The shearing rock stress is much like the transform plate boundary. Two rocks slide against each other. You can think of it like shearing a sheep (the shear slides against the sheep). Shearing can happen when rocks are pushed in different directions. Parts of the rock can break off, and even cause small earthquakes because of friction (according to sciencing.com).
Like the convergent plate boundary, the compression rock stress is two plates (in this case, rocks), pushing against each other. You can demonstrate this by pushing your hands together. Mountains are an example of what happens because of this rock stress.
Tension is like the divergent plate boundary because the rocks/plates go away from each other. It is the opposite of compression. This can form rift valleys. Some scientists think tension caused Pangaea to break apart into the seven continents.
A reverse fault is the opposite of a normal fault. The hanging wall block is above the foot wall block, because the hanging wall is thrust higher. It is also called a thrust fault and a dip-slip fault.
Earthquakes are caused when a transform plate boundary starts to shake, along a fault line. The two plates start rubbing against each other, shacking the ground, and causing buildings to collapse. Often, fires start.
Tsunamis happen when an underwater fault line (a transform boundary on an oceanic plate) is active. Just like an earthquake, the plates start to shake, causing a huge wave that ultimately can destroy entire cities. Sometimes buildings catch on fire while floating in the water, causing even more damage.