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A rockfall or rock-fall [1] is a quantity of rock that has fallen freely from a cliff face. The term is also used for collapse of rock from roof or walls of mine or quarry workings. The term is also used for collapse of rock from roof or walls of mine or quarry workings.
Talus cones produced by mass moving, north shore of Isfjord, Svalbard, Norway Mass wasting at Palo Duro Canyon, West Texas (2002) A rockfall in Grand Canyon National Park. Mass wasting, also known as mass movement, [1] is a general term for the movement of rock or soil down slopes under the force of gravity.
Rockslide at Oddicombe Beach in Devon, UK Rockslides in Nigeria Landslips. A rockslide is a type of landslide caused by rock failure in which part of the bedding plane of failure passes through compacted rock and material collapses en masse and not in individual blocks.
A: Diagram illustrating the resistance to, and causes of, movement in a slope system consisting of an unstable block B: Diagram illustrating the resistance to, and causes of, movement in a slope system consisting of an unstable block. In some situations, the presence of high levels of fluid may destabilise the slope through other mechanisms ...
La Conchita is a small community located on the southern California coastline between Ventura and Santa Barbara. [2] It lies on a narrow strip of land about 250 meters (820 feet) wide between the shoreline and abutting a 180-meter (590 ft) high bluff. [2]
Scree is formed by rockfall, [3] [6] which distinguishes it from colluvium. Colluvium is rock fragments or soil deposited by rainwash, sheetwash, or slow downhill creep, usually at the base of gentle slopes or hillsides. [7] However, the terms scree, talus, [2] [3] and sometimes colluvium [8] tend to be used interchangeably.
Diagram of horsts and grabens In geology , horst and graben (or range and valley ) refers to topography consisting of alternating raised and lowered fault blocks known as horsts and grabens . The features are created by normal faulting and rifting caused by crustal extension . [ 1 ]
Cross-section diagram of a thrust fault with a fault-bend fold. A thrust fault has the same sense of motion as a reverse fault, but with the dip of the fault plane at less than 45°. [22] [23] Thrust faults typically form ramps, flats and fault-bend (hanging wall and footwall) folds.