they slide against each other going side-to-side.
At a convergent boundary two plates move toward each other. At a transform boundary plates slide past each other.
That is a Strike-slip fault. This type of plate boundary is a relatively conservative boundary because the plates moves side by side horizontally causing little or no destruction of old plates or creation of new plates, but only causes a kind of boundary known as a Transform Boundary. An example of a transform boundary is the San Andreas fault, in California, USA North America.
a boundary at which two plates moves past each other horizontally
a boundary at which two plates moves past each other horizontally
At a transform boundary, plates slide past each other horizontally in opposite directions. This movement can cause earthquakes along the boundary.
The boundary where two plates slide against each other is called a transform plate boundary. At this boundary, the plates are sliding past each other horizontally. Transform boundaries are characterized by frequent earthquakes due to the intense friction between the plates.
At a transform plate boundary, the motion is horizontal and parallel to the boundary. The plates slide past each other in opposite directions, causing earthquakes due to the friction between the plates. This type of boundary is also known as a strike-slip boundary.
At a transform boundary, tectonic plates slide past each other horizontally in opposite directions. This movement can cause earthquakes along the boundary.
Transform boundary
A transform fault boundary is a type of tectonic plate boundary characterized by horizontal sliding of plates past each other. This movement can cause earthquakes as the plates grind against each other. An example of a transform fault boundary is the San Andreas Fault in California.
At transform boundaries, the plates move horizontal in relation to each other.
traverse fault