Compressional stresses occur at convergent plate boundaries.
The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.
transform boundary
a mountainous one.
transform fault boundary
Its a divergent boundary
Destructive (Plate) Boundary.Under converging convection currents in the asthenosphere, two plates converge.This is called slab pull.The denser plate sinks, then subducts into the asthenosphere and melt into magma.
transform fault boundary
The type of plate boundary where two plates grind past each other without destroying the lithosphere is called a transform boundary. At these boundaries, the plates slide laterally against one another, leading to friction and stress that can result in earthquakes. An example of a transform boundary is the San Andreas Fault in California. Unlike convergent or divergent boundaries, transform boundaries do not create or consume crust.
The boundary between the Indian-Australian Plate and the Eurasian Plate is primarily a convergent boundary. This type of boundary is characterized by the collision of the two plates, which has resulted in significant geological activity, including the uplift of the Himalayas. The intense pressure and friction at this boundary can also lead to earthquakes.
When a divergent boundary occurs beneath oceanic lithosphere, the rising convection current below lifts the lithosphere producing a mid-ocean ridge!!!Hope i helped.
Stormy weather often occurs along the boundary between air masses or in association with a low pressure system.
convergent boundary.