The Line of intersection between the axial plane and the surface of
any of the consituent rock bed is called axis of fold.
2.Axial Fold
An Imaginary Plane Which Divides the fold into two equal halves is
called axial plane.
3.Plunge of Fold
The Inclination of the fold axis with the horizontal is called the
plunge of fold.
4.Non Confirmity
The uncinformity in which the older beds formation is made up of
plutonic igneous rocks lying below the younger bed of sedimentary
rocks, is called as non confirmity
5.Disconfirmity
The unconformity in which the beds lying below and above the surface
of erosion are almost parallel is called disconformity.
6.Chevoron fold
These are characterized by very long limbs and very narrow hinges
(Figure ) and most of the naturally developed chevron folds have an
interlimb angle around 60°.