a transform boundary
Where 2 plates slide past each other in a horizontal motion that boundary is called a Transform Boundary, or a fault.
When plates slide past each other, it is called a transform boundary or a strike-slip boundary. This type of boundary is characterized by horizontal movement along fault lines, such as the San Andreas Fault in California.
A transform plate boundary is where two plates slide past each other horizontally, causing lateral movement. This interaction can lead to earthquakes due to the friction between the plates as they grind against each other. An example of this type of boundary is the San Andreas Fault in California.
A transform boundary. This is where tectonic plates slide horizontally past each other in opposite directions. This movement can cause earthquakes along the boundary.
Transform fault boundaries happen at the site where two tectonic plates move past each other in opposite directions. The two plates will grind past each other, breaking off pieces of crust from the plates. The plates can get caught on each other and pressure will build up until a break develops and the plates will lurch forward.
fault lines
Where 2 plates slide past each other in a horizontal motion that boundary is called a Transform Boundary, or a fault.
It is a transform boundary.
slip fault?
The fault between two plates moving sideways past each other is called a transform fault. This type of fault occurs at transform boundaries where tectonic plates slide horizontally past each other.
Transform fault/boundary. Its when two plates slide past each other.
When plates slide past each other, it is called a transform boundary or a strike-slip boundary. This type of boundary is characterized by horizontal movement along fault lines, such as the San Andreas Fault in California.
The transform boundary, where two plates slide past each other.
When plates slide past each other, it is known as a transform boundary. This movement causes earthquakes along the fault line between the two plates. Friction between the plates can build up over time, eventually releasing in a sudden movement that shakes the Earth's surface.
A transform plate boundary is where two plates slide past each other horizontally, causing lateral movement. This interaction can lead to earthquakes due to the friction between the plates as they grind against each other. An example of this type of boundary is the San Andreas Fault in California.
When two plates slide past each other, this is called a transform fault. Earthquakes can occur when the plates scrape by. If the earthquake happens underwater, a tsunami may occur. (Like in Japan)
Tectonic plates slide past each other at transform plate boundaries. This movement can result in earthquakes as the plates grind against each other. Examples of transform plate boundaries include the San Andreas Fault in California and the Alpine Fault in New Zealand.