When divergent boundary plates move apart, magma rises from the mantle to fill the gap, creating new oceanic crust. As the crust cools and solidifies, it forms a series of underwater mountain ranges known as mid-ocean ridges.
Plate boundaries, essentially, are the areas where two lithospheric plates meet. When this happens, one of three things can happen. Plates can move apart from each other, creating divergent boundaries. Plates can collide together, created convergent boundaries. Or plates can rub against each other in a parallel motion, created transform fault boundaries. Divergent boundaries, usually between two oceanic plates, creates an upswelling of magma from the lithosphere. Convergent boundaries, usually between oceanic and continental plates, causes the oceanic plate to subduct underneath the continental plate, leading to the destruction of seafloor. Transform fault boundaries neither destroy nor create lithosphere.
Mid-ocean ridges can form as new crust is created at divergent plate boundaries. Earthquakes can occur as the plates pull away from each other. New ocean basins can develop as the plates move apart.
The three types of interactions that occur at plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally.
The major types of plate tectonic boundaries are:Divergent Plate Boundary: The area where two plates are moving in relatively opposite directions and new crustal material is being created. Examples would be the mid-ocean ridges, and the East African Rift.Convergent Plate Boundary: The area where two tectonic plates are moving toward each other and one of two things happens; either the more dense plate subducts under the lighter plate and heads toward the mantle, or, if the plates are of similar density, they cause uplift and mountain forming events. Examples would be the oceanic to continental crustal collision creating the Andes Mountains, and the continental to continental crustal collision creating the Himalayan Mountains.Transform Plate Boundary: The area where two plates are grinding past each other, snapping into place from elastic rebound as they go, causing numerous earthquakes. The San Andreas Fault is an example of a transform plate boundary between the North American and Pacific plates.Convergent (plates are crashing together), divergent (plates are spreading apart), and transverse (plates are grinding past each other.) There are key structures that you get at each: Convergent boundaries can produce subduction or uplift, resulting in mountains and volcanoes. Divergent boundaries form mid-oceanic ridges and rift valleys. Transverse boundaries create faults, and are prone to earthquakes.They are all boundaries between or fractures within the Tectonic Plates forming the Earth's crust.A convergent boundary is that between two approaching plates; usually an ocean-floor plate being subducted beneath the continental plate as the ocean closes. This is happening now to the Pacific Ocean.A divergent boundary is the opposite: the fracture of plate into two parts moving away from each other. The break is closed by upwelling magma. E.g. The Mid-Atlantic Ridge - the Atlantic is presently widening away from this subsea mountain-range at a mean rate of about 25mm/yr.Transform boundaries, or Transform Faults, are shear fractures across the plate at roughly right-angles to the spreading-ridge from which the emanate. They represent the effect of unequal spreading forces. If you look at a relief map of the Atlantic Ocean bed you will see many transform faults to E and W of the Mid-Atlantic Ridge
The Mid-Ocean Ridge is a divergent boundary where tectonic plates are moving away from each other, creating new oceanic crust. Magma rises to the surface, solidifies, and forms new crust, leading to the continuous spreading of the seafloor. This process results in volcanic activity, earthquakes, and the formation of hydrothermal vents along the ridge.
Plates at boundaries can move apart (divergent boundary), collide (convergent boundary), or slide past each other horizontally (transform boundary). These movements can result in the formation of new crust, subduction of plates, or earthquakes along fault lines.
Plate boundaries, essentially, are the areas where two lithospheric plates meet. When this happens, one of three things can happen. Plates can move apart from each other, creating divergent boundaries. Plates can collide together, created convergent boundaries. Or plates can rub against each other in a parallel motion, created transform fault boundaries. Divergent boundaries, usually between two oceanic plates, creates an upswelling of magma from the lithosphere. Convergent boundaries, usually between oceanic and continental plates, causes the oceanic plate to subduct underneath the continental plate, leading to the destruction of seafloor. Transform fault boundaries neither destroy nor create lithosphere.
Yes and No. Earth's plates push toward each other to form multiple regions known as convergent plate boundaries. At these boundaries there is a variety of lands formations such as mountains, trenches, earthquakes, etc.. A convergent plate boundary occurs because two tectonic plates collide with one another creating one of two zones, a subduction zone or a collision zone. A Subduction zone occurs when when two plates collide and the plate with the greater of the two densities is forced below the other, this creates earthquakes and trenches. A collision cone is when two plates of equal density collide and as a result both are pushed up, this creates mountains. On the other hand if one plate is moving toward another that means it is also moving away from another. This is known as a divergent plate boundary. At a divergent plate boundary mainly just a few things happen( all under water ). Formation of volcanic islands, abyssal planes, ocean basins, etc..
Mid-ocean ridges can form as new crust is created at divergent plate boundaries. Earthquakes can occur as the plates pull away from each other. New ocean basins can develop as the plates move apart.
Divergent Plate Boundary: The area where two plates are moving in relatively opposite directions and new crustal material is being created by rising decompressed mantle rock. Examples would be the mid-ocean ridges, and the East African Rift. Convergent Plate Boundary: The area where two tectonic plates are moving toward each other and one of two things happens; either the more dense plate subducts under the lighter plate and heads toward the mantle, or, if the plates are of similar density, they cause uplift and mountain forming events. Examples would be the oceanic to continental crustal collision creating the Andes Mountains, and the continental to continental crustal collision creating the Himalayan Mountains. Transform Plate Boundary: The area where two plates are grinding past each other, snapping into place from elastic rebound as they go, causing numerous earthquakes. The San Andreas Fault is an example of a transform plate boundary between the North American and Pacific plates.
Both involve tectonic plate moving relative to one another and help recycle oceanic crust. At divergent boundaries plates move away from each other and new crust is created. At most convergent boundaries oceanic crust is destroyed.Both of these boundary types produce volcanoes.
Divergent Plate Boundary: The area where two plates are moving in relatively opposite directions and new crustal material is being created. Examples would be the mid-ocean ridges and the East African Rift.Convergent Plate Boundary: The area where two tectonic plates are moving toward each other and one of two things happens; either the more dense plate subducts under the lighter plate and heads toward the mantle, or, if the plates are of similar density, they cause uplift and mountain forming events. Examples would be the oceanic to continental crustal collision creating the Andes Mountains, and the continental to continental crustal collision creating the Himalayan Mountains.Transform Plate Boundary: The area where two plates are grinding past each other, snapping into place from elastic rebound as they go, causing numerous earthquakes. The San Andreas Fault is an example of a transform plate boundary between the North American and Pacific plates.
Tectonic plates move both horizontally and vertically. Most tectonic plate movement occurs horizontally along plate boundaries through processes like subduction, spreading, and transform motion. However, vertical movement can also occur, such as during the formation of mountain ranges through crustal uplift or subsidence of areas due to tectonic forces.
They could meet and cause an earthquake.
If two plates crashed into each other two possible things can happen: 1 The plates bump into each other and can cause an earthquake. 2 The plates crash, then they go upwards to form a mountain or a volcano. ~Doraexplorer
they create trenches underwater, valleies and other things like the Great Rift Valley of the Marianis Thrench
The Appalachian Mountains are a divergent boundary.