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Name: d 1 Be A 45 d 2 Be dip Face 1 apparent dip Face 3 Face 2 Because the beds dip at 45 o, which is ½ of 90 o (a right angle corner of a cube). Angle A measures 60 o because of the oblique perspective, therefore the dip on Face 1 is ½ of 60 o or 30 o. Projecting Bed 1 at 30 o to the dotted corner, and then onto Face 2 gives the apparent dip solution (blue lines) by connecting the ends where the corner is cut off. The same are Geol used for Bedand 2. The apparent dip of the Fromtechniques /Rider/Lisle Struct Maps. pdf o blue lines is 30 , because the angle is measured from a horizontal Geology 310 2012 GCHERMAN 3 line (green)Rider and Structural on a vertical face (3) that is not distorted by an oblique perspective.

Name: Strike: Dip Direction: Angle of Dip: Rider Structural Geology 310 2012 GCHERMAN From /Rider/Lisle Geol Struct and Maps. pdf 4

Rider Structural Geology 310 2012 GCHERMAN Name: Answer: 5 From /Rider/Lisle Geol Struct and Maps. pdf

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