Fault (geology)#Dip-slip faults
In a deportation is a rejection, in which the layers in the hanging wall are shifted down. This happens most often with an incidence angle of 30-60 ° from the perpendicular, but there are also flatter deportations known ( Detachment ). Deportations are form typical of strain areas where the surface most grave structures (see grave breach ).
Through deportation can off-road a desk plaice arise.