The University of Zambia School of Education LSE 3069: Fundamental Topics in Secondary School Compiled By K.Mundende 2020 Faulting • Fracturing or breaking of the rocks within the earths crust • Associated with either lateral or vertical earth movements • Associated with movement of the rock blocks • Rocks that fracture are usually brittle and compact, which may fracture or break whenever they are subjected to either tensional or compressional forces • Tensional or compressional forces might be as a result of tectonic movements (Movement of plates that make up Earth’s crust or causing deformation of Earth’s crust) Cont’d • Fracture on a rock that is caused by earth movements is known as a fault • Fault refers to a fracture in the crust due to stress or strain associated with rock displacement • Joint is a crack in the rock due to stress or strain but not associated with rock displacement Factors influencing development of a Fault • Nature of the force involved (Tensional or compressional) • Nature of the rocks on which the force acts (Brittle or soft) Types of Faults Normal Fault: Develops when the brittle, hard but breakable rocks are subjected to tensional forces. Cont’d • Include faults in which the inclination of the fault planes and the down throw are on the same side. • Footwall rises while the hanging wall goes down • A throw is a vertical displacement of the faulted blocks. Blocks can either be displaced upwards (up-throw) or down wards (down – throw) • Hanging wall is a steep slope on the up-throw that faces the downthrow • Floor is the plain ground on the down -throw Cont’d • Reverse Fault: Develops when brittle rocks are subjected to compressional forces. Cont’d • The inclination and the down throw are not on the same side • The foot wall subsides while the hanging wall rises above the foot wall Cont’d • Tear/Shear/Slip/Transform Fault: Develops when brittle rocks are subjected to compressional forces • Blocks slide past each other in a shear manner, like a pair of scissors Cont’d • Also called wrench fault • Vertical fracture produced when two rock blocks slide against one another Cont’d • Step Fault: Develop on brittle rocks which have been subjected to several tensional forces • Rocks may sink at different levels to form fault steps Cont’d • Three main types of fault in motion during the development of step fault are: Normal fault Reverse fault Strike slip fault Features Developed through Faulting • Fault blocks(Block Mountains) • Rift valley • Till blocks • Plateaus • Escarpments (Fault scarps) Activity • With the aid of an annotated diagram, explain the development of: (i) An over thrust Fault (ii) Monocline Fault References • Kinunda, E.J. and Msabila, T.D. (2012). The Comprehensive Approach to Ordinary Level: Geography. Dar es Salaam: Nyambari Nyangwine Publishers • Yogo, J.M. (2012). Ordinary Level Physical Geography. Dar es Salaam: Nyambari Nyangwine Publishers