2. The bending of rock strata of
plastic nature due to
compressional forces acting
horizontally towards a common
point or plane from opposite
directions is known as folding.
INTRODUCTION
3. It results in the crumbling of
strata , resulting in a wavy
formation on the surface of the
earth , which are known as
folds.
Folds are described by their
form & orientation.
CONTINUE...
4.
5. The stretch of the rock beds lying
between any crest and any of the
adjacent troughs on either sides is
known as the limb of the fold.
The limb may be then redefined as the
fold segment between a hinge line and
the adjacent inflection line.
1.LIMBS
6.
7. A point can be found where curvature is
maximum is called hinge point.
When rocks occur in a sequence & their
all hinge points are joined together ,
they make a line , called the hinge line.
2.HINGE
8.
9. An axial plane is that imaginary plane
that passes through all the points of
maximum curvature in a folded
sequence.
It may be vertical , inclined or
horizontal in nature.
3.AXIAL PLANE
10.
11. A line drawn parallel to the hinge line of
a fold.
A precise definition is the line
representing the intersection of the
axial plane of a fold with any bed of the
fold.
4.AXIS OF A FOLD
12.
13. The angle of inclination of the fold axis
with the horizontal as measured in a
vertical plane is termed the plunge of
the fold.
In other words , plunge is the angle
which this line makes with a horizontal
plane.
5.PLUNGE OF A FOLD
14.
15. Crest-Highest points in an uparched
fold.
Trough-Lowest point in a downarched
fold.
Inflection point-A point on a fold at
which the fold changes from syncline
to anticline or vice versa.
6.CREST,TROUGH & INFLECTION
POINT
16.
17. Engineering & general geology-Parbin
Singh.
A textbook of geology-G.B.Mahabatra
https://en.wikipedia.org/wiki/File:Flank_
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on.JPG
REFERNCE