Sliding or shear forces are typically associated with a transform plate boundary. A transform plate boundary, also known as a conservative plate boundary, occurs when two tectonic plates slide past each other horizontally in opposite directions. As the plates move, they generate shear forces that result in lateral displacement along the boundary.
Transform plate boundaries are characterized by prominent fault lines, such as strike-slip faults, where the movement of the plates is predominantly horizontal. The San Andreas Fault in California, USA, is a well-known example of a transform plate boundary.
Unlike convergent boundaries (where plates collide) or divergent boundaries (where plates move apart), transform boundaries primarily accommodate horizontal displacement and exhibit intense shear stress. These boundaries do not typically involve significant volcanic or mountain-building activities but are primarily responsible for earthquakes caused by the release of accumulated stress along the fault lines.
In a convergent boundary
What you call a pull apart rift zone is what is called a divergent boundary. Most divergent zones are located under water and are a zone where new oceanic crust is born. One location where a divergent zone can be seen on land can be found in Iceland.
Earthquakes associated with convergent plate boundaries typically occur in the subduction zones where one tectonic plate is forced beneath another. These earthquakes are known as megathrust earthquakes and can have very high magnitudes due to the intense tectonic forces involved in the subduction process.
FRICTION
An anticline typically forms at convergent plate boundaries where compression forces cause the Earth's crust to fold upwards. This type of folding is common in areas where two tectonic plates collide and the crust is pushed together.
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.
In a convergent boundary
What you call a pull apart rift zone is what is called a divergent boundary. Most divergent zones are located under water and are a zone where new oceanic crust is born. One location where a divergent zone can be seen on land can be found in Iceland.
High folded mountains where two plates are pushing toward each other
The 1994 Northridge earthquake occurred due to the movement along the Northridge blind thrust fault, which is a reverse fault associated with the Pacific Plate sliding northwest relative to the North American Plate. This earthquake was a result of the tectonic forces between these two plates.
Earthquakes associated with convergent plate boundaries typically occur in the subduction zones where one tectonic plate is forced beneath another. These earthquakes are known as megathrust earthquakes and can have very high magnitudes due to the intense tectonic forces involved in the subduction process.
Sliding Friction
FRICTION
Sliding Static Fluid Rolling
Static friction is stronger than sliding friction because it prevents an object from starting to move, while sliding friction resists the motion of an object in contact with another surface. Rolling friction is typically the weakest of the three, as it only occurs when an object is already in motion, and the friction forces are reduced due to rolling instead of sliding.
The force that prevents two forces in contact from sliding past each other is friction. Friction has the ability to keep things from moving.
Sliding friction requires more force to overcome its friction.