(From Tempur-Pedic's Website) Tempur-Pedic mattresses have been designed to be paired with a Tempur-Pedic foundation. However, we understand that some consumers wish to use their existing platform style bed with slats (as opposed to a flat surface) with our mattress.
The type of motion along a fault depends on the type of fault. The main types of faults are described below. 1  Normal dip-slip fault. 2  Normal faults happen in areas where the rocks are pulling apart (tensile forces) so that the rocky crust of an area is able to take up more space. 3  The rock on one side of the fault is moved down relative to the rock on the other side of the fault.
Starting at the Earth's surface, the following rock types are usually encountered in a shear zone: uncohesive fault rocks. Examples being fault gouge, fault breccia, and foliated gouge. cohesive fault rocks like crush breccias and cataclasites (protocataclasite, cataclasite, and ultracataclasite). glassy pseudotachylites.