Webnoun. foot· wall ˈfu̇t-ˌwȯl. 1. : the lower underlying wall of a vein, ore deposit, or coal seam in a mine. 2. : the lower wall of an inclined fault. WebJul 20, 1998 · When rocks slip past each other in faulting, the upper or overlying block along the fault plane is called the hanging wall, or …

Classification of Faults Rocks Geology - Geography Notes

Webfootwall. [ foot-wawl ] show ipa. noun. the top of the rock stratum underlying a vein or bed of ore. a mass of rock lying beneath a fault plane. Compare More Words. WebDefinition 1 / 2 A hanging wall is one of the two sides of a non vertical fault, the other side is called a foot wall. The hanging wall is the portion above the fault plain. A hanging wall usually extends over a certain area of the surface hence its name. http://upload.wikimedia.org/wikipedia/commons/5/50/Hanging_%26_footwall.jpg ictmon

Footwall geology Britannica

WebOther articles where thrust fault is discussed: fault: Reverse dip-slip faults result from horizontal compressional forces caused by a shortening, or contraction, of Earth’s crust. The hanging wall moves up and over the footwall. Thrust faults are reverse faults that dip less than 45°. Thrust faults with a very low angle of dip… WebThe hanging-wall block of a fault is therefore always to the right, and the footwall block on the left. This is important because rake (which gives the slip direction) is defined as the movement of the hanging wall relative to … WebDec 8, 2008 · 2.3.6 Reverse and thrust faults. In a reverse or thrust fault, the hanging wall has moved up relative to the footwall. The distinction between a reverse fault and a thrust fault is that a reverse fault has a steeper dip, greater than 30 degrees. Reverse and thrust faults develop in sectors of the crust that are experiencing compression. money titles blox fruits