FOLDS ND FOLDING
Folds.ppt
 FOLD:- it may be defined as UNDULATIONS OR BENDS OR
CURVATURES developed in a rocks because of STRESSES
witch are acting on rocks from time to time in past history of the
earth.
 The shape and extent of a folds depends upon a no. of factors;-
- nature - magnitude
- direction and duration of forces act upon the rocks
- and on nature of the rocks.
PARTS OF FOLDS LIMBS :- these are the sides or flanks of the folds.
 HINGE :- in folded layer a point at curvature is maximum is called
hinge point.
 HINGE LINE :- rocks occur in a sequence and their all hinge
points are joined together, they make a line called hinge line.
 AXIAL PLAIN :- an axial plane is that imaginary plane that
passes through all the points of maximum curvature in a folded
sequence
 PLUNGE OF FOLD :- plunge is angle which axis line makes with
a horizontal plane.
PARTS OF FOLDS
 CREST AND TROUGH :- the line running through the highest
points in an up arched fold defines as CREST.
 THE line running through the lowest point in a down arched fold
make its THROUGH.
Folds
Types of FOLDS:--
1) Anticline fold
2) syncline fold
3) Symmetrical Folds
4) Asymmetrical fold
5) overturned fold
6) Isoclinal fold
7) Recumbent Fold
1) Anticline fold:-
in this fold strata are convex upwards.
2) syncline fold:--
in this fold strata are convex downward.
3) Symmetrical fold:-
this are also called normal folds . Axial plane is
essentially vertical. The limbs are equal in length and dip equaly in in
opposite directions.
4) Asymmetrical fold:-
in this folds limbs are unequal in length and dip are of
different angle. Are termed as Asymmetrical folds.
5) Overturned fold:-
these are folds with inclined axial plains in witch both
limbs are dipping essentially in the same general direction.
6)Isoclinal folds:-
these are group of folds in witch all the axial plains are
parallel. They may b made up of series of anticlines and synclines.
7) Recumbent fold:-
this may be described as extreme types of overturned
fold in witch the axial plain acquires an almost horizontal attitude.
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     FOLD:- itmay be defined as UNDULATIONS OR BENDS OR CURVATURES developed in a rocks because of STRESSES witch are acting on rocks from time to time in past history of the earth.  The shape and extent of a folds depends upon a no. of factors;- - nature - magnitude - direction and duration of forces act upon the rocks - and on nature of the rocks.
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    PARTS OF FOLDSLIMBS :- these are the sides or flanks of the folds.  HINGE :- in folded layer a point at curvature is maximum is called hinge point.  HINGE LINE :- rocks occur in a sequence and their all hinge points are joined together, they make a line called hinge line.  AXIAL PLAIN :- an axial plane is that imaginary plane that passes through all the points of maximum curvature in a folded sequence  PLUNGE OF FOLD :- plunge is angle which axis line makes with a horizontal plane.
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    PARTS OF FOLDS CREST AND TROUGH :- the line running through the highest points in an up arched fold defines as CREST.  THE line running through the lowest point in a down arched fold make its THROUGH.
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    Types of FOLDS:-- 1)Anticline fold 2) syncline fold 3) Symmetrical Folds 4) Asymmetrical fold 5) overturned fold 6) Isoclinal fold 7) Recumbent Fold
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    1) Anticline fold:- inthis fold strata are convex upwards. 2) syncline fold:-- in this fold strata are convex downward.
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    3) Symmetrical fold:- thisare also called normal folds . Axial plane is essentially vertical. The limbs are equal in length and dip equaly in in opposite directions. 4) Asymmetrical fold:- in this folds limbs are unequal in length and dip are of different angle. Are termed as Asymmetrical folds. 5) Overturned fold:- these are folds with inclined axial plains in witch both limbs are dipping essentially in the same general direction. 6)Isoclinal folds:- these are group of folds in witch all the axial plains are parallel. They may b made up of series of anticlines and synclines.
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    7) Recumbent fold:- thismay be described as extreme types of overturned fold in witch the axial plain acquires an almost horizontal attitude.
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