When these landforms lie parallel to one another, they create raised and lowered areas called horsts and grabens.
When these landforms lie parallel to one another, they create raised and lowered areas called horsts and grabens. Flat irons form from scarps, which are located along these features. These features divide a surface into a hanging wall and a footwall. At lower depths, they are called shear zones. If the movement of one of these features has both strike and dip components, it is known as an oblique-slip one. They also come in transform and strike-slip types. For 10 points, name these cracks in the Earth's surface, the movement of which causes earthquakes.
When these landforms lie parallel to one another, they create raised and lowered areas called horsts and grabens.
{faults}