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.
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.
The sea-floor spreading begins at the mid-ocean ridge, which forms along a crack in the oceanic crust. Along the ridge, molten material that forms several kilometers beneath the surface, rises and erupts. At the same time, older rock moves outward on both sides of the ridge. As the molten material cools, it forms a strip of solid rock in the center of the ridge. When more molten material flows into the crack, it forms a new strip of rock.
The sea-floor spreading begins at the mid-ocean ridge, which forms along a crack in the oceanic crust. Along the ridge, molten material that forms several kilometers beneath the surface, rises and erupts. At the same time, older rock moves outward on both sides of the ridge. As the molten material cools, it forms a strip of solid rock in the center of the ridge. When more molten material flows into the crack, it forms a new strip of rock.
Pillow lava forms when molten lava erupts underwater and cools rapidly, creating characteristic pillow-like structures. This type of lava is commonly found along mid-ocean ridges, which are areas where sea-floor spreading occurs. The presence of pillow lava on the ocean floor is evidence of volcanic activity associated with sea-floor spreading.
The molten material then spreads out, pushing the older rock to both sides of the ridge. As the molten material cools, it forms a strip of solid rock in the center of the ridge. Then more molten material flows into the crack. The material splits apart the strip of solid rock that formed before, pushing it aside.
Typically the fragments are worn into rounded shapes.
The magma spills over the ridge and pushes the old sea floor away toward a subduction zone where the old sea floor melts.
ash particles, cinders, tephra, gases
Which part of the Earth's interior is spewed out in a volcanic eruption?
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.
False. Mountains that begin when molten material reaches Earth's surface and then cools and solidifies are known as volcanic mountains. Fault-blocked mountains are formed when tectonic forces cause the Earth's crust to be uplifted and tilted along faults.