Overview: Can you always tell the difference between anticlines and synclines, themselves. You can often tell whether you‘re dealing with joints and faults, unconformities and disconformities, concretions sedimentary, igneous or metamorphic rocks, and that‘s usually all and conglomerates, bedding and cleavage, strike and dip, you need in order to recognise structures and sort out their apparent dip and true dip? If your answer to all that is a firm yes, orientation. Details in the rocks themselves may enable you to then stop reading right now. If not . . . distinguish, say, a limestone from a
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