Folds and Faults - ROCKS CAN BEND OR BREAK
Mountains are regions of disturbed or deformed rocks. They are differentiated into three types according to the nature of the deformation which created them:

   1. dome mountains result from the upward bending of rocks into the form of a dome. The Black Hills of South Dakota are a typical example of a naturally dissected dome mountain.

   2. fold mountains consist of a series of long, more or less parallel wrinkles, or folds. The mountains of West Virginia and central Pennsylvania are good examples of fold mountains in the mature stage of erosion. This type of lateral compressional folding, whether it occurs in mountain building or on a much more localized scale in the subsurface, creates structures which may contain hydrocarbons. These are anticlines, synclines, and monoclines.

   3. block mountains are formed by faulting and uplifting of angular blocks of rock. Some of the blocks are pushed and tilted at various angles into block mountains. The depressed blocks between the uplifted ones are block basins.

Anticlines are the raised peaks of folds (the tops of the hills) and may be evident at the surface, although deeply buried anticlines may be covered by flat lying sediments. Synclines are the valleys between folds. A monocline is a long, relatively flat, sloping surface usually with a more or less flat plain at the bottom end and a flat plateau at the top end.

Formation dip is the angle relative to horizontal at which the top surface of a formation rests. The dip direction, or dip azimuth, is the direction relative to north at which the formation dips downward. Strike is the direction of a line along the surface at right angles to the dip direction.

Definitions of folds

A fold is made of:
   1. an axial plane or an axial surface of folding
   2. two flanks, or limbs
   3. a zone of flexure
   4. an axis where the axial plane crosses the rock layers

A fold is described according to:
   1. the orientation of the axial surface with respect to vertical:
       - symmetrical when the axial plane is vertical
       - asymmetrical when the axial surface is oblique
      - overturned when the axial surface is oblique, and one flank has been overturned; i.e., dips in the same direction as the other flank
      - recumbent when the axial surface is horizontal or nearly so, one flank is overturned

   2. the dip of both flanks with regard to the axial plane;
      - anticline when the flanks dip downward away from the axial plane
      - syncline when the flanks dip downward toward the axial plane

   3. the direction of the angle of folding:
      - convex when the angle of folding points upward (upfold, anticline)
      - concave when the angle of folding points downward (downfold, syncline)

   4. the angle of folding:
      - open when the angle of folding is greater than 90 degrees
      - closed when the angle of folding is less than 90 degrees

A dome is a fold where the beds dip in all directions away from the point of folding. The axial plane may be a warped surface.

The same type of forces that act on a major scale to build mountains act in a smaller localized way to create faults. The gravity, or normal, fault is caused by tensional forces. Removal of compression allows one block of the earth to move downward with respect to another.

Definitions of faults

When compressional forces are exerted, a reverse or thrust fault results. In a thrust fault, pressure forces cause the hanging wall (the rock above the fault plane) to move upward and over the top of the foot wall (the rock below the fault plane). Reverse faults are similar except that there is no motion of the upper block along the top of the lower block.

Movement of either wall in a direction parallel with the fault plane is called a rift or tear or shear fault.

In some instances a long and narrow block drops down between two or more faults, and is called a graben. Blocks that remain raised between two faults are called horsts. The faults bounding both grabens and horsts are gravity (or normal) faults.

A fault is a fracture with relative movement of the two blocks of rock on either side of the fracture. It is made of:
   1. the fracture proper
   2. fault plane(s) or fault zone
   3. the upper block above the fault plane, called the hanging wall
   4. the lower block below the fault plane, called the foot wall
   5. a zone of distortion, which may occur on both or either side of the fault plane, usually called rollover, drag, or gouge

A fault can be described:
   1. according to the relative movements of both blocks with respect to vertical
      - normal when the upper block is downthrown (gravity fault)
      - reverse when the upper block is upthrown

   2. according to the relative movement of both blocks with respect to the dip of the fault plane
      - strike-slip when the movement occurs laterally along the strike of the fault plane (horizontal throw)
      - dip-slip when the movement occurs down the dip of the fault plane (vertical throw)
      - oblique-slip when the movement occurs along both the strike and dip of the fault plane
      - rotational when the movement occurs around an axis with rotation on only one block
      - pivotal when both blocks rotate in opposite directions around a common axis

   3. according to the magnitude of dip of the fault plane
      - high angle when the fault plane dips more than 45 degrees
      - low angle when the fault plane dips less than 45 degrees
      - vertical when the fault plane is vertical

   4. according to the time of occurrence with respect to deposition
      - post-depositional when the fault occurs long after deposition
      - contemporaneous when the fault grows at the same time as deposition, also called growth faults

Other descriptive terms used are:
   1. separation: the distance from one bed boundary in one block to its counterpart in the other.

   2. throw: the vertical component of separation; i.e., separation measured in a vertical plane normal to the fault plane. The term 45-foot fault means that 45 feet of vertical section are missing at the well bore (if a normal fault) or 45 feet of section is repeated (if a reverse fault).

   3. slip: the movement along the fault, being the distance between two formerly adjacent points. Slip can be in any direction within the fault plane; same as separation if there is no horizontal component of movement.

   4. extent: a fault is limited in horizontal and vertical extent by sudden disappearance against another fault, or against an unconformity, or by gradual decrease of throw along the fault plane. In rotational faults, throw decreases in the direction of the plane of rotation.

   5. correlation gaps or repeats: when a well crosses a normal fault, correlation of the well logs will show a missing section. When a well crosses a reverse fault, the same formation is crossed twice, and appears as a repeat section on the log. A reversed repeat can occur when drilling through a recumbent fold.

   6. drag and rollover: are fold-like deformations of the bedding planes in the vicinity of a fault and associated with the fault. Such folding is called drag when it is caused by friction of the two blocks against each other along the fault. The result is:
      - concave folding on the downthrown block.
      - convex folding on the upthrown block.

Drag on faults

In certain regions, normal faulting occurs with reverse drag, or rollover in the downthrown block. In this configuration, the bedding planes dip into the fault plane instead of away from it. Rollover is frequently associated with growth faults; i.e., faulting contemporaneous with deposition, with greater formation thickness on the downthrown side of the fault.

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