page_title: Fault (geology)
hierarchical_section_title: Fault (geology)
caption_attribution_description: English: The Blue Anchor Fault Possibly the most obvious fault in Britain. The red rock with reduction horizons is Triassic Mercia Mudstone (MMS). To the left there are younger rocks, Late to Latest Triassic (Norian-Rhaetian) and/or Earliest Jurassic interbedded marls and muds (with evaporites like gypsum). You can tell this is a normal fault, this means the younger strata has slid downwards to sit beside the MMS. Also near the fault in the MMS the lighter reduction horizons are dipping downwards probably due to marginal drag. The line of the fault runs along the beach, shown by the rock/sand divide.
context_page_description: A fault is a fracture, or break, in the Earth's crust. Some faults are active. Here, sections of rock move past each other. This sometimes makes earthquakes.
  Faulting occurs when shear stress on a rock overcomes the forces which hold it together. The fracture itself is called a fault plane. When it is exposed at the Earth's surface, it may form a cliff or steep slope called a fault scarp.
  The angle between the fault plane and an imaginary horizontal plane is called the dip angle of the fault. Faults may dip shallowly or steeply.
  Faults are categorized into three types:
  A normal fault is one where the fault dips toward the downthrown block. Normal faults occur in rifted terranes, such as Mid-Ocean Ridges, the African Rift, and the Basin and Range Province of western North America. It is shown on geologic maps as a black line with either a block pattern on the downthrown side, or the letters U/D showing the upthrown and downthrown sides.
  A reverse fault or thrust fault is a fault where the fault plane dips toward the upthrown block. It is shown on the geologic map with triangular teeth pointing toward the upthrown side of the fault.
context_section_description: A fault is a fracture, or break, in the Earth's crust (lithosphere). Some faults are active. Here, sections of rock move past each other. This sometimes makes earthquakes.
  Faulting occurs when shear stress on a rock overcomes the forces which hold it together. The fracture itself is called a fault plane. When it is exposed at the Earth's surface, it may form a cliff or steep slope called a fault scarp.
  The angle between the fault plane and an imaginary horizontal plane is called the dip angle of the fault. Faults may dip shallowly or steeply.
  Faults are categorized into three types:
  A normal fault is one where the fault dips toward the downthrown block. Normal faults occur in rifted terranes, such as Mid-Ocean Ridges, the African Rift, and the Basin and Range Province of western North America. It is shown on geologic maps as a black line with either a block pattern on the downthrown side, or the letters U/D showing the upthrown and downthrown sides.
  A reverse fault (if steeply dipping) or thrust fault (if shallowly dipping) is a fault where the fault plane dips toward the upthrown block. It is shown on the geologic map with triangular teeth pointing toward the upthrown side of the fault. Reverse and thrust faults shorten (horizontally) and thicken the crust. They are characteristic of collision origins.
  A transform (oceanic) or strike-slip (continental) fault is one where the relative motion is horizontal. The fault plane is usually vertical and can be horizontal. Famous examples of these include the San Andreas Fault of California, the Alpine Fault of New Zealand's south island, and the Anatolian Fault in Turkey.
caption: Normal fault on the coast of Somerset, England. On left, younger blue-grey rock is late Triassic to early Jurassic. On right, the red rock is older Triassic mudstone. Strata of the red rock deformed when it moved upwards. The line of the fault runs along the beach, shown by the rock/sand divide.
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