'Strike slip faults' presentation slideshows

Chapter: Earthquakes

Table of Contents. Chapter: Earthquakes. Section 1: Forces Inside Earth. Section 2: Features of Earthquakes. Section 3: People and Earthquakes. Forces Inside Earth. 1. Earthquake Causes. The bending and breaking of wooden craft sticks are similar to how rocks bend and break.

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Chapter: Earthquakes

Table of Contents. Chapter: Earthquakes. Section 1: Forces Inside Earth. Section 2: Features of Earthquakes. Section 3: People and Earthquakes. Forces Inside Earth. 1. Earthquake Causes. The bending and breaking of wooden craft sticks are similar to how rocks bend and break.

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How did this happened?

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Wrench Fault Architecture of Trenton Black River Hydrothermal Dolomite Reservoirs

Wrench Fault Architecture of Trenton Black River Hydrothermal Dolomite Reservoirs. Taury Smith and Richard Nyahay New York State Museum. Model for Hydrothermal Dolomitization.

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Chapter 8

Chapter 8. The Theory of Plate Tectonics. Objectives. Given information about Plate Tectonics you will be able to describe: The history & development of the theory Supporting evidence Plate tectonic processes Phenomena explained by tectonic theory. Guiding Questions.

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Folding and Faulting

Folding and Faulting. Chapter 4, Sec. 4. Stress. Amount of force per area put on an object. Rocks can change shape due to stress. Three types of stress:. Compression Tension Shear. FOLDING. Rock layers bend due to stress Assume most rocks are laid down horizontal. FAULTS.

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Plate Tectonics and Earthquakes

Plate Tectonics and Earthquakes. Brittle vs. Ductile Deformation. Brittle. Ductile. Bends when stressed. Breaks when stressed. Brittle vs. Ductile Deformation. Deformation is dependent on: 1. Temperature (Cold or Hot) 2. Composition (Soft or Hard) 3. Strain Rate (Fast or Slow).

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Plate Tectonics and Earthquakes

Plate Tectonics and Earthquakes. Brittle vs. Ductile Deformation. Brittle. Ductile. Bends when stressed. Breaks when stressed. Brittle vs. Ductile Deformation. Deformation is dependent on: 1. Temperature (Cold or Hot) 2. Composition (Soft or Hard) 3. Strain Rate (Fast or Slow).

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Strike-slip fault and its related structure

Strike-slip fault and its related structure. 01003117 LuoMao. Strike-slip fault. Definition : a kind of fault that the two blocks move along the strike direction of fault plane. It can be subdivided into two kinds. ?sinistral(left lateral)-----the opposite block moves to the left

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Gly 326 Autumn, of the year that we are in

GLY 326 Structural Geology. Lecture 31 Strike-slip Faults. Gly 326 Autumn, of the year that we are in. Strike-slip faults: i.e. the movement parallels strike. Transform Plate Boundaries.

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Lecture Outlines Physical Geology, 7/e

Lecture Outlines Physical Geology, 7/e. Carlson. Geologic Structures Physical Geology 7/e, Chapter 6. Steve Kadel, Glendale Community College. Geologic Structures.

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Lecture Outlines Physical Geology, 10/e

Lecture Outlines Physical Geology, 10/e. Plummer, McGeary & Carlson. Geologic Structures Physical Geology 10/e, Chapter 15. Steve Kadel, Glendale Community College. Geologic Structures.

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Structural Geology

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Tim Horner CSUS Geology Department

Geologic Structures Physical Geology, Chapter 15. Tim Horner CSUS Geology Department. Geologic Structures. Geologic structures are dynamically-produced patterns or arrangements of rock or sediment that result from, and give information about, forces within the Earth

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Coulomb stress change due to Wenchuan Earthquake

Coulomb stress change due to Wenchuan Earthquake. Source fault. dCFS on Reverse faults. H=30km, Reverse faults. dCFS on faults with rake=135. dCFS on strike-slip faults.

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Strike-Slip Faults

Strike-Slip Faults. The rocks on either side of the fault grind past each other side-ways with little up or down motion Transform boundary: boundary between 2 plates is a strike-slip fault. San Andreas Fault in California. Strike-slip Fault. Strike-slip Fault.

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