The strike and dip geology define the position of the structure with respect to a horizontal plane and both together provide a more accurate structural description rather than only strike geology. Strike and dip are two references that are important for defining the attitude of any geologic feature. Strike geology is also used in maps to depict the orientation of a particular feature. Thus, strike definition geology or strike geology helps in understanding the attitude or the position of the linear structural characteristics of the above mentioned geologic features. The line of a bed (for example bedding of sedimentary rocks), fault (for example oblique-slip fault), or other planar feature that intersects with a horizontal plane is known as a strike line and the entire concept is known as a strike. Strike in geology is a reference to the attitude of a geologic feature such as a fault, bed or any other planar feature.
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