In A Fault The Hanging Wall Moves Down Relative To The Footwall

Along a normal fault the hanging wall moves down relative to the footwall.

In a fault the hanging wall moves down relative to the footwall.

Fill in the blank 1. If the hanging wall rises relative to the footwall you have a reverse fault. Are exactly the opposite of normal faults. The crust experiences extension.

Normal fractures in rock with no offset where there has been no motion are called. What is a reverse fault. Normal faults are common. Reverse faults indicate compressive shortening of the crust.

The hanging wall moves down relative to the footwall. Other articles where normal fault is discussed. After the occurrence of a normal dip slip fault in flat lying sedimentary rocks the fault scarp produced is eliminated by erosion. Describe three types of faults.

The footwall moves down relative to the hanging wall. Choose one or more. Jack0m digitalvision vectors getty images strike slip faults have walls that move sideways not up or down that is the slip occurs along the strike not up or down the dip. Normal dip slip faults are produced by vertical compression as earth s crust lengthens.

A reverse fault is the opposite of a normal fault the hanging wall moves up relative to the footwall. In thrust or reverse faults the hanging wall moves up relative to the footwall and in strike slip faults it moves horizontally relative to the footwall. Which fault will see the hanging wall move down relative to the footwall. What is the age of the rocks on the surface of the footwall side of the fault relative to those on the hanging wall.

Tension is stress that pulls rocks apart. In these faults the fault plane is usually vertical so there is no hanging wall or footwall. The terminology of normal and reverse comes from coal mining in england where normal faults are the most common. When the hanging wall moves up in relative to the footwall it is called a fault.

The dip of a reverse fault is relatively steep greater than 45. These usually occur when tectonic forces cause tension that pulls rocks apart. The hanging wall slides down relative to the footwall. Which of the following happens at a normal fault.

A n fault forms when the hanging wall moves down relative to the footwall a. Normal faults usually form where tectonic plate motions cause tension. Reverse faults occur in areas undergoing compression squishing. This is true of normal faults.

The motion of the crustal blocks is referred to as strike slip. The hanging wall moves down relative to the footwall. The hanging wall moves up relative to the footwall.