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Strike and dip are generally written as 'strike/dip' or 'dip direction,dip', with the degree symbol typically omitted. The general alphabetical dip direction (N, SE, etc) can be added to reduce ambiguity. For a feature with a dip of 45° and a dip direction of 75°, the strike and dip can be written as 345/45 NE, 165/45 NE, or 075,45.
Strike and dip symbols consist of a long "strike" line, which is perpendicular to the direction of greatest slope along the surface of the bed, and a shorter "dip" line on side of the strike line where the bed is going downwards. The angle that the bed makes with the horizontal, along the dip direction, is written next to the dip line.
Includes strike and dip, vertical strata, horizontal strata, anticline axis, syncline axis, plunging anticline axis, plunging syncline axis, and strike-slip fault. For more details and symbols, see the FGDC Digital Cartographic Standard for Geologic Map Symbolization at the official website
Rake is used to describe the direction of fault motion with respect to the strike (measured anticlockwise from the horizontal, up is positive; values between −180° and 180°): left-lateral strike slip: rake near 0° right-lateral strike slip: rake near 180° normal: rake near −90° reverse/thrust: rake near +90°
Reason: The dip angle is designated here as the angle between the dipe line of the „real“ (i.e. the red/pink) plane and the East direction. Since the real plane does not strike in N-S direction, there has to be a dip direction line within the horizontal plane which is oriented 90° to the strike line and not identical to the East direction.
its orientation in space, as strike and dip, or dip and dip direction; its relationship to other foliations, to bedding and any folding; measure intersection lineations;
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Likewise, the orientation of a plane can be described with two values as well, for instance by specifying the orientation of a line normal to that plane, or by using the strike and dip angles. Further details about the mathematical methods to represent the orientation of rigid bodies and planes in three dimensions are given in the following ...