it makes mid-oceanic ridges
Sea floor spreading
A divergent plate boundary is where the sea floor spreads, such as along mid-ocean ridges. At these boundaries, tectonic plates move apart from each other, allowing magma to rise and create new crust.
Around divergent boundaries, land features such as rift valleys, volcanic mountains, and mid-ocean ridges can be found. These features are a result of tectonic plates moving apart, leading to the creation of new crust through volcanic activity and the stretching and thinning of the lithosphere.
Continental and Oceanic plates.
Three main structures form by convergent boundaries. There are three types of convergent boundaries, oceanic-oceanic, oceanic-continental, and continental- continental. Oceanic to oceanic boundaries form volcanic islands, because the two plates come together, one crust goes under, the other forms a mountain, and the lava from the crust that went under the other one goes through the mountain, making it a volcano. Oceanic- continental convergent boundaries form volcanoes, the continental crust form the mountain, the oceanice goes under and makes the lava that goes up through the mountain and makes a volcano. continental to continental boundaries form mountains. since both crusts are of the same density, they both shoot up and form a mountain.
Sea floor spreading
A rift zone on land, a mid ocean ridge under the ocean.
it is a tsunami or an under water volcano
Divergent boundaries are tectonic plate boundaries where two plates move away from each other. This movement results in the upwelling of magma from the mantle, creating new crust. Divergent boundaries are typically found along mid-ocean ridges.
A divergent plate boundary is where the sea floor spreads, such as along mid-ocean ridges. At these boundaries, tectonic plates move apart from each other, allowing magma to rise and create new crust.
Around divergent boundaries, land features such as rift valleys, volcanic mountains, and mid-ocean ridges can be found. These features are a result of tectonic plates moving apart, leading to the creation of new crust through volcanic activity and the stretching and thinning of the lithosphere.
Continental and Oceanic plates.
Melting of material under divergent plate boundaries is primarily caused by decompression of rock as tectonic plates move apart, reducing pressure on the underlying mantle and allowing rock to melt. This process creates magma that rises to the surface, forming new crust along the mid-ocean ridges.
Three main structures form by convergent boundaries. There are three types of convergent boundaries, oceanic-oceanic, oceanic-continental, and continental- continental. Oceanic to oceanic boundaries form volcanic islands, because the two plates come together, one crust goes under, the other forms a mountain, and the lava from the crust that went under the other one goes through the mountain, making it a volcano. Oceanic- continental convergent boundaries form volcanoes, the continental crust form the mountain, the oceanice goes under and makes the lava that goes up through the mountain and makes a volcano. continental to continental boundaries form mountains. since both crusts are of the same density, they both shoot up and form a mountain.
the most famous divergent fault is the san Andreas faultEDIT: Actually, the San Andreas Fault is a Transform boundary. A Transform Boundary is when two plates are rubbing against each other while going opposite ways. A Divergent Boundary is when two plates move away from each other. Scientists have not pinpointed and named a Divergent Boundary but Divergent Boundaries usually occur under water in the sea, also called Sea Floor Spreading.
The 3 general types are constructive, destructive, and conservative boundaries. Constructive (divergent) - plates move away from each other, typically creating a rift Destructive (convergent) - one plate will be subducted, or continental plates collide Conservative (transform) - plates grind past each other, stalling and slipping
There are three main types of plate boundaries: divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally. Each type of boundary can result in different geological features and processes, such as rift valleys at divergent boundaries, mountain ranges at convergent boundaries, and earthquakes at transform boundaries.