a sliding boundry is where earthquakes occur. if you picture two squares with a crack in between them, imagine that one slides forward and the other slides back... that's a sliding boundry.
No, this statement is not accurate. Along a sliding boundary, called a transform boundary, the crust is neither created nor destroyed. Instead, the crust is transformed horizontally as two tectonic plates slide past each other.
The North America and Caribbean plates meet at a transform plate boundary. This type of boundary is characterized by plates sliding past each other horizontally, causing earthquakes along the boundary.
At a transform boundary, plates slide past each other horizontally in opposite directions. This movement is called lateral sliding. It can create earthquakes as the plates become stuck and then suddenly release along the boundary.
I think you're referring to tectonic plates, there are 3 ways one is convergent boundary, divergent, and transform. Plates that slide against each other are called transform boundary's. And your welcome
A transform plate boundary does not involve subduction zones. This boundary is characterized by plates sliding past each other horizontally without any crust being destroyed or created. The San Andreas Fault in California is an example of a transform plate boundary.
transform
A sliding boundary is a type of boundary condition in physics and engineering where the boundary is able to move or slide in response to external forces. This allows for deformation or movement of the boundary without causing discontinuities in the system being studied. Sliding boundaries are often used in simulations to model realistic physical scenarios.
Transform boundary is when the plates are sliding past each other: ↑ ↓; Divergent is when plates are sliding away from each other: ← →; and convergent is when plates are sliding towards each other: → ←. Those are the three main plate boundaries.
A transform plate boundary involves two plates sliding alongside one another horizontally. This movement can cause earthquakes and create features like strike-slip faults. An example of this boundary is the San Andreas Fault in California.
A transverse boundary is when two plates collide, causing great amounts of pressure. The plates crumble, and usually get destroyed. This is a very destructive type of boundary. This is also know as a transform boundary, or a sliding boundary- even though this action is the opposite of sliding.
forms when two {crustal} lithosphere plates move apart.
Green
The movement of the plates can be compared to... Transform boundary- sliding past one another convergent boundary- moving together divergent boundary- pulling apart
its true
the sliding boundary goes up and shoots magma out
No, this statement is not accurate. Along a sliding boundary, called a transform boundary, the crust is neither created nor destroyed. Instead, the crust is transformed horizontally as two tectonic plates slide past each other.
A transform plate boundary has plates sliding past each other horizontally. This movement can result in earthquakes due to friction and pressure build-up along the boundary.