Transform
transform
No, a strike-slip fault forms at a transform boundary where two plates slide past each other horizontally. A convergent boundary is where two plates move towards each other, leading to subduction or collision.
No, when two continental plates diverge, a divergent boundary forms, not a transform boundary. At a divergent boundary, the plates move away from each other, leading to the formation of rift valleys or mid-ocean ridges. Transform boundaries occur where two plates slide past each other horizontally.
False. A strike-slip fault forms at a transform boundary where two tectonic plates slide past each other horizontally. A convergent boundary is formed when two plates collide and one plate is forced beneath the other in a subduction zone.
Divergent Boundary.
A transform plate boundary forms where two plates slide past one another horizontally. This movement can cause earthquakes due to the friction and pressure buildup along the boundary. An example of this type of boundary is the San Andreas Fault in California.
A transform boundary occurs when tectonic plates slide past each other horizontally, causing earthquakes. On the other hand, a convergent boundary forms when two tectonic plates collide, leading to the formation of mountains, trenches, and volcanic activity.
A transformational plate boundary forms earthquakes.
A transform boundary forms where plates slide past each other horizontally. Most transform boundaries are found near Mid-ocean ridges.
The boundary between the Pacific Plate and the North American Plate is a transform boundary. At this boundary, the plates slide past each other horizontally, causing frequent earthquakes along the boundary. This boundary is known as the San Andreas Fault.
no
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.