(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.
Movement on faults can be a combination of dip-slip and strike-slip. Pure dip-slip faults can be normal (h/wall down) or reverse (h/wall up). Pure strike-slip faults can be dextral (right-lateral) or sinistral (left-lateral). Oblique-slip faults combine dip-slip and strike-slip components.Net slip = displacement on a fault, measured in the plane of the fault.) Classification. Fault rocks are classified according to the size of the fragments, and whether they are cohesive or not. If cemented by minerals precipitated from circulating groundwater it is an indurated gouge. Cataclasite: Cohesive fault rocks composed of broken, crushed and rolled grains.