Chapter 9 Folds, Faults,and Mountains 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 Strain- rocks response to stress Three types of stresses Types of Deformation ELASTIC DEFORMATION BRITTLE FAILURE PLASTIC DEFORMATION Elastic deformation deformation not permanent (minor amount of stress) Brittle stress amount exceeds the yield point or elastic limit Plastic (Ductile) deformation stress applied gradually to deep warm rocks Elastic Deformation Plastic Deformation Brittle Failure Folding at Converging Plate Boundaries Factors affecting rock deformation Intensity of Applied Stree Lithostatic Pressure Heat leads to stretching of rocks at near Earth’s surface without breaking at depth- plastic deformation Time Composition – different minerals have different strength Deformed rocks in the field Most apparent in Sedimentary Rocks Importance of deformation – Indicate Past Plate Motions – Indicates other Past Geological Events – Locates Specific Natural Resources – Rock Orientation: Strike and Dip Interpretation of Rock DeformationFolds 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-like Anticline- arch-like Types of folds- symmetrical, broad, open, overturn, recumbent Basin Rock deformation that is bowl shaped. Domes Rock deformation that is ova-shaped bulges Geometry of anticlines and synclines Artificial valleys and synclinal ridges Artificial valleys and synclinal ridgescontd. Various folds – Symmetrical (open) Various Folds - Assymetrical Various Folds - Overturned Various Folds - Recumbent Various Folds - Plunging Structural Domes and Basins Faults 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) Evidence of Faults Visible displacement of rocks Pulverized rock Slickensides Discontinuity of Rock Sequences Types of Faults: – Strike-Slip Fault – Dip-Slip Fault Fault Planes Fault Disruption Map of San Andreas Fault Horizontal movement along strike-slip fault Dip-slip Fault Mid-Atlantic Ridge Plate Tectonics and Faulting Normal Faults: Mid-Ocean Ridge & Continental Rifts Reverse and Thrust Faults: Convergent Plate Boundaries Strike-Slip Faults: Transform Boundaries Geology at a Glance Oblique Slip Correlation of different fault types Accumulation of Oil & Natural Gas Accumulation of oil along fault planes A terrace-producing scenario The mountain ranges of North America A terrace-producing scenario Provinces of the Applachian mountain system Mountainbelt collapsing Mountainbelt collapsing-contd.