Transform boundaries can create or destroy tectonic plates through lateral movement. At these boundaries, plates slide past each other, which can lead to earthquakes as stress builds up and is released. In contrast, divergent boundaries create new plates as tectonic plates move apart, allowing magma to rise and solidify, while convergent boundaries can destroy plates as one plate is forced beneath another in a process known as subduction.
A divergent boundary forms when tectonic plates pull apart. As the plates move away from each other, magma rises up to create new crust, resulting in features like mid-ocean ridges or rift valleys on land.
When two tectonic plates separate, a divergent boundary is formed. At this boundary, magma rises from the mantle to create new crust, often resulting in the formation of mid-ocean ridges or rift valleys. This process can lead to volcanic activity and earthquakes as the plates move apart. An example of a divergent boundary is the Mid-Atlantic Ridge.
A plate boundary in the ocean where tectonic plates move apart is called a divergent boundary. At these boundaries, magma rises from the mantle to create new crust as the plates separate. An example of a divergent boundary is the Mid-Atlantic Ridge.
tectonic plates. just because they are convergent doesnt change the fact that they are tectonic..
A transform boundary does not destroy or create crust. Instead, it occurs where two tectonic plates slide past each other horizontally. This lateral movement can lead to earthquakes but does not involve the formation of new material or the destruction of existing crust. Examples include the San Andreas Fault in California.
A transform boundary is a type of plate boundary where tectonic plates slide past each other horizontally. Before the formation of a transform boundary, the movement of tectonic plates may have been different, such as moving towards each other at a convergent boundary or moving apart at a divergent boundary. After the formation of a transform boundary, the movement of tectonic plates changes to sliding past each other horizontally, which can cause earthquakes and create new geological features.
A divergent boundary forms when tectonic plates pull apart. As the plates move away from each other, magma rises up to create new crust, resulting in features like mid-ocean ridges or rift valleys on land.
A convergent boundary is where plates move together.
no
When two tectonic plates slide past each other, it is called transform boundary. This movement can create earthquakes along the boundary where the plates are in contact.
A transform plate boundary does not create or destroy crust. Instead, adjacent plates slide horizontally past each other. This movement can cause earthquakes along the boundary without significantly changing the amount of crust.
When two tectonic plates separate, a divergent boundary is formed. At this boundary, magma rises from the mantle to create new crust, often resulting in the formation of mid-ocean ridges or rift valleys. This process can lead to volcanic activity and earthquakes as the plates move apart. An example of a divergent boundary is the Mid-Atlantic Ridge.
A plate boundary in the ocean where tectonic plates move apart is called a divergent boundary. At these boundaries, magma rises from the mantle to create new crust as the plates separate. An example of a divergent boundary is the Mid-Atlantic Ridge.
Any area where two or more tectonic plates do not touch each other is a not a tectonic plate boundary.
the tectonic plates move and the lava rises
a divergent boundary
plate boundary