Types_of_Folds_and_Faults In Geology pdf

ashes200209 30 views 29 slides Aug 01, 2024
Slide 1
Slide 1 of 29
Slide 1
1
Slide 2
2
Slide 3
3
Slide 4
4
Slide 5
5
Slide 6
6
Slide 7
7
Slide 8
8
Slide 9
9
Slide 10
10
Slide 11
11
Slide 12
12
Slide 13
13
Slide 14
14
Slide 15
15
Slide 16
16
Slide 17
17
Slide 18
18
Slide 19
19
Slide 20
20
Slide 21
21
Slide 22
22
Slide 23
23
Slide 24
24
Slide 25
25
Slide 26
26
Slide 27
27
Slide 28
28
Slide 29
29

About This Presentation

Geology


Slide Content

Types of Folds and Faults
Paper-GGRM 101T4(Geomorphology)
Dr. NavamallikaSharma
Assistant Professor
Department of Geography
N. N. SaikiaCollege, Titabar

Forces responsible for landform
development
Forces which affect the earths crust
Endogeneticforces Exogeneticforces

Endogenetic
Forces
Diastrophic
Forces
Epeirogenetic
forces
Orogenetic
forces
Sudden
Forces
Volcanic
Eruption
Earthquake

Diastrophic
Forces
Orogenetic
forces
Tensional
forces
Crustal
Fracture
Cracking
Faulting
(Faults)
Compressional
forces
Crustal
bending
Warping
Upwarping Downwarping
Folding
(Folds)
Epeirogenetic
forces
Upward
movement
(Emergence)
Downward
Movement
(Submergence)

What is fold?
Wave-likebendsformedinthecrustal
rocksduetotangentialcompressiveforce
resultingfromhorizontalmovementcaused
bytheendogeneticforceoriginatingdeep
withintheeartharecalledfolds.

Different components of fold
Theupfoldedrockstratainarch-likeformare
calledanticlines.

Differentcomponentsof fold
Thedownfoldedstructureformingtrough-like
featureiscalledsynclines.

Different components of fold
Thetwosidesofafoldarecalledlimbsofthe
fold.

Different components of fold
•Theplanewhich
bisectstheangle
betweentwolimbsof
theanticlineormiddle
limbofthesynclineis
calledtheaxisoffold
oraxialplane.
•Onthebasisof
anticlineandsyncline
theseaxialplanesare
calledasaxisof
anticlineandaxisof
syncline

Dip and Strike
The inclination of rock beds with respect to
horizontal plane is termed as dip.
Dip is important as it gives the following
information:
The direction of maximum slope down a bedding
plane
The angle between the maximum slope and the
horizontal plane

Dip and Strike
•The strike of an inclined bed is the direction of
any horizontal line along a bedding plane.
•The direction of dip is always at right angle to
the strike.

Types of fold
Symmetrical fold

Types of fold
Asymmetrical fold

Types of fold
Monoclinalfold

Types of fold
IsoclinalFold

Types of fold
Recumbent Fold

Types of fold
Overturned Fold

Types of fold
Plunge Fold

Types of fold
Fan Fold

Types of fold
Open Fold

Types of fold
Closed Fold

What is Fault
Whenthecrustalrocksaredisplacedduetotensional
movementcausedbytheendogeneticforces,alongaplane
theresultantstructureiscalledafault.

Different parts of Fault
•The plane along which the rock blocks are displaced is
called fault plane.
•The angle between the fault plane and horizontal plane
is termed as fault dip.
•Uppermost block of a fault is called upthrownside
•Lowermost block of a fault is called downthrown side.
•Upper wall of a fault is known as hanging wall.
•Foot wall represents the lower wall of a fault.
•The steep wall-like slope caused by faulting of the
crustal rocks is called as fault scarp.

Different parts of Fault

Types of Faults:
Normal Faults are formed due to the
displacement of both the rock blocks in
opposite directions due to fracture upon
greatest stress.

Types of Faults:
ReverseFaultsareformedduetothe
movementofboththefracturedrockblocks
towardseachother.

Types of Faults:
Strike-slipFaultsareformedwhentherock
blocksaredisplacedhorizontallyalongthe
faultplaneduetohorizontalmovement.

Types of Faults:
Step Faults are a series of faults occur in any
area in such a way that the slops of all the
fault planes of all the faults are in the same
direction.

Thank you