basaltic magma is produced at the coolest temperatures because it has a lower silica content and therefore has a lower melting point compared to other types of magma. This type of magma typically erupts quietly and forms basaltic rock, such as the kind found at mid-ocean ridges.
Magma that has bubbled up through the crack in the Earth's surface.