those are tecktonic plates which are delicate.when they move crackes occur.
when tecktonic plates move under water it creates viberations which causes tsunamis.
The crack in the ocean floor where magma rises is called a mid-ocean ridge. At these underwater mountain ranges, tectonic plates separate and magma rises to fill the gap, creating new oceanic crust. This process is known as seafloor spreading.
Old ocean floor is destroyed and absorbed by the Earth at subduction zones, where tectonic plates collide and one plate is forced beneath the other. The remelting occurs beneath volcanic arcs, where the subducted crust melts and rises to the surface as magma, leading to the formation of new crust.
When magma rises through sea floor rifts, it cools and solidifies into new oceanic crust as part of the process known as seafloor spreading. This creates new crust at the boundaries of tectonic plates, contributing to the continual movement and renewal of the Earth's outer shell.
It is called a volcano.
The ocean floor spreads due to tectonic processes at mid-ocean ridges, where new crust is formed as magma rises and solidifies. This process is balanced by subduction, where older oceanic crust is pushed back into the mantle at ocean trenches. As a result, while new material is created, it is offset by the recycling of crust, keeping the overall size of the Earth stable. Thus, the continuous creation and destruction of crust maintain equilibrium in Earth's dimensions.
The crack in the ocean floor where magma rises is called a mid-ocean ridge. At these underwater mountain ranges, tectonic plates separate and magma rises to fill the gap, creating new oceanic crust. This process is known as seafloor spreading.
In some areas along the Mid- Ocean Ridge, the gigantic plates that form the Earth's crust are moving apart, creating crack and crevices in the ocean floor. Seawater seeps into these openings and id heated by the molten rock, or magma, that lies beneath the Earth's crust. As the water is heated, it rises and seeks a path back out into the ocean through an opening in the seafloor.
It causes what we call "sea-floor spreading." Sea-floor spreading is the process in which the ocean floor is extended when two plates move apart. As the plates move apart, the rocks break and form a crack between the plates. Earthquakes occur along the plate boundary. Magma rises through the cracks and seeps out onto the ocean floor like a long, thin, undersea volcano.
a hydrothermal vent
Old ocean floor is destroyed and absorbed by the Earth at subduction zones, where tectonic plates collide and one plate is forced beneath the other. The remelting occurs beneath volcanic arcs, where the subducted crust melts and rises to the surface as magma, leading to the formation of new crust.
A mid-ocean ridge is an undersea mountain chain where new ocean floor is produced through volcanic activity. Here, magma rises up from the Earth's mantle and solidifies as it cools, leading to the formation of new crust.
A seamount forms through volcanic activity, where magma rises from beneath the Earth's crust to create a mountain-like structure on the ocean floor. Over time, as the volcano becomes inactive and cools, it sinks below the ocean surface but remains as a seamount.
Magma rises to the surface at mid-ocean ridges due to the process of seafloor spreading. As two tectonic plates move apart, hot magma from the mantle wells up to fill the gap, creating new oceanic crust. This process is responsible for the formation of mid-ocean ridges and contributes to the Earth's continuous process of plate tectonics.
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.
Magma rises and slidifies and creates a new crust.