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Stress: Force per unit area Strain: Change in length/area/volume to original length/area/volume ...

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Stress: Force per unit area Strain: Change in length/area/volume to original length/area/volume Rocks are subjected to great forces- particularly at plate margins Compression- converging plate boundary Tension- diverging plate boundary Shearing- transform plate boundary Chapter 9 Folds, Chapter 9 Folds, Faults,and Mountains Faults,and Mountains
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Page 1: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Stress: Force per unit areaStrain: Change in length/area/volume to original length/area/volumeRocks are subjected to great forces- particularly at plate margins

Compression- converging plate boundaryTension- diverging plate boundaryShearing- transform plate boundary

Strain- rocks response to stress

Chapter 9 Folds, Faults,and Chapter 9 Folds, Faults,and Mountains Mountains

Page 2: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Three types of stressesThree types of stresses

Page 3: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Types of DeformationTypes of DeformationELASTIC DEFORMATIONBRITTLE FAILUREPLASTIC DEFORMATIONElastic deformation

deformation not permanent (minor amount of stress)

Brittlestress amount exceeds the yield point or elastic limit

Plastic (Ductile) deformationstress applied gradually to deep warm rocks

Page 4: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Elastic DeformationElastic Deformation

Page 5: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Plastic DeformationPlastic Deformation

Page 6: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Brittle FailureBrittle Failure

Page 7: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Folding at Converging Plate BoundariesFolding at Converging Plate Boundaries

Page 8: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Factors affecting rock deformationFactors affecting rock deformation

Intensity of Applied StreeLithostatic PressureHeat

leads to stretching of rocks at near Earth’s surface without breaking

at depth- plastic deformation

TimeComposition

– different minerals have different strength

Page 9: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Deformed rocks in the fieldDeformed rocks in the field

Most apparent in Sedimentary RocksImportance of deformation

– Indicate Past Plate Motions– Indicates other Past Geological Events– Locates Specific Natural Resources

– Rock Orientation: Strike and Dip

Page 10: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Interpretation of Rock Deformation-Interpretation of Rock Deformation-FoldsFolds

In describing folds, need to know the orientation of the rock in space- STRIKE and the angle at which rock is inclined to the horizontal- DIP

Folds- rocks deform plastically (most occur at convergent plates)Syncline- trough-likeAnticline- arch-likeTypes of folds- symmetrical, broad, open, overturn,

recumbent Basin

Rock deformation that is bowl shaped. Domes

Rock deformation that is ova-shaped bulges

Page 11: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Geometry of anticlines and synclinesGeometry of anticlines and synclines

Page 12: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Artificial valleys and synclinal ridgesArtificial valleys and synclinal ridges

Page 13: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Artificial valleys and synclinal ridges-Artificial valleys and synclinal ridges-contd.contd.

Page 14: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Various folds – Symmetrical (open)Various folds – Symmetrical (open)

Page 15: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Various Folds - AssymetricalVarious Folds - Assymetrical

Page 16: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Various Folds - OverturnedVarious Folds - Overturned

Page 17: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Various Folds - RecumbentVarious Folds - Recumbent

Page 18: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Various Folds - PlungingVarious Folds - Plunging

Page 19: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Structural Domes and BasinsStructural Domes and Basins

Page 20: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

FaultsFaults A fracture is a break in a rock (joint or a fault) Joints: Fractures with no relative movement Fault is when there is relative movement along the break Fault Types

Strike-Slip fault horizontal movement (transform plate boundary)

Dip-Slip fault Normal (tensional stress) Reserve (compressional stress) Thrust (low angle reserve fault) Oblique (combination of strike-slip & dip-slip)

Page 21: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Evidence of FaultsEvidence of FaultsVisible displacement of rocksPulverized rockSlickensidesDiscontinuity of Rock Sequences

Types of Faults:– Strike-Slip Fault– Dip-Slip Fault

Page 22: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Fault PlanesFault Planes

Page 23: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Fault DisruptionFault Disruption

Page 24: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Map of San Andreas FaultMap of San Andreas Fault

Page 25: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Horizontal movement along strike-slip faultHorizontal movement along strike-slip fault

Page 26: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Dip-slip FaultDip-slip Fault

Page 27: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Mid-Atlantic RidgeMid-Atlantic Ridge

Page 28: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Plate Tectonics and FaultingPlate Tectonics and Faulting

Normal Faults: Mid-Ocean Ridge & Continental Rifts

Reverse and Thrust Faults: Convergent Plate Boundaries

Strike-Slip Faults: Transform Boundaries

Page 29: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Geology at a GlanceGeology at a Glance

Page 30: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Oblique SlipOblique Slip

Page 31: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Correlation of different fault typesCorrelation of different fault types

Page 32: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Accumulation of Oil & Natural GasAccumulation of Oil & Natural Gas

Page 33: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Accumulation of oil along fault planesAccumulation of oil along fault planes

Page 34: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

A terrace-producing scenarioA terrace-producing scenario

Page 35: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

The mountain ranges of North AmericaThe mountain ranges of North America

Page 36: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

A terrace-producing scenarioA terrace-producing scenario

Page 37: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Provinces of the Applachian mountain systemProvinces of the Applachian mountain system

Page 38: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Mountainbelt collapsing Mountainbelt collapsing

Page 39: Stress: Force per unit area  Strain: Change in length/area/volume to original length/area/volume  Rocks are subjected to great forces- particularly.

Mountainbelt collapsing-contd.Mountainbelt collapsing-contd.


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