Convergent boundaries.
A convergent boundary causes compressional stress.
In a reverse fault the maximum principal stress is horizontal, compression causes reverse (thrust) faults.
All three type of Earthquakes (Shallow-seated, Medium-seated and Deep-seated) occur only at the Convergent plate boundary. At divergent plate boundary we find mostly Shallow-seated Earthquakes only.
The type of stress force that produces a strike-slip fault is transform stress. This stress occurs when two tectonic plates slide past each other horizontally, causing displacement along a fault line. Strike-slip faults are often associated with transform plate boundaries, such as the San Andreas Fault in California.
A transform boundary is a type of plate boundary where two tectonic plates slide past each other horizontally. The friction between the plates can build up over time, causing stress to accumulate. When this stress is released suddenly, it can result in an earthquake along the transform boundary.
A convergent boundary causes compressional stress.
Transform Boundary
compression
In a reverse fault the maximum principal stress is horizontal, compression causes reverse (thrust) faults.
The type of stress developed at a convergent boundary is Compressional Stress.
it is compression
compression
Shear stress: At a transform boundary, two plates are moving past each other, either in opposite directions or both in the same direction but at differing speeds. As the boundary between the two plates is not perfectly smooth there will be some interlocking along the boundary. As the plates continue to move and this interlocking resists movement, shear stresses develop.
compression
Compressive or compression
Compression.
Compression.