A normal fault is a type of fault in which lengthening, or extension, of a portion of Earth’s crust causes a block of rock above the fault to move downward relative to the block below.

Normal, or Dip-slip, faults are inclined fractures where the blocks have mostly shifted vertically. If the rock mass above an inclined fault moves down, the fault is termed normal, whereas if the …

Jun 26, 2019 · Learn what geological faults are, how they form, and the main types of faults — normal, reverse, thrust, strike-slip, and oblique — with their causes and effects.

In a normal fault, the block above the fault moves down relative to the block below the fault. This fault motion is caused by tensional forces and results in extension.

Normal faults are geological structures that arise when the Earth's crust experiences tensional forces, leading to vertical movement of crustal blocks. In a normal fault, one block, known as …

A normal fault is a geological fault where the hanging wall has moved downward relative to the footwall due to extensional forces, typically associated with divergent plate boundaries.

Normal faults form when the hanging wall moves down relative to the footwall. Faults are the places in the crust where brittle deformation occurs as two blocks of rocks move relative to …

Mar 13, 2025 · In the realm of structural geology, a normal fault is a type of dip-slip fault, characterized by a distinct pattern of movement. This geological feature occurs when the …

Normal and reverse faults display vertical, also known as dip-slip, motion. Dip-slip motion consists of relative up-and-down movement along a dipping fault between two blocks, the hanging wall …

What is a normal fault? Learn the normal fault definition and see normal fault examples. Also, differentiate between a normal fault and a reverse fault.